2019 Hypothetical Atlantic Hurricane Season (Sebastian's Version)

The 2019 Hypothetical Atlantic hurricane season was a very hyperactive season with the Greek naming list being exhausted. This was the first year STCC Atlantic was introduced after being built in Miami, Florida along with the NHC on Decemebr 30, 2018. The first storm formed on January 1 and the last storm dissipated on October 28. The strongest storm of the season was Hurricane Alpha that peaked with winds of 175 mph (280 km/h) and a minimum pressure of 904 mbar. There were 60 total depressions, 45 named storms, 35 hurricanes, and 30 major hurricanes. The season had caused $20.921 billion in damages (2019 USD) and 2,121 fatalities. The costliest storm of the season was Hurricane Tau which caused $4.03 billion (2019 USD) in damages in the Lesser Antilles, Colombia, Venezuela, Jamaica, Central America, Mexico, and Texas combined. The deadliest storm of the season was Hurricane Rho which caused 517 total deaths in the Caribbean Islands, The Bahamas, and the United States combined. The most memorable landfall of the season was Hurricane Mu was the strongest storm to hit Greenland, the first storm to hit Greenland still as a tropical system, and the first major hurricane to hit Greenland still tropical. A lot of storms made landfall over areas that had not had major hurricanes since record keeping began such as in Ireland, Northeastern United States, Greenland, and other unusual tropical landfall locations.The longest lasting storm was Hurricane Gamma which lasted for 42 days from May 4 to June 14, 2019. It is the longest lasting storm in the hypothetical world of hurricanes, surpassing Hurricane John in the real world of hurricanes. A lot of hurricanes reached major hurricane strength at an unusually high latitude such as Hurricane Sebastien, Hurricane Van, Hurricane Alpha, Hurricane Gamma, Hurricane Zeta, and every other storm that reached major hurricane strength at an unusually high latitude. A few storms managed to reach Europe or Greenland while stil being tropical such as Hurricane Sebastien making landfall in Ireland as a hurricane still tropical and Hurricane Mu making landfall in Greenland as a major hurricane still tropical. Despite the hyperactivity, only one storm of all had reached Category 5 status which was the strongest storm of the season, Alpha with peak winds of 175 mph (280 km/h).

Hurricane Andrea (01L)
On December 27, a low pressure area moved erratically across the tropical Atlantic, entering and exiting the eastern Caribbean Sea a lot of times; without being organized. On December 31, a high pressure area formed east of the low pressure area, meaning that the system moved to the west-northwest. Shortly afterward, the system encountered deep convection. On the following year and day, January 1, the system strengthened into Tropical Depression One, becoming the first depression of the season. An hour later, it strengthened into a tropical storm and given the first name on the list, Andrea, becoming the first named storm of the season. It reached its initial peak intensity with winds of 45 mph (75 km/h) until moderate shear and land interaction caused the system to weaken to a tropical depression. Shortly afterward, it made 2 landfalls over the Bahamas. It maintained its intensity while over The Bahamas until January 3 when it crossed into the Straits of Florida, restrengthening into a tropical storm and made its third landfall over the Florida Keys and shortly afterward, emerged into the Gulf of Mexico. In the Gulf of Mexico and strengthened to a Category 1 hurricane 6 hours later, becoming the first hurricane of the season and Category 2 then Category 3 major hurricane status on January 5, becoming the first major hurricane of the season. Shortly after peaking, it underwent an eyewall replacement cycle, weakening to a Category 2 hurricane. Shortly afterward, it weakened to a Category 1 hurricane due to cooler sea surface temperatures before making its fourth and final landfall over Texas with winds of 95 mph (145 km/h). It rapidly weakened when moving even further inland, degenerating into a remnant low on January 8. The remnants hit New Mexico, dissipating on January 9. The system and its precursor brought heavy rainfall in the Windward Islands and flooding but no deaths reported. It also brought heavy rainfall across the Leeward Islands bringing major flooding in Barbuda and St. Martin and minor flooding in Antigua and St. Thomas. There was also tropical storm force winds over the islands. In the Greater Antilles, the northern coast was flooding due to surf and heavy rainfall up to 300-400mm, killing 6 people. In the Bahamas, a man died due to cancer when men were trying to get him to the hospital during flooding. This was the only indirect death. In the Florida Keys, 2 people died due to drowning in floodwaters. In the Gulf Coast, Texas was the hardest hit with high flooding in Galveston, Greater Houston, Dallas, and the Bolivar Peninsula. There was 2 deaths in Texas and one in Louisiana. New Mexico had no deaths and flooding. The system had caused $49.6 million (2019 USD) in all the areas it affected and damaged.

Hurricane Barry (02L)
On December 28, a non-tropical low formed west of the Canary Islands, it drifted westward, still non-tropical. On December 30, it had gained subtropical characteristics. The following day, December 31, it became a tropical disturbance due to sea surface temperature up to 26 degrees Celsius. It had bursts of convection for two days. On January 2, it organized into Tropical Depression Two, becoming the second depression of the season. Two hours later, it strengthened into a tropical storm and given the next name, Barry, becoming the second named storm of the season. Soon afterward it traversed into very warm sea surface temperatures, 29-31 degrees Celsius, rapidly intensifying into a Category 1 hurricane the following day, January 3, becoming the second hurricane of the season and a Category 2 in just 18 hours in the same day. 12 hours later, it rapidly intensified into a Category 3 major hurricane, becoming the second major hurricane of the season. Shortly after peaking, it began undergoing an eyewall replacement cycle, dropping below major hurricane strength. Shortly after the eyewall replacement cycle. It entered a zone of high wind shear (55-60 knots), causing the system to rapidly weaken to a Category 1 before making landfall over North Carolina with winds of 75 mph (120 km/h). Shortly after landfall, it transitioned to an extratropical cyclone while moving inland for two days while continuing to weaken. It dissipated on January 13. The system brought heavy rainfall and gusty winds over Bermuda, bringing flooding across the island. Despite this, no deaths were reported. In the United States, North Carolina was the hardest hit from the storm despite the system only being a minimal hurricane at landfall. It brought very high flooding, high waves, and gusty winds in the Outer Banks, caused an indirect and only death by a traffic accident in flooding in Charlotte, North Carolina from Barry as an extratropical cyclone. The other states it affected had no deaths but major damages and flooding reported. The storm caused $246.78 million (2019 USD) in all the areas it affected and damaged.

Tropical Storm Chantal (03L)
On January 4, a disorganized but well-defined tropical wave exited the coast of West Africa. It became disorganized until January 7, when deep convection in the tropical wave developed. Its convection developed when it crept closer to the Lesser Antilles for six days. On January 13, the tropical wave organized into Tropical Depression Three, becoming the third depression of the season. Six hours later it strengthened into a tropical storm and given the next name on the list, Chantal, becoming the third named storm of the season. Shortly after being upgraded to a tropical storm, it reached its peak. At its peak, it had an eye-like feature. On January 15, Chantal made landfall over the Dominican Republic with winds of 45 mph (75 km/h) and a pressure of 999 mbars. Shortly after landfall, it weakened into a tropical depression. Later on the same day it moved offshore, restrengthening into a tropical storm again during its secondary peak intensity north of the Tiburon Peninsula in Haiti. Its second peak didn't last for long due to land interaction in Cuba, where it weakened into a tropical depression. On January 17, it was downgraded into a remnant low but later on the same day, it reorganized back into a tropical depression. Shortly after being re-classified as a tropical depression, it reached its third peak intensity with winds of 35 mph (55 km/h). Shortly after peaking wind shear from a high pressure area over the Southeastern United States prevented the system from restrengthening into a tropical storm again. On January 19, it made its final landfall near Brownsville, Texas. Shortly after landfall it degenerated into a remnant low again. The system moved further inland into Mexico, where it dissipated over the Mexican state of Coahuila the following day, January 20. The tropical depression brought major flooding across the Lesser Antilles, particularly in Dominica, Montserrat, Guadeloupe, St. Martin, and St. Lucia. In the Greater Antilles, there were tropical storm force winds over Hispaniola and Cuba. Puerto Rico did not have tropical storm force winds but it had rip currents over the southern coastline. There was flooding in San Juan. There were 6 indirect deaths there, mostly due to turbulent flights for people with diseases. In Hispaniola, this was the hardest hit, particularly in Haiti. In Haiti, 19 people died due to drowning and freshwater flooding. In the Dominican Republic, there were tropical storm force winds over the country. Two deaths were reported in the country, mostly in Santo Domingo. In Cuba, there was also tropical storm force winds. There was also high waves and coastal flooding, where one died in Santiago de Cuba. In Texas, there was flooding in Brownsville, McAllen, Corpus Christi, and Rockport. There were 3 deaths in Corpus Christi due to drowning. There was 200-350mm of rainfall. In Mexico, the storm's remnants brought 50-100mm of rainfall over Coahuila and flooding but no deaths reported. The system caused $2 million (2019 USD) in all the areas it affected and damaged.

Tropical Depression Four (04L)
On January 16, a tropical wave moved off the coast of West Africa. The following day, January 17, it completed a tight counter-clockwise loop, turning to the north due to a high pressure area south of it. It moved north, nearly stationary, over warm sea surface temperatures. The system had bursts of convection for days, until January 21, when the tropical wave organized into Tropical Depression Four, becoming the fourth depression of the season. Shortly after formation, it reached its peak. It stayed at its peak for four days until it made landfall over Cape Verde where it encountered unfavorable conditions. Shortly after landfall, it turned to the northwest, due to a ridge to its east on January 26. When it turned to the northwest, it encountered dry air, causing it to degenerate into a remnant low the following day, January 27. It dissipated later that day. Due the system's slow movement near Cape Verde, it brought heavy rainfall across all of the Cape Verde islands with the highest being 400mm in Santiago and Praia. It brought high flooding across Brava, Sal, Fogo, Praia, and Boa Vista. Despite the high flooding, there was minimal damage in the islands.

Hurricane Dorian (05L)
On January 20, a tropical wave move off the coast of West Africa. It became disorganized while south of the Cape Verde islands as a slow-moving tropical wave. On January 22, it developed bursts of convection when moving away from the Cape Verde islands. Bursts of deep convection were already in the tropical wave and on January 25, it organized into Tropical Depression Five, becoming the fifth depression of the season. It maintained its intensity for a day until it strengthened into a tropical storm early the next day, January 26, and given the next name on the list, Dorian, becoming the fourth named storm of the season. Shortly after being named, Dorian began a period of rapid intensification, intensifying from a tropical storm into a hurricane in just 18 hours, becoming the third hurricane of the season and into a major hurricane in the following period, becoming the third major hurricane of the season and reaching its initial peak intensity as a Category 3. Shortly after reaching major hurricane strength and its initial peak intensity, it underwent an eyewall replacement cycle, falling to a Category 2 hurricane and made its first landfall over the Bahamas on January 29. It maintained its intensity for nearly two days and made its second landfall in the Florida Keys on January 31 and emerged into the Gulf of Mexico the following day, February 1. Shortly after it moved into the Gulf of Mexico, it rapidly intensified and regained major hurricane status and reached its peak on the following day, February 2. A few hours after peaking, it underwent another eyewall replacement cycle before landfall, weakening to a Category 3. Shortly after the eyewall replacement cycle, it made its final landfall over Corpus Christi. It rapidly weakened while moving even further inland and lost its convection over New Mexico, becoming a remnant low. The remnant low dissipated over Arizona, two days later. Dorian brought rough surf and heavy rain around 700mm, bringing flooding across St. Croix, Antigua and Barbuda, and St. Martin, killing 21 people, 19 direct due to flooding and 2 indirect due to a plane crash in bad weather conditions near St. Thomas. In the Greater Antilles, there was rough surf, rip currents, storm surge, coastal flooding, and major flooding in Hispaniola, Cuba, and Puerto Rico. There were 400-500mm of rainfall in Cuba, 300-400mm in Hispaniola, and 200mm in Puerto Rico. There were 22 deaths in the Greater Antilles, 13 in Hispaniola, 5 in Cuba, and 4 in Puerto Rico, all due to flooding except for Cuba, where there was 5-7 tornadoes caught on camera. In the Florida Keys and South Florida, there was also major flooding, mostly in Miami, Fort Lauderdale, Key West, Cudjoe Key, and Loggerhead Key. There were only 3 deaths in Florida. 2 in the Florida Keys and 1 in South Florida. In the Gulf Coast, large swells, rip currents, storm surges, torrential rainfall up to 750mm, and flooding up to 5 meters high in Corpus Christi, Dallas, Houston, Brownsville, and Galveston, causing 4 deaths, 2 in Corpus Christi, 1 in Houston, and 1 in Dallas. In Mexico, there was heavy rainfall up to 100mm brought minor flooding Nuevo Leon and Coahuila. In Tamaulipas, there were storm surges and coastal flooding, killing one person. In New Mexico and Arizona the storm's remnants brought moderate to heavy rainfall in Scottsdale, Santa Fe, El Paso, and Albuquerque. Despite this, there was no flooding and deaths. The system caused $128.34 million (2019 USD) in all the areas it affected and damaged.

Tropical Storm Erin (06L)
On January 24 a tropical disturbance formed south of Cuba. The disturbance turned to the north-northeast shortly after emerging into the Gulf of Mexico. On January 25, the disturbance completed a tight loop over Florida, particularly near Lake Okeechobee, bringing heavy rainfall over the state. On the following day, January 26, it reemerged into the Gulf of Mexico. On the following day, January 27, bursts of convection caused the disturbance to organize into Tropical Depression Six, becoming the sixth depression of the season. The following day, January 28, the tropical depression strengthened into a tropical storm and given the next name on the list, Erin, becoming the fifth named storm of the season. At its peak, it had a hurricane eye-like feature Shortly after being upgraded to a tropical storm, it reached its peak intensity. It stayed at tropical storm intensity for five days until February 1 when nearby outflow from the larger Hurricane Dorian caused the system to weaken to a tropical depression. The system continued weakening and weakened into a remnant low the following day, February 2. Later on the same day, the remnants made landfall over the Texas-Louisiana border. The following day after landfall, February 3, its remnants were eventually absorbed by the larger Hurricane Dorian. The precursor brought heavy to torrential rainfall across Western Cuba, including Isla de la Juventud. This resulted in major flooding in Havana, Harlem, Mariel, San Cristobal, and Artemisa. Despite this, no deaths were reported. The precursor also brought torrential rainfall and flooding due to the fact that it completed a tight loop near Lake Okeechobee, causing the water levels of the lake to rise 3-4 feet high, bringing flooding across the areas surrounding the lake. Despite this, there was even major flooding in the Florida Keys and the state's peninsula, most especially in Key West, Key Largo, Cudjoe Key, Big Pine Key, Fort Lauderdale, Tampa, Jupiter, and Miami. Despite this there was no deaths reported in the state. In the Gulf Coast, the system brought rip currents and heavy rainfall, even its remnants did, particularly in Texas and Louisiana. In both states, the level of the Mississippi River rose to 2 feet high, bringing flooding across the areas surrounding the river, including Lake Sabina. Despite this, there was no deaths and no tropical storm force winds. The system caused $3,590 (2019 USD) in all the areas it affected and damaged.

Hurricane Fernand (07L)
On February 3 a non-tropical low formed miles north of San Juan, Puerto Rico. It was originally moving northeast due to a ridge a few miles northwest of the non-tropical low. It continued to moved northeast for two days until February 5, when the system turned to the west when the ridge dissipated. The following day, February 6, the system became a subtropical low. Shortly after being subtropical, it organized into Subtropical Depression Seven, becoming the seventh depression of the season. Early the following day, the system strengthened into a subtropical storm and given the next name, Fernand, becoming the sixth named storm of the season. Shortly after being upgraded to a subtropical storm, it transitioned into a tropical storm since it moved into sea surface temperatures of 27-29 degrees Celsius. Shortly after becoming a tropical system, it rapidly intensified into a hurricane in just 24 hours, becoming the fourth hurricane of the season and into a major hurricane in also 24 hours, becoming the fourth major hurricane of the season. On February 13, it reached its peak intensity. Shortly after peaking, Fernand started undergoing an eyewall replacement cycle causing it to rapidly weaken below major hurricane status. Shortly after weakening, it made landfall near Charleston, South Carolina on February 14 with winds of 110 mph (175 km/h). Shortly after landfall, it rapidly weakened due to high mountains, degenerating into a remnant low on February 14. It dissipated on the following day. The system brought tropical storm force winds, storm surges, and flooding in Bermuda. There were 2 indirect deaths due to car accidents due to winds. In Northeast Florida, rainbands brought heavy rainfall and a tornado outbreak was reported in Jacksonville and also in St. Augustine, killing 1 person. In the East Coast, South Carolina was the hardest hit, with waves being 4-5 feet high, flooding 3 feet high, and rainfall up to 600mm mostly in Charleston, Myrtle Beach, Florence, and Columbia. In coastal area in Georgia and the Carolinas, there were waves and rip currents. There was also flooding, mostly in Savannah and Augusta in Georgia, 2 feet high, Wilmington, Charlotte, and Fayettville in North Carolina, 3 feet high. The system caused $4 million (2019 USD) in all the areas it affected and damaged.

Hurricane Gabrielle (08L)
On February 7, a tropical wave moved off the coast of West Africa. Bursts of convection and low wind shear allowed the tropical wave to organize into a tropical depression and on the following day, February 8, the wave organized into Tropical Depression Eight, becoming the eighth depression of the season. It stayed at its intensity for two days until February 10 when the tropical depression strengthened into a tropical storm and given the next name on the list, Gabrielle, becoming the seventh named storm of the season. The system maintained its intensity for four days due to low to moderate northerly wind shear. On February 14, when wind shear was low and sea surface temperatures were high, deep convection was associated in the system causing the system to rapidly intensify into a hurricane in the afternoon of the same day, becoming the fifth hurricane of the season. The system strengthened into a major hurricane on February 16, becoming the fifth major hurricane of the season. 6 hours after being upgraded to a major hurricane. Gabrielle reached its peak intensity. Shortly after reaching its peak, it began to undergo an eyewall replacement cycle, falling briefly below major hurricane status. When it finished the eyewall replacement cycle. It restrengthened into a major hurricane reaching its second peak intensity. Shortly after restrengthening to major hurricane strength. It entered a zone of moderate wind shear, on February 18, weakening below major hurricane status and even further into a Category 1 but restrengthened to reach a third peak with winds of 95 mph (145 km/h) and a pressure of 975 mbars on February 20. It weakened again due to land interaction and made landfall near Brunswick, Georgia with winds of 85 mph (140 km/h) on the following day, February 21. It rapidly weakened while moving further inland, degenerating into a remnant low after moving inland for two days on February 23. It dissipated the following day, February 24.

The system brought hurricane force winds, waves up to 5 feet high, and major flooding in the Bahamas, mostly in Grand Bahama, Nassau, and Freeport. Despite this no deaths have been reported. In Florida, there was high surf in the eastern coast of the state but in the northeastern part of the state, its eyewall brought strong winds and heavy to torrential rainfall across the state. Despite this, there was also no deaths reported. In Georgia, torrential rainfall up to 600mm brought high flooding across the state, most especially in Brunswick, Atlanta, and Athens. There was also no deaths reported. Inland, in Alabama and Mississippi, there was heavy rainfall and despite the remnants dissipating over Alabama, it even reached into Mississippi, bringing rainfall up to 150mm. Despite this, there were also no deaths reported. The system caused $99.2 million (2019 USD) in all the areas it affected and damaged.

Hurricane Humberto (09L)
On February 13, a tropical wave exited West Africa. There was no further development due to moderate wind shear for two days until February 15 when the system entered a zone of low wind shear. Bursts of convection allowed the system to organize into Tropical Depression Nine, becoming the ninth depression of the season. The following day, February 17, the depression strengthened into a tropical storm and given the next name on the list, Humberto, becoming the eighth named storm of the season. On February 19, Humberto made its first landfall over St. Lucia. Shortly after landfall, bursts of convection allowed the system to strengthen into a hurricane the following day, February 20, becoming the sixth hurricane of the season. On February 22, the eyewall passed over Jamaica. Despite this, the system continued to strengthen and on February 23, the system strengthened into a major hurricane, becoming the sixth major hurricane of the season. Shortly after being upgraded to a major hurricane, the system made its second landfall near Mahahual, Quintana Roo later that day. Despite landfall, the system maintained major hurricane status for two days until February 24, when the system underwent an eyewall replacement cycle, falling below major hurricane status. Shortly after Humberto finished the eyewall replacement cycle, it rapidly weakened to a Category 2 hurricane to a tropical storm in just six hours due to cooler sea surface temperatures up to 24 degrees Celsius just before making its final landfall near Tampico, Veracruz with winds of 70 mph (110 km/h) on February 25. It rapidly weakened while moving inland, degenerating into a remnant low the following day, February 26. It dissipated later that day over Zacaetas, Mexico.

In the Windward Islands, there were tropical storm force winds in Barbados, St. Lucia, Dominica, Martinique, St. Vincent and the Grenadines, and Grenada. There was also torrential rainfall up to 300mm in the islands with tropical storm force winds. There was also major flooding in the same areas, killing 3 people. In the Greater Antilles, the eyewall passed over Jamaica as a Category 2 hurricane with winds of 100mph (155km/h), bringing hurricane force winds, rainfall up to 500-600mm and destroyed buildings that killed 14 people; indirect. There was flooding that killed 6 people. The rest of the Greater Antilles experienced high surf and rip currents, killing 2 people; 1 in Puerto Rico, and 1 in Cuba; all direct. In the Cayman Islands, there was strong winds, also, storm surges, rainfall up to 600mm and major flooding, killing 4 direct due to drowning and 3 indirect due to car accidents. In Belize and Guatemala, the storm's outer edges brought torrential rainfall and flooding that killed 1 person. Despite this, there was also a tornado reported in Corozal Town, Belize, but no deaths reported. In the rest of Central America, there was high surf. In Mexico, Quintana Roo was the hardest hit with winds equivalent to a major hurricane, high waves, storm surge up to 4 feet high and flooding up to 3 feet high, killing 2 people. In the rest of Mexico, heavy rainfall in Veracruz and all the areas affected by the storm in Mexico up to 200mm. Despite this, there was no flooding and deaths. The system caused $298 million (2019 USD) in all the areas it affected and damaged.

Hurricane Imelda (10L)
On February 16, a tropical wave emerged off the coast of West Africa. Its convection deepened for two days until February 18 when the tropical wave organized into Tropical Depression Ten, becoming the tenth depression of the season, southwest of the Cape Verde islands. The following day, the system strengthened into a tropical storm and given the next name on the list, Imelda, becoming the ninth named storm of the season. The system maintained its intensity for two days until February 21 when the system strengthened into a hurricane, becoming the seventh hurricane of the season. The system maintained Category 1 intensity for three days until February 24, when the system was upgraded to a Category 2 hurricane. Shortly after being upgraded to a Category 2, it underwent rapid deepening. The system strengthened into a major hurricane in just six hours, becoming the seventh major hurricane of the season. The system rapidly intensified from a Category 3 into a Category 4 in just six hours, again. In just twelve hours, the system reached its peak intensity on February 27. Shortly after reaching its peak intensity, it underwent an eyewall replacement cycle, falling to a Category 3. When Imelda finished the eyewall replacement cycle it started undergoing a weakening phase due to unfavorable conditions, falling below major hurricane status on March 1. The day after Imelda fell below major hurricane status, it began to restrengthen briefly into a major hurricane after it entered a favorable zone. On March 4, Imelda reached its secondary peak with winds of 115 mph (185 km/h) and a pressure of 958 mbars. Shortly after reaching its secondary peak, it began to undergo its second eyewall replacement cycle, falling below major hurricane status again. It began to weaken rapidly due to wind shear from a high pressure area east of Bermuda. It weakened even further into a Category 1 and made landfall over North Carolina on March 6 with winds of 85 mph (140 km/h) and a pressure of 972 mbars. Shortly after landfall it underwent extratropical transition and completed it in just below six hours. It continued to weaken. The extratropical remnant passed east of Lake Erie and dissipated east of the lake over New York.

In the East Coast, North Carolina was the hardest hit, mostly in the Outer Banks with its strongest winds of landfall, rainfall up to 700mm, and flooding the entire bank up to 5-6 meters high, killing 12 people. In the rest of the state, there was also strong winds, torrential rainfall up to 600-635mm, and flooding up to 4 meters high, in Wilmington, Raleigh, Durham, Jacksonville, and Greenville, killing 5 people in all cities combined. In the rest of the East Coast, there was high surf and its outer edges brought rainfall up to 200-300mm. There was no flooding. There was 3 deaths due to high surf. In the Great Lakes region, the flood waters in Lake Erie rose up to 3 meters high, bringing flooding around the lake. All deaths were from flooding. In Canada, its extratropical remnants brought flooding in Quebec and Ontario. There were no deaths reported. In its extratropical phase, it summoned a tornado outbreak from March 8-10 in the Delmarva Peninsula, West Virginia, Pennsylvania, New York, New Jersey, and Vermont. There were 29-30 tornadoes reported in all states combined. Despite this, there were no deaths reported. The system caused $50 million (2019 USD) in all the areas it affected and damaged.

Hurricane Jerry (11L)
On February 19, a tropical wave moved off the coast of West Africa. The following day, February 20, bursts of convection allowed the system to organize into Tropical Depression Eleven, becoming the eleventh depression of the season. The system maintained its intensity for two days until February 22, when the system strengthened into a tropical storm and given the next name on the list, Jerry, becoming the tenth named storm of the season. Jerry had maintained its intensity for three days until early on February 25, when the system made landfall over Dominica with winds of 70 mph (110 km/h) and a pressure of 988 mbars. On the same day, it emerged into the Caribbean Sea and shortly afterward, it strengthened into a hurricane, becoming the eighth hurricane of the season. It maintained Category 1 intensity for two days until February 27 when it passed south of Jamaica. Shortly after passing near Jamaica, it intensified into a Category 2 hurricane. The following day, February 28, it strengthened into a major hurricane, becoming the eighth major hurricane of the season. Shortly after strengthening into a Category 3 major hurricane, it made landfall near Chetumal, Quintana Roo. The following day after landfall, March 1, it weakened into a Category 2, falling below major hurricane status. Later that day, it emerged into a Bay of Campeche. Shortly afterwards, it headed west-southwest towards Tabasco due to a high pressure area over the Gulf Coast of the US, causing the eyewall to hit Tabasco. Shortly after the eyewall hitting Tabasco, another high pressure area in the Gulf of Tehuantepec steered the system to the west-northwest and shear from the high pressure area north of it caused to weaken to a Category 1 hurricane just before making its final landfall near Heroica Veracruz, Veracruz early the following day, March 2. It rapidly weakened degerating into a remant low just off the coast of Jalisco in the Northeast Pacific but turned northeast due to a ridge to its southwest. The remnants dissipated the following day, March 3, near Tepic, Nayarit.

In Cape Verde, there was heavy rainfall in Sao Felipe. In the Lesser Antilles, Guadeloupe, Dominica, Montserrat, Antigua and Barbuda, Martinique, St. Lucia, Barbados, St. Vincent and the Grenadines experienced 400mm of rainfall in two days, waves up to 2 feet high, and flooding in all the areas affected in 400mm of rainfall up to 3 feet high when the system made landfall over Dominica, killing 4 people direct due to high surf and 9 indirect due to falling trees collapsing on them due to the winds. In the Greater Antilles, there were tropical storm force winds and rainfall up to 300mm and large swells in all of the islands. Despite this, there were no deaths reported. In Central America, Belize had hurricane force winds and Guatemala had tropical storm force winds. In the rest, there were just large swells. There were also no deaths reported. Mexico, Quintana Roo was still recovering from the effects of Humberto when it was the hardest hit. This was similar to Jerry since it brought rainfall up to 600mm, storm surge up to 2-3 meters high, and flooding up to 4 meters high, killing 8 direct due to drowning, 10 indirect due to trafic accidents during evacuations. In Tabasco, the Category 2 eyewall hit with winds of 105mph (166km/h) bringing hurricane force winds that knocked down trees and rainfall up to 300mm. There was no flooding and deaths. In Veracruz, there was Category 1 winds and rainfall up to 180mm. No deaths and flooding were reported. In the rest of the Mexicans states affected, there was strong winds and rainfall up to 230mm but no flooding and deaths reported. The system caused $23.4 million (2019 USD) in all the areas it affected and damaged.

Tropical Storm Karen (12L)
On February 23, a tropical wave exited West Africa. The wave couldn't organize at first due to unfavorable conditions but as it crept closer to land it encountered favorable conditions for development and on February 27, the wave organized into Tropical Depression Twelve, becoming the twelfth depression of the season. The following day, February 28, the system strengthened into a tropical storm and given the next name on the list, Karen, becoming the eleventh named storm of the season. The following day after the system was upgraded into a tropical storm, March 1, it reached its initial peak intensity with its peak winds of 60 mph (95 km/h) but a pressure higher than its peak. The pressure higher than its peak is 994 mbar. Shortly after reaching its initial peak intensity with its peak winds but not its minimum pressure, Moderate wind shear displaced the system's center and caused it to weaken while approaching the Bahamas and on March 4, Karen weakened into a tropical depression and made its first landfall over the Bahamas as a tropical depression with winds of 35 mph (55 km/h) and a pressure of 1000 mbar. The following day, March 5, Karen crossed into the Straits of Florida and made its second landfall between Islamorada and Leyton still as a tropical depression with winds of 30 mph (45 km/h) and a pressure of 1003 mbar. Shortly after landfall, the system restrengthened to a tropical storm just west of Florida. On March 7, Karen reached its peak intensity. In its peak intensity, Karen's wind reached its secondary peak with winds of 50mph (85km/h) and its minimum pressure of 992 mbar. Karen stayed at its peak for 24 hours. On March 8, it began to weaken due to land interaction despite being offshore. Early on March 9, Karen made its final landfall near the Texas-Louisiana border, the same area where Erin made landfall nearly 2 months ago. The following day after landfall, Karen degenerated into a remnant low. Early the following day, March 11, Karen dissipated over Texas.

In the Leeward Islands, the system brought rainfall up to 300mm and flooding up to a meter high in Anguilla, the USVI, and the BVI. Despite this, there was no deaths reported. In the Greater Antilles there was rainfall up to 330mm in Puerto Rico and Hispaniola and 300mm in Cuba. Karen brought tropical storm force winds over Hispaniola and Puerto Rico and waves up to a meter high. In Cuba there was no major problems. Despite this, there was also no deaths. In the Bahamas, there was torrential rainfall and flooding up to 2 meters high. Despite this there was even not a single death reported. In Florida, mostly in the Florida Keys and South Florida, they were the hardest hit despite being a tropical depression, there was rainfall up to 400mm and flooding up to 2-3 meters high, mostly in the Florida Keys and in Miami and the Everglades. In the Gulf Coast, mostly in Texas and Louisiana, there was flooding from Lake Sabina an the Mississippi River and rainfall up to 300mm. Despite this, there was no deaths reported. The system caused $12 million (2019 USD) in all the areas it affected and damaged.

Hurricane Lorenzo (13L)
On February 25, a tropical wave exited West Africa. The wave did not organize until February 28, when the wave organized into Tropical Depression Thirteen, becoming the thirteenth depression of the season. The following day, March 1, the system strengthened into a tropical storm and given the next name on the list, Lorenzo, becoming the twelfth named storm of the season. The following day, March 2, the system strengthened and made its first landfall over Barbados with winds of 60 mph (95 km/h) and a pressure of 995 mbar. A few hours later, it strengthened once again and made its second landfall as a strong tropical storm with winds of 70 mph (110 km/h) and a pressure oh 992 mbar. The following day after landfall, March 3, the system emerged into the Caribbean Sea and shortly afterward, strengthened into a Category 1 hurricane, becoming the ninth hurricane of the season. The system underwent steady intensification, strengthening into a Category 2 hurricane the following day, March 4. The system rapidly intensified and reached major hurricane strength the following day, March 5. Shortly after reaching major hurricane strength, it reached its initial peak intensity with winds of 120 mph (195 km/h) and a pressure of 959 mbar. Shortly after reaching major hurricane status, Lorenzo underwent an eyewall replacement cycle, falling below major hurricane status to a Category 2 but regained major hurricane status later that day. It rapidly intensified, reaching its peak intensity, and made its third landfall over Hopkins, Belize at its peak on March 7. Shortly after reaching its peak intensity, it began to weaken steadily, falling below major hurricane status on the following day, March 8. Later that day, it emerged into the Bay of Campeche but despite this, upwelling caused the system to weaken even further into a Category 1 just before making its final landfall over Túxpam de Rodríguez Cano, Veracruz, Mexico on March 9. It began to rapidly weakened while moving further inland, degenerating into a remnant low on the following day, March 10. It was rapidly drawn to the north-northeast from a large, long extratropical cyclone, being absorbed by the cyclone the following day, March 11.

In the Lesser Antilles, there were tropical storm force winds, torrential rainfall up to 500mm, and flooding up to 2.5 feet high in Barbados, St. Lucia, Dominica, St. Vincent and the Grenadines, and Martinique, killing 16 people; 12 people direct due to drowning and 4 indirect due to a heart attack when all were trying to get to higher ground. In the Greater Antilles, Jamaica had tropical storm force winds rainfall up to 200mm but no flooding, killing 5 people; 3 direct due to high surf, 2 indirect due to flying debris. In the rest of the islands, there was high surf and rip currents, killing 6 people; all direct. In Belize, this was the hardest hit with major hurricane winds, rainfall up to 600.5mm and flooding up to 2.5-3.2 feet high, killing 10 people; 7 direct due to drowning, 3 indirect due to a building collapsing on them. In Guatemala, there was hurricane force winds, rainfall up to 512.4mm, and flooding a feet high, killing 1 person; indirect due to a building collapsing during the flood. In the rest of Central America, there were rip currents but no deaths reported. In Mexico, there was rainfall up to 300-400mm, hurricane force winds, and flooding up to 2.4 feet high, mostly in Veracruz, Yucatan, Campeche, Quintana Roo, and all the areas affected by the system, killing 6 people; all direct due to high surf in Veracruz, killing 4 and flooding in Campeche, killing 2 people. The system caused $1.45 million (2019 USD) in all the areas it affected and damaged.

Hurricane Melissa (14L)
On February 28, a tropical wave exited West Africa. Three days later, on March 3, the wave organized into Tropical Depression Fourteen, becoming the fourteenth depression of the season. Its movement was nearly stationary due to light steering currents and maintained its intensity for two days until March 5 when the system strengthened into a tropical storm and given the next name on the list, Melissa, becoming the thirteenth named storm of the season. Shortly after being upgraded to a tropical storm, Melissa's movement speed began to increase but it maintained its intensity for four days until March 9 when the system strengthened into a Category 1 hurricane, becoming the tenth hurricane of the season. It maintained its intensity as a minimal hurricane for two days until March 11, when it rapidly intensified, reaching Category 2 intensity early the following day, March 12. The following day, March 13, the system strengthened into a Category 3 major hurricane, becoming the tenth major hurricane of the season. Early the following day, March 14, Melissa reached Category 4 intensity. Shortly after reaching Category 4 intensity, it reached its initial peak intensity with winds of 130 mph (215 km/h) and a pressure of 939 mbar. Shortly after reaching its initial peak intensity, it weakened back to a Category 3 due to a brief eyewall replacement cycle but restrengthened into a Category 4 early the following day, March 15. Later the same day, Melissa reached its peak intensity. Later that day, also, Melissa underwent a second eyewall replacement cycle, falling back to Category 3 intensity early on March 16. When it finished the eyewall replacement cycle, it restrengthened back to a Category 4 again, reaching a secondary peak intensity with winds of 135 mph (215 km/h), the same winds at its peak but a higher pressure of 937 mbar, just 1 mbar higher than its minimum pressure later that day. Early the following day, March 17, it entered an area of moderate wind shear, falling back to Category 3 intensity for the final time. It continued to weaken, falling below major hurricane intensity to a Category 2 hurricane early on March 19. It maintained its intensity that day. The following day, Melissa regained major huricane strength. Melissa reached a fourth peak intensity with winds of 120 mph (195km/h) and a pressure of 949 mbar March 21. Melissa weakened slightly just before making landfall over the Savannah River with winds of 115 mph (185 km/h) and a pressure of 951 mbar later that day. Shortly after landfall, Melissa began to rapidly weaken while moving further inland. Two days after landfall, March 23, it became a remnant low. It dissipated over Arkansas the following day, March 24.

In the Bahamas, its outer edges brought strong winds and torrential rain in Nassau, Freeport, Grand Bahama, Great Abaco, and Nicholls and Congo Town, bringing flooding up to 1.5-2 meters high that killed 18 people; 5 direct from drowning, 13 indirect from diseases and car accidents. In Florida, its outer edges brought strong winds and also torrential rainfall up to 500mm, the heaviest in Fernandina Beach and Jacksonville. It also summoned a tornado outbreak that lasted from March 20-21, the highest being an EF3 tornado in Yulee with winds of 152 mph that killed 15 people; 3 direct by being blown away by an EF2 tornado and 12 direct by a collapsing building caused by the same EF2 tornado in Jacksonville Beach. There was a direct death from drowning from floods in Jacksonville. In Georgia and South Carolina, when the storm made landfall on March 21 over the Savannah River, its eyewall brought strong winds on both states, torrential rainfall up to 600mm, the heaviest in Savannah, Hilton Head Island, Richmond Hill, and Beaufort. Flooding up to 2.5 meters high killed 4 people; all direct. In Alabama, Louisiana, Mississippi, and Arkansas, there was strong winds in Alabama and Mississippi, heavy rainfall in all states with 400-500mm the highest in Montogomery, Alabama. In the rest, there was rainfall up to 300mm except for Arkansas. 40mm in Arkansas. The rest of the deaths were from flooding and diseases. The system caused $689 million (2019 USD) in all the areas it affected and damaged.

Hurricane Nestor (15L)
On March 1, a tropical wave exited West Africa. The wave continued to slowly organize while heading northwest. Six days later, on March 7, the wave organized into Tropical Depression Fifteen, becoming the fifteenth depression of the season. The following day, March 8, the system strengthened into a tropical storm and given the next name on the list, Nestor, becoming the fourteenth named storm of the season. It maintained its intensity for two days until March 10 when Nestor strengthened into a Category 1 hurricane, becoming the eleventh hurricane of the season. It rapidly strengthened and reached Category 2 intensity after maintaining its intensity for two days on March 12. Later that day, the system rapidly intensified into a Category 3 major hurricane becoming the eleventh major hurricane of the season. Nestor struggled to strengthened to a Category 4 and fluctated in strength due to moderate wind shear, maintaing its intensity for five days. On March 17, Nestor finally strengthened into a Category 4 hurricane since wind shear decreased. Later that day, Nestor reached its initial peak intensity with winds of 140 mph (220 km/h) and a pressure of 930 mbar. Nestor maintained its intensity for 12 hours. Early the following day, March 18, Nestor underwent an eyewall replacement cycle, weakening to a Category 3 on March 20. Despite the weakening, it maintained its initial minimum pressure. After completing the eyewall replcaement cycle, it restrengthened into a Category 4 hurricane and its initial minimum pressure started decreasing again. On March 24, it reached its peak intensity as a slow moving storm. After reaching its peak intensity, it moved over to cooler sea surface temperatures of up to 20-22 degrees Celsius. The following day, March 25, it underwent an eyewall replacement cycle, causing the sea surface temperatures to fall to 17-19 degrees Celsius, undergo extratropical transition, and rapidly weaken Nestor to a Category 1 hurricane. It became small due to high shear of up to 55-60 knots near Atlantic Canada, causing the system to have its size shrunk to a small storm, just before making landfall over Metaghan, Nova Scotia with winds of 80 mph (130 km/h) and a pressure of 971 mbar on March 28. Shortly after landfall, it completed extratropical transition. It rapidly weakened into a post-tropical depression just before heading to the north into the Gulf of St. Lawrence. While in the gulf, its movement was nearly stationary and moved north. On April 1, it moved ashore Anticosti Island just before its remnants were absorbed by an extratropical cyclone after moving ashore later that day.

In Bermuda, there was hurricane-force winds of 82-84 mph (130 km/h), torrential rainfall up to 400mm and a storm surge of 2-3.5 feet in coastal areas. There was also 3 tornadoes reported in St. George's, the highest being an EF2 with winds of 116 mph (185 km/h). Despite this, there were no deaths reported. In the US East Coast, there were rip currents in Georgia and South Carolina. In North Carolina, Virginia, and the Delmarva Peninsula, its outer edges brought heavy rainfall and flooding up to 4 meters high, and a tornado was reported in Wilmington, EF0, winds of 75 mph (120 km/h). In New Jersey, Rhode Island, Connecticut, Massachusetts, New Hampshire, and Maine, its eyewall brought Category 4-equivalent winds, rainfall up to 700mm, and flooding up to 4.5 meters high. Despite this, there were no deaths reported in all states. In Atlantic Canada, there was Category 1-equivalent winds in the western part of Nova Scotia and tropical storm force winds in the rest of the province. In Newfoundland, Prince Edward Island, and Quebec, there was rainfall up to 200mm and storm surge up to 2.5 meters high. Despite this there were also no deaths reported. The system caused $928.67 million (2019 USD) in damages in all the areas it affected and damaged.

Tropical Depression Sixteen (16L)
On March 7, two tropical waves exited West Africa, one large, one small. The waves were separated from a high pressure area between them on the following day, March 8.The larger one developed into a tropical depression on March 13 that brushed Western Cuba. The smaller wave continued to head west with slow development due to wind shear of 10-15 knots. On March 10, the smaller wave entered the Caribbean Sea. The following day, the smaller wave organized into Tropical Depression Sixteen south of Hispaniola. Shortly after formation, it reached its peak intensity. It maintained its peak intensity until it made landfall over the Dominican Republic. Shortly after landfall, it degenerated into a remnant low. Despite this, it made a second landfall over the Tiburon Peninsula in Haiti. The system turned to the west and brushed Jamaica and Cuba. While brushing them, the larger wave entered the Caribbean Sea at a fast speed on March 13 and absored the remnants later that day.

In Hispaniola, there was rainfall up to 100mm and flooding in the island, killing a woman in Haiti. In both Jamaica and Cuba, there was the same amount of rainfall in Hispaniola but no deaths and flooding reported. The system caused $5,100 (2019 USD) in all the areas it affected and damaged.

Tropical Depression Seventeen (17L)
As it was said in Section 2.16, there were two tropical waves that left West Africa on March 7. The one above was the small one. This one is the large tropical wave. This is just brief information. The full info is at Section 2.16 in this page. The largest one continued westward and its movement accelerated while moving closer to the Lesser Antilles and encountered unfavorable conditions. On March 13, it entered the Caribbean Sea and its movement started slowing down due to decreasing shear. Later that day, the wave organized into Tropical Depression Seventeen. Shortly after formation, it absorbed the remnants of the smaller tropical depression that brushed Hispaniola, Cuba, and Jamaica and reached its peak intensity. Soon after reaching its peak intensity, its winds fell to 30 mph (50 km/h). It maintained its strength until it made landfall over Western Cuba on March 15. Later that day, it degenerated into a remnant low just before dissipating the following day, March 16.

In the Cayman Islands, it brought torrential rainfall and flash flooding. Despite this, there were no deaths reported. In Cuba, the tropical depression grazed the Western Coast hardest as it brought the highest rainfall and flash flooding from the storm (in Isla de la Juventud). No deaths were also reported. The system caused minimal damage.

Tropical Storm Olga (18L)
On March 10, a tropical wave left West Africa. The system slowly organized as it crept closer to the Bahamas and six days later, on March 16, the wave organized into Tropical Depression Eighteen, becoming the eighteenth depression of the season. Twelve hours later, the depression strengthened into a tropical storm and given the next name on the list, Olga, becoming the fifteenth named storm of the season. Shortly after reaching tropical storm intensity, it reached its initial peak as a minimal tropical storm and increasing wind shear weakened the system into a tropical depression just before making its first landfall over the Bahamas with winds of 35 mph (55 km/h) and a pressure of 1003 mbar on the following day, March 17.The following day again, March 18, the system made its second landfall in South Florida with winds of 30 mph (45 km/h) and a pressure of 1005 mbar. Early the following day, March 19, it emerged in the Gulf of Mexico. Shortly after emerging into the gulf, wind shear relaxed, allowing the system to restrengthen into a tropical storm the following day, March 20. At 06:00 UTC the following day, March 21, Olga reached its peak intensity. Olga maintained its peak intensity for 24 hours until the following day, March 22, when moderate southerly wind shear of 20 knots displaced the system's convection to the north, exposing the southern part of the low level circulation center. The the following day at 12:00 UTC, March 23, Olga made its third and final landfall over Galveston Island and Texas City both in Texas. Shortly after landfall, it experienced the brown ocean effect, a phenomenon when a system maintains its structure and intensity over land due to saturated soil conditions. However, the phenomenon was short lived, when the system degenerated rapidly into a remnant low in just 24 hours after it happened. The remnants dissipated early the following day, March 25.

In the Bahamas, Olga brought tropical storm winds of 38 mph (61 km/h), the minimum of tropical storm winds, rainfall up to 10-11 inches, but no flooding. Despite this, there were no deaths reported. In the United States, Florida and the Gulf Coast were the hardest hit, with 60 mph (96 km/h) winds in the Gulf Coast and torrential rainfall and flooding in both Florida and the Gulf Coast. No deaths were also reported. The system caused $129,000 (2019 USD) in all the areas it affected and damaged.

Hurricane Pablo (19L)
On March 18, a tropical wave exited West Africa. It rapidly organized while heading west-northwestwards at a speed of 10 mph (16 km/h). Early the following day, March 19, the wave organized into Tropical Depression Nineteen. The tropical depression slowly strengthened due to sea surface temperatures of 26 degrees Celsius. It maintained its intensity for two days until March 21 at 18:00 UTC when the system strengthened into a tropical storm and given the next name on the list, Pablo, becoming the sixteenth named storm of the season. It slowly strengthened and maintained its intensity for five days until it briefly strengthened into a Category 1 hurricane, its first peak, with winds of 74 mph (120 km/h), becoming the twelfth hurricane of the season. Six hours after reaching hurricane strength, outflow from Hurricane Nestor, weakened Pablo back to a strong tropical storm. However, again, six hours later, Pablo restrengthened back into a Category 1 hurricane. Finally, Pablo rapidly strengthened and grew a regular eye. On March 28 at 12:00 UTC, Pablo strengthened into a Category 2 hurricane. Twelve hours later, the system strengthened into a Category 3 major hurricane, becoming the twelfth major hurricane of the season. The following day, on March 29 at 24:00 UTC, Pablo strengthened even further into a Category 4 hurricane. On April 1 at 12:00 UTC, Pablo reached its initial peak intensity with winds of 145 mph (230 km/h) and a pressure of 930 mbar. On April 2 at 24:00 UTC, Pablo underwent its first eyewall replacement cycle, weakening into a Category 3 major hurricane on April 3. Early the following day, April 4, Pablo reintensified back to a Category 4 major hurricane. The following day, April 5 at 18:00 UTC, Pablo reached its peak intensity. Early the following day, April 6, Pablo underwent its second eyewall replacement cycle, weakening into a Category 3 major hurricane for the second time at the same day at 12:00 UTC. It maintained its intensity for two days until April 8 at 12:00 UTC, when the system restrengthened back to a Category 4 major hurricane for the final time, reaching its secondary and final peak intensity with winds of 130 mph (216 km/h). Shortly after reaching its secondary peak, it underwent its third and final eyewall replacement cycle, falling to a Category 3 major hurricane for the final time just twelve hours later. Shortly after finishing the eyewall replacement cycle, Pablo entered an area of cooler sea surface temperatures of 20-21 degrees Celsius and strong wind shear of 30-35 knots. Despite this, Pablo maintained its intensity for two days until early on April 11, when cooler sea surface temperatures and strong wind shear finally took toll on the system, weakening the system to a Category 2 hurricane. It maintained its intensity for two days until early on April 13, when Pablo weakened even further to a Category 1. Soon afterward, it begun extratropical transition and its eye became cloud-filled. Later that day, Pablo made landfall over Southwest Harbor, Maine with winds of 90 mph (146 km/h) and a pressure of 970 mbar. The following day after landfall, at April 14, 00:01 UTC, Pablo finished extratropical transition. Despite this it summoned a tornado outbreak with in Maine, New Brunswick, Quebec, and Labrador on April 16-19. It dissipated on April 21 over Labrador.

In Bermuda, there were tropical storm force winds of up to 65 mph (101 km/h) and gusts up to 75 mph (120 km/h), flooding up to 2 meters high, and waves up to 6 meters high, killing 2 people. In the United States East Coast, Maine was the hardest hit, with hurricane force winds up to 87 mph (147 km/h), flooding up to 2 meters high, and storm surge up to 3 meters high, bringing coastal flooding, killing 10 people; 1 direct due to drowning, and 9 indirect due to a building collapsing on them. In Canada, Nova Scotia had tropical storm winds of up to 62 mph (96 km/h) and flooding but no deaths reported. In its extratropical phase, Maine, New Brunswick, Quebec, and Labrador, had a tornado outbreak with 40 tornadoes reported, the highest being an EF4 with winds of 176 mph (282 km/h) in Sept-Iles, Quebec. The rest of the deaths were caused by the tornado outbreak in all four affected areas. The system caused $314 million (2019 USD) in all the areas it affected and damaged.

Tropical Depression Twenty (20L)
On March 16, a tropical wave moved off West Africa, it continued towards the northwest encountering unfavorable conditions. However while it approached the Bahamas on March 22, a high pressure area over the United States East Coast turned it to the west, encountering favorable conditions. The following day, however, March 23, the wave made landfall over Florida. Despite this, it continued to organize. Finally on March 24, the wave organized into Tropical Depression Twenty, becoming the twentieth depression of the season. Six hours later, it emerged into the Gulf of Mexico and strengthened slightly, reaching its peak intensity. It maintained its peak intensity until the following day, March 25 at 12:00 UTC, when the system encountered increasing wind shear began taking toll on the system. It maintained its intensity until the following day, March 26, at 24:00 UTC, when it degenerated into a remnant low. Despite this, it made landfall over Freeport, Texas early on March 27. It dissipated later that day at 24:00 UTC.

In both Florida and the United States Gulf Coast, the system brought torrential rainfall and flash flooding, killing one person directly. 5 indirect deaths were due to the car being swept in the Mississippi River. Only one person survived. The system caused $1 million (2019 USD) in all the areas it damaged.

Hurricane Rebekah (21L)
On March 27, an area of disturbed weather formed off the coast of Veracruz in the Bay of Campeche. It rapidly organized and at 06:00 UTC the following day, March 28, the area of dsturbed weather organized into Tropical Depression Twenty-one, becoming the twenty-first depression of the season. Later that day, the tropical depression made its first landfall near Campeche, Campeche at 14:00 UTC with winds of 35 mph (55 km/h) and a pressure of 1000 mbar. It moved out into sea at 24:00 UTC on the same day at its first landfall. 24 hours later, the system strengthened into a tropical storm and given the next name on the list, Rebekah, becoming the seventeenth named storm of the season. It maintained its intensity for four days until April 2 at 12:00 UTC when Rebekah rapidly intensified into a Category 1 hurricane, becoming the thirteenth hurricane of the season. The system rapidly strengthened even further into a Category 2 hurricane in just six hours. The following day, April 3 at 18:00 UTC, Rebekah intensified into a Category 3 major hurricane, becoming the seventeenth major hurricane of the season. Twelve hours later, April 4 at 06:00 UTC, it intensified even further into a Category 4 major hurricane. Shortly after reaching Category 4 intensity, Rebekah reached its peak. It maintained its intensity until the following day 18:00 UTC, April 5, when the system underwent an eyewall replacement cycle, weakening into a Category 3 major hurricane. Despite the weakening, the wind field expanded. Early the following day, April 6, Rebekah made its final landfall over Apalachicola in the Florida Panhandle. Despite landfall, it maintained its intensity for 24 hours when early the following day, April 7, Rebekah weakened into a Category 2 hurricane, below major hurricane strength. Again, it maintained its intensity until 12:00 UTC the following day, April 8, when the system weakened even further to a Category 1 hurricane. It maintained its intensity, again, for 24 hours until the following day, April 9, when Rebekah fell below hurricane intensity to tropical storm intensity. The following day, April 10, the system weakened into a tropical depression. Early the following day, April 11, Rebekah degenerated into a remnant low. It dissipated later that day at 18:00 UTC.

In Mexico, the precursor and the system in its tropical depression stage dumped torrential rainfall up to 16-20 inches in Veracruz, Puebla, Oaxaca, Tabasco, Chiapas, Campeche, and the Yucatán Peninsula, killing 10 people; 6 direct due to drowning, 4 indirect due to a building buit of light materials collapsing on all 6 people. Only 3 survived. The rest died. In the United States Gulf Coast, the Florida Panhandle was the hardest hit with winds of 119 mph (184 km/h) reported in the areas affected by the eyewall, rainfall of 22-23 inches in the entire Panhandle except Panama City where rainfall was up to 21 inches. In the rest of the US Gulf Coast, Alabama received 19 inches of rain, Mississippi received 16-17 inches of rainfall and Louisiana received 3 inches of rainfall. There were hurricane force winds in Florida, Alabama, and Mississippi while Louisiana had tropical storm force winds. There was flooding 3 feet high in Florida while the rest had 2 feet high flooding, killing 54 people; 15 direct due to high surf and 41 indirect due to building collapses in Mississippi, Alabama, and Florida, and diseases like measles in Louisiana. In Georgia and the Carolinas. Georgia and South Carolina received 15 inches of rainfall while North Carolina received 0.9 inches of rainfall. There were hurricane force winds in Georgia and tropical storm force winds in South Carolina. There was a tornado outbreak that killed 11 people in Georgia and South Carolina. The highest was an EF2 tornado in St. George, South Carolina with winds of 123 mph (200 km/h). The system caused $1.23 billion (2019 USD) in all the areas it affected and damaged.

Hurricane Sebastien (22L)
On April 1, an area of disturbed weather formed about 30 nautical miles off the west coast of Costa Rica in the Northeast Pacific Ocean. It initially tracked northwest at 9 knots but tracked north and east-northeast in just under six hours at a speed of 11 knots. An hour after changing course, the disturbance made its first landfall over El Tránsito, Nicaragua at 19:00 UTC on the same day after formation it continued its northeast track until a high pressure area spawned over Cuba, causing the disturbance to track south on 22:00 UTC on the same day and west-southwest on April 2 at 00:00 UTC. Two hours later, it emerged back out into sea. Four hours later, the disturbance turned westward. Later that day at 18:00 UTC, it moved west-northwest. However, the system turned north and moved slowly on April 3 at 00:00 UTC due to a building ridge in the southernmost part of the Gulf of California. However, at 13:00 UTC it started its long-lived northeast movement. Shortly after moving northeast it attained gale-force winds but still remained a disturbance due to moderate wind shear of 20 knots. On April 4 at 18:00 UTC, it emerged in the Gulf of Tehuantepec. On April 5 at 01:10 UTC, it made its second landfall over Aguachil, Oaxaca, Mexico. It still maintained gale-force winds despite land interaction. Early on April 6, it emerged in the Bay of Campeche in the Atlantic Ocean. Shortly after emerging in the Bay of Campeche it lost gale-force winds but organized into Tropical Depression Twenty-two six hours later, becoming the twenty-second depression of the season. Due to its close proximity to land, it slowly strengthened. It maintained its intensity for three days until April 9 at 14:00 UTC when the depression intensified into a tropical storm north of Quintana Roo and given the next name on the list, Sebastien, becoming the eighteenth named storm of the season. It slowly strengthened due to wind shear of 15-25 knots and took a long-lived east-northeast movement. Early on April 13, Sebastien made its third landfall; first landfall as a tropical system between Nokomis and Venice and it reached its initial peak intensity at the same time with winds of 73 mph (117 km/h), just below hurricane strength. Early the following day, April 14, Sebastien emerged into the Atlantic Ocean. Despite this it weakened to winds of 53 mph (88 km/h). However, at 00:00 UTC the following day, April 15, the system started restrengthening slowly. Finally, on April 17 at 18:00 UTC, Sebastien intensified into a Category 1 hurricane, becoming the fourteenth hurricane of the season. It maintained minimal hurricane intensity for 18 hours until it begun rapidly intensifying. On April 20 at 06:00 UTC, Sebastien intensified even further into a Category 2 hurricane. The following day, April 21 at 18:00 UTC, Sebastien reached Category 3 major hurricane intensity, becoming the fourteenth major hurricane of the season. On April 23 at 19:25 UTC, the system intensified even further into a Category 4 major hurricane. Early the following day, April 24, Sebastien reached its peak intensity. On April 25 at 23:50 UTC, Sebastien underwent an eyewall replacement cycle, weakening briefly into a Category 3 but reintensfied back into a Category 4 at 03:00 UTC. Shortly after restrengthening into a Category 4, it reached its secondary peak intensity, with winds of 133 mph (213 km/h). However a second eyewall replacement cycle weakened Sebastien back into a Category 3 major hurricane. Sebastien maintained its intensity until May 7 when increasing wind shear, decreasing sea surface temperatures, and a final eyewall replacement cycle weakened the system into a Category 2 hurricane. The following day, May 8, it weakened even further into a Category 1 hurricane. On May 10, Sebastien made its fourth landfall; final tropical landfall over Fanore, Ireland with winds of 86 mph (140 km/h). Shortly after landfall, it became extratropical. It still had hurricane force winds but on May 11, it weakened to an extratropical storm. On May 12, it made its fifth landfall; first post-tropical landfall over Lake District National Park with winds of 64 mph (100 km/h). Later that day, it emerged into the North Sea and continued weakening. On May 15, it made its final landfall and post-tropical landfall over Kristiansand, Norway. It rapidly dissipated later that day.

In Central America, the precursor dumped heavy rainfall over Nicaragua, Guatemala, Honduras, Costa Rica, and Belize, bringing flooding that killed 2 people directly. In Mexico the precursor and tropical depression dumped more rainfall than in Central America over Chiapas, Oaxaca, Guerrero, Puebla, Veracruz, Tabasco, and the Yucatan Peninsula, killing 10 people; 6 direct, 4 indirect. In America, Florida had gale-force winds and major flooding that killed 11 people; 5 direct, 6 indirect. On the US East Coast, Sebastien brought rip currents that killed 3 people directly. In Atlantic Canada, Nova Scotia and Newfoundland had hurricane force winds that killed 2 people directly. In Europe, Ireland was the hardest hit, as hurricane force winds hit the nation in which the rest of the deaths were from flooding. In the rest of the European countries affected (United Kingdom had gale force winds while the British Isles, France, Belgium, Netherlands, Norway, Sweden, and Denmark had just heavy rainfall. The system caused $678 million (2019 USD) in all the areas it affected and damaged.

Tropical Storm Tanya (23L)
On March 31, a tropical wave exited West Africa. Shortly after exiting West Africa, the wave turned northwest, slowly organizing despite moderate wind shear. On April 6 at 18:00 UTC, the wave organized into Tropical Depression Twenty-three, becoming the twenty-third depression of the season. Six hours later, it strengthened into a tropical storm and given the next name on the list, Tanya, becoming the nineteenth storm of the season despite increasing wind shear. Tanya then rapidly strengthened and on April 9 at 07:25 UTC, Tanya peaked with winds of 71 mph (112 km/h). Shortly after peak intensity, increasing wind shear finally took toll on Tanya and the system weakened into a tropical depression on April 12 at 13:00 UTC. It had maintained tropical depression intensity for three days as wind shear slowly decreased until April 15 at 23:45 UTC when the system restrengthened into a tropical storm. Shortly after being upgraded to a tropical storm, it interacted with the larger Sebastien but did not weaken or get absorbed by the larger storm. On May 19 at 03:00 UTC, Tanya reached a secondary peak intensity with the same wind speeds at its peak but a higher pressure of 995 mbar. Shortly after reaching its secondary peak, decreasing sea surface temperatures and increasing wind shear began to take toll on the system again, causing a weakening trend. Finally, on April 21 at 16:30 UTC, Tanya weakened into a tropical depressiona again. At 00:00 UTC on April 23, Tanya degenerated into a remnant low. It dissipated the following day, April 24.

In North Carolina and the Delmarva Peninsula, its outer edges killed 1 person in North Carolina due to flooding. The system caused minimal damage only.

Hurricane Van (24L)
On April 5 at 00:00 UTC, a trough of low pressure formed off the coast of Nicaragua. An hour later, it made landfall over Krukira, Nicaragua. Despite landfall, it continued to organize. On the same day at 18:00 UTC, it reemerged back out at sea and turned north. However, twelve hours later, on April 6 at 00:00 UTC, a binary interaction with the precursor of Sebastien started. The disturbance moved west-northwest and made 4 landfalls in Mexico; Banco Chinchorro on April 6 at 09:00 UTC, Puerto Bravo, Quintana Roo on the same day at 12:00 UTC, Isla del Carmen, Campeche on April 7 at 12:00 UTC, and Isla Aguada, Campeche on the same day at 18:00 UTC. On April 7, the disturbance organized into Tropical Depression Twenty-four, becoming the twenty-fourth depression of the season. It still interacted with the newly formed Tropical Depression Twenty-two, delaying intensification but on April 10 at 06:00 UTC, the system strengthened into a tropical storm and given the next name on the list, Van, becoming the twentieth named storm of the season. The following day, April 11, at 23:00 UTC, Van intensified into a Category 1 hurricane, becoming the fifteenth hurricane of the season. Two days later, on April 13 at 00:00 UTC, the system intensified even further into a Category 2 hurricane. Later that day, at 20:00 UTC, Van intensified further into a Category 3 major hurricane, becoming the fifteenth major hurricane of the season. The following day, April 14, at 07:00 UTC, Van strengthened rapidly into a Category 4 major hurricane. The following day, April 15, at 19:00 UTC, Van reached its peak intensity. The following day, April 16, at 15:00 UTC, Van made its final landfall; only tropical landfall over Largo, Florida with winds of 147 mph (236 km/h) and a pressure of 929 mbar. Despite landfall, it maintained its intensity while moving further inland due to a phenomenon known as the "brown ocean effect". Two days later, on April 18, Van finally weakened into a Category 3 major hurricane just before moving offshore later that day. It maintained its intensity for four days until April 22 when Van briefly restrengthened into a second peak intensity as a Category 4 with winds of 130 mph (215 km/h) and a pressure of 937 mbar. Shortly after reaching its second peak intensity and eyewall replacement cycle and increasing wind shear weakened Van to a Category 3 in just six hours. The following day, April 23 at 00:00 UTC, Van weakened into a Category 2 hurricane, falling below major hurricane intensity. The following day, April 24, at 06:00 UTC, Van weakened even further into a Category 1 hurricane. Three days later, on April 27 at 06:00 UTC, Van restrengthened into a Category 2 hurricane. On April 28, Van reintensified even further into a Category 3 major hurricane, regaining major hurricane strength. On May 2, Van restrengthened into a Category 4 major hurricane. Van weakened into a Category 3 and restrengthened to a Category 4 three times. On May 6, Van restrengthened back into a Category 4 for the final time. Later that day, it rapidly weakened to a Category 2, falling below major hurricane strength. The following day, May 7 at 00:00 UTC, Van weakened even further into a Category 1 hurricane. Six hours later, the system became extratropical. The extratropical remnants dissipated on May 9, southeast of Newfoundland.

In Central America, the precursor dumped heavy rainfall in Guatemala, Belize, Nicaragua, and Honduras, kiling 17 people; 8 direct due to drowning, 9 indrect due to a building collapse. In Mexico, when its was in tropical depression and precursor stage, the system dumped torrential rainfall, along with the precursor of Sebastien in the Northeastern East Pacific which brought high flooding in Quintana Roo, Yucatan, Campeche, Tabasco, Chiapas, Veracruz, and Puebla, killing 10 people; 4 direct, 6 indirect. In Florida, this was the hardest hit bringing Category 4-equivalent winds and rainfall up to 30-33 inches in West Florida and flooding of 4 meters high which killed 70 people; 35 direct; 35 indirect. In the Gulf Coast, large swells killed 3 people indirectly. In the East Coast rip currents killed 7 people indirectly due to house collapse. In Bermuda and Atlantic Canada, there was only minimal damage and no deaths. The system caused $2.3 billion (2019 USD) in all the areas it affected and damaged.

Hurricane Wendy (25L)
Wendy was the first of five storms that failed to reach major hurricane intensity. On April 12, Tropical Depression Twenty-five formed with a complex origin having originated from several tropical waves and a non-tropical low heading southwest towards a low latitude and interacting with the waves. It had maintained tropical depression intensity for two days until April 14, when the tropical depression intensified into a tropical storm and was given the final name on the list, Wendy, becoming the twenty-first named storm of the season. Wendy started slowly strengthening. Five days later, on April 19 at 00:00 UTC, Wendy strengthened into a Category 1 hurricane, becoming the sixteenth hurricane of the season. The following day, April 20, Wendy reached its peak intensity. Early the following day, Wendy rapidly weakened to a tropical storm and became extratropical. The extratropical remnants affected the Canary Islands, Azores, and Madeira before dissipating on May 2.

There was no areas affected in its tropical stage but in its extratropical stage, Wendy affected the Canary Islands, Azores, and Madeira but brought light rainfall and caused minimal damage.

Hurricane Alpha (26L)
On April 18, a slow-moving tropical wave moved off West Africa. Five days later, April 23 at 06:00 UTC, the wave organized into Tropical Depression Twenty-six, becoming the twenty-sixth named storm of the season. The following day, April 24, the newly formed system intensified into a tropical storm and given the first name on the Greek list, Alpha, since all the names of the 2019 season were exhausted, becoming the twenty-second named storm of the season. Five days later, Alpha strengthened into a Category 1 hurricane, becoming the seventeenth hurricane of the season. Alpha slowly strengthened and on May 1 at 17:00 UTC, Alpha intensified into a Category 2 hurricane. Two days later, on May 3 at 20:30 UTC, the system strengthened into a Category 3 major hurricane becoming the sixteenth major hurricane of the season. Three days later, on May 6, Alpha strengthened even further into a Category 4 major hurricane. During its nearly 2 week Category 4 stage, it fluctated in strength several times. However, on May 17, Alpha finally intensified into a Category 5 major hurricane. Later that day, Alpha reached its initial peak intensity with winds of 159 mph (258 km/h) and a pressure of 914 mbar. However, it underwent the first of five eyewall replacement cycles, falling to a Category 4 but its pressure slightly increased to 918 mbar. The following day, May 18, Alpha had reintensified into a Category 5 major hurricane. Early the following day, May 19, Alpha reached its second peak with winds of 161 mph (263 km/h) and a pressure of 909 mbar. It underwent a brief eyewall replacement cycle, the second of five, briefly weakening to a Category 4. Six hours later, Alpha had restrengthened to a Category 5 again. The following day, May 20, Alpha reached its peak intensity. It reached its longest Category 5 duration in its lifetime. After reaching its peak intensity, it underwent the third of five eyewall replacement cycles, falling to a Category 4 for the third time. The following day at 05:00 UTC, Alpha regained Category 5 status for the final of four times. It reached a secondary peak intensity with winds of 159 mph (259 km/h) and a pressure of 907 mbar. It underwent the fourth of five eyewall replacement cycles, falling to a Category 4 for the final time. It began to undergo a weakening trend due to slowly decreasing sea surface temperatures. On May 25, it underwent the final of five eyewall replacement cycles, causing the system to rapidly weaken to a Category 1 on the same day due to a rapid decrease of sea surface temperatures. Early the following day, it rapidly weakened into a tropical storm and became extratropical six hours later. The extratropical storm dissipated the following day, May 27.

In Bermuda, there was only large swells but there were no deaths. In Atlantic Canada, mostly in Newfoundland, there was huge amount of rainfall even in its extratropical stage and tropical storm force winds causing huge damage but also no deaths. The system caused $32 million (2019 USD) in all the areas it affected and damaged.

Tropical Storm Beta (27L)
On April 17, a tropical wave exited West Africa. A week passed and it emerged into the Gulf of Mexico on April 24. The following day, April 25 at 18:00 UTC, the wave organized into Tropical Depression Twenty-seven becoming the twenty-seventh depression of the season. The following day, April 26, the depression strengthened into a tropical storm and given the next name on the Greek list, Beta, becoming the twenty-third named storm of the season. The pressure slowly decreased and two days later, April 28 at 17:00 UTC, Beta reached its peak intensity. Shortly after reaching its peak intensity, it encountered dry air. It seemed small at first but began to increase as it began to approach the Gulf Coast. The following day, April 29, Beta weakened into a tropical depression. Early on May 2, Beta made landfall near Gulfport, Mississippi with winds of 30 mph (45 km/h) and a pressure of 1006 mbar. Later that day, it degenerated into a remnant low. The remnants dissipated the following day, April 23 over Louisiana.

The only area affected was the Gulf Coast of the United States where there was briefly tropical storm force winds. There was also heavy rainfall in parts of Mississippi and Louisiana. The western part of the Florida Panhandle was also affected with heavy rainfall up to 4.65 inches and flooding up to 2-3 meters high but no deaths. In both Mississippi and Louisiana encountered 5-6 inches of rainfall but no flooding in Louisiana. In Mississippi, Lake Pontchartrain had its water level risen but no deaths reported also. The system caused $875,000 (2019 USD) in all the areas it affected and damaged.

Tropical Depression Twenty-eight (28L)
On May 1, a disturbance detached from the Intertropical Convergence Zone (ITCZ). Between 12:00 UTC and 18:00 UTC, the disturbance moved eastwards due to a bulding ridge in the Bay of Campeche. The following day, May 2, at 00:00 UTC, it moved northeast towards Cuba. The following day, May 3, at 00:00 UTC, the disturbance organized into Tropical Depression Twenty-eight, becoming the twenty-eight depression season. The following day, May 4, it made its first landfall near Playa Dayaniguas, Cuba with winds of 30 mph (45 km/h) and a pressure of 1012 mbar. Later that day, it emerged into the Straits of Florida. The following day, May 5, the system reached its peak intensity. It was expected to strengthen into a tropical storm but increasing wind shear took toll on the system. The following day, May 6, the system made its second landfall over Vaca Key in the Florida Keys with winds of 30 mph (45 km/h) and a pressure of 1010 mbar. The following day, May 7 it made its third landfall over Everglades National Park, Florida with winds of 30 mph (45 km/h) and a pressure of 1011 mbar. Later that day, it degenerated into a remnant low. On May 9, it made its final landfall as a remnant low over West End, Grand Bahama. It dissipated the following day, May 10, over Great Abaco.

In Central America, Belize and Honduras were affected by the precursor dumping heavy rainfall, killing 10 people; 5 direct, 5 indirect. In Cuba, the depression dumber 5.75-6 inches of rainfall in Western Cuba, bringing high flooding killing 13 people; all directly. In Florida, the Florida Keys were the hardest hit and also the Everglades, bringing 5.50 inches of rainfall in all areas, killing 5 people; all directly due to flooding. In the Bahamas, its remnants dumped torrential rainfall in Grand Bahama and Great Abaco, killing one person directly. The system caused $8.3 million (2019 USD) in all the areas it affected and damaged.

Hurricane Gamma (29L)
On May 4, a tropical wave left West Africa. Later that evening, the wave organized into Tropical Depression Twenty-nine becoming the twenty-ninth depression of the season. It was moving nearly stationary but the following day, May 5, at 07:00 UTC, it turned northwest due to a building ridge southwest of Cape Verde. Intensification was expected but instead, increasing wind shear and drier air began to take toll on the system. Three days later, on May 8, at 08:00 UTC, Twenty-nine made its closest approach to Cabo Verde. The following day, May 9, at 06:00 UTC, Twenty-nine degenerated back into a tropical wave. The STCC expected the remnants to dissipate, despite not even strengthening into a tropical storm. However, wind shear and dry air began to decrease, allowing convection to redevelop. Two days later, May 11, at 06:00 UTC, the remnants of Twenty-nine reorganized into a tropical depression. Intensification was slow due to marginally favorable conditions. Four days later, on May 15, the system strengthened into a tropical storm and given the next name on the Greek list, Gamma, becoming the twenty-fourth named storm of the season. A week later, on May 22, at 12:00 UTC, Gamma strenghented into a Category 1 hurricane, becoming the eighteenth hurricane of the season. Gamma had remained at Category 1 intensity for nearly a week until May 27, when Gamma intensified into a Category 2 hurricane at 23:00 UTC. The following day, May 28, at 06:00 UTC, Gamma weakened back into a Category 1 hurricane but restregnthened into a Category 2 hurricane just six hours later at 12:00 UTC. It reached its initial peak intensity with winds of 97 mph (154 km/h) and a pressure of 968 mbar at both its initial and second peak intensities. It weakened to a Category 1 for the final time and restrengthened to a Category 2 in just under six hours. Five days later, June 2, at 06:00 UTC, Gamma intensified into a Category 3 major hurricane, becoming the seventeenth major hurricane of the season. Three days later, on June 5, Gamma intensified even further into a Category 4 major hurricane and reached its peak intensity shortly afterward. However, six hours later that day, the system weakened to a Category 3 major hurricane due to an eyewall replacement cycle. It had maintained Category 3 intensity. Models expected rapid weakening and extratropical transition in just 4-5 days but abundant moisture caused the system to persist and maintain its intensity. A week later, on June 13, Gamma finally weakened to a Category 2 hurricane as it began extratropical transition. The following day, June 14, Gamma weakened even further into a Category 1 hurricane and became extratropical six hours later. The remnants dissipated on June 17.

In West Africa, mostly in Sierra Leone, Guinea, and Guinea-Bissau were all affected by heavy rainfall by the precursor and tropical depression stage but no deaths reported. In Cabo Verde, rainfall up to 10.34-11 inches were dumped in the western part of the archipelago but also no deaths reported. In the Azores, tropical storm force winds were experienced and also storm surge up to 4-5 feet in the northernmost areas of the region, killing 1 person indirectly. In Ireland, there were rip currents in the western coast of the country and in extratropical transiton, the frontal system dumped the country heavy rainfall but even no deaths reported. The system caused minimal damage.

Tropical Storm Delta (30L)
On May 6, a tropical wave left West Africa. Five days later, on May 11, the wave organized into Tropical Depression Thirty at 18:00 UTC, becoming the thirtieth depression of the season. It was initially moving stationary for the first 18 hours but the following day, May 12 at 06:00 UTC, the movement accelerated due to steering currents in the area. Thirty had no change in intenisty and two days later, on May 14, the depression briefly degenerated into a tropical wave due to dry air. Six hours later, it briefly regenerated into a tropical depression just before making its first landfall over Playa de los Muetros, Cuba. It degenerated into a remnant low. The system changed course by heading northwest. This happens to some storms while overland or near land. The following day, May 15, at 06:00 UTC, the remnants emerged back out into sea and regenerated into a depression for the second time. It was expected to continue northwest and strengthen to a tropical storm and hit Florida, Georgia, and South Carolina but a high pressure area over the United States caused it to head southwest, making landfall near Cayo Conuco, Cuba with winds of 30 mph (45 km/h) and a pressure of 1008 mbar. It degenerated into a remnant low on the same day, six hours later, at 12:00 UTC. It had remained a remnant low for 18 hours until it emerged into the Gulf of Mexico, where it reorganized into a tropical depression, again on the following day, May 16, at 12:00 UTC. The following day, May 17, at 12:00 UTC, the depression strengthened into a tropical storm and given the next name on the Greek list, Delta, becoming the twenty-fifth named storm of the season. The following day, May 18, Delta reached its peak intensity. Later that day, Gamma entered an area of slowly declining sea surface temperatures as it continued moving west-northwest. Movement also started to slow down as it approached the western Gulf Coast. On May 19, at 18:00 UTC, Delta made its final landfall over Port Mansfield, Texas with winds of 45 mph (75 km/h) and a pressure of 1001 mbar. The following day, May 20 at 00:00 UTC, Delta weakened into a tropical depression. Later that day, at 12:00 UTC, it degenerated into a remnant low. It dissipated the following day, May 21 over Coahuila, Mexico. In the Leeward Islands, there was torrential rainfall from the system, mostly up to 10.30-11.01 inches in St, Kitts and Nevis, Anguilla, USVI, and BVI but no deaths were reported. In the Greater Antilles, the worst of the storm was in Cuba, with rainfall up to 12-13 inches in the northern areas. Puerto Rico and Hispaniola were also hit but it was not the worst with rainfall up to 11.40 inches. In the Bahamas, Grand Bahama was the only one affected by the storm with just intense rainfall but also no deaths. In the United States Gulf Coast, this was the hardest hit, mostly in Texas with torrential rainfall in Texas and Louisiana. Despite this, there was even no deaths reported. In Mexico, Tamaulipas, Nuevo León, and Coahuila was battered by heavy rainfall and flash flooding but no deaths were also reported. The system caused $14.7 million (2019 USD) in all the areas it affected and damaged.

Hurricane Zeta (31L)
Late on May 20, a tropical wave exited West Africa. The following day, May 21 at 18:00 UTC, the wave organized into Tropical Depression Thirty-one, becoming the thirty-first depression of the season. The STCC expected the depression strengthen into a tropical storm and head towards the Lesser Antilles and enter a favorable area for storms but a high pressure area over the Canary Islands turned it northwest towards Cape Verde, entering an area of dry air and increasing wind shear. On May 23, it made its closest approach to Cabo Verde. Later that day, at 18:00 UTC, Thirty-one degenerated into a tropical wave. Shortly afterward, dry air and wind shear slowly decreased and the system encountered favorable conditions but the STCC expected the remnants to dissipate despite favorable conditions. Two days later, May 25, at 12:00 UTC, the remnants of Thirty-one regenerated into a tropical depression. Intensification was slow due to marginally favorable conditions. However, on May 28, Thirty-one strengthened into a tropical storm and given the next name on the Greek list, Zeta, since the next name on the Greek list after Delta, Epsilon, was given to System 32L, becoming the twenty-seventh named storm of the season. It had remained a storm for a week. Finally on June 5, Zeta strengthened into a Category 1 hurricane, becoming the nineteenth hurricane of the season. On June 9 at 00:00 UTC, Zeta intensified into a Category 2 hurricane. The following day, June 10, Zeta strengthened even further to a Category 3 major hurricane, becoming the eighteenth major hurricane of the season. Between June 13 and June 15, Zeta strengthend into a Category 4 hurricane, weakened to a Category 3, and restrengtbened to a Category 4. It did that three times until it underwent an eyewall replacement cycle. Two days later, on June 17, Zeta restrengthened into a Category 4 and lasted much longer as its first three Category 4 stages. The following day, Gamma reached its peak intensity but weakened slightly to 140 mph (220 km/h). It maintained its intensity for nearly two weeks until an eyewall replacement cycle, rapidly declining sea surface temperatures, increasing wind shear, and drier air caused the system to rapidly weaken on June 29 and became extratropical twelve hours later while remaining nearly stationary. It increased its movement speed and headed southwest. The STCC expected it to regenerate to a subtropical storm and be tropical four days later, and hit the US East Coast and Bermuda but a frontal system caused the system to accelerate to the east-northeast and northeast and was absorbed by the same front on July 1. In Cape Verde, the islands received rajnfall of up to 13-15.50 inches in Boa Vista, Bravo, Fogo, and Sal and killed one person indirectly because of a building collapse in Santiago. In the Azores, there were rip currents that killed a person, also indirectly. The system caused minimal damage.

Hurricane Epsilon (32L)
Epsilon was the second of five storms that failed to reach major hurricane strength. On May 17, a tropical wave left West Africa. Four days later, on May 21, the wave organized into Tropical Depression Thirty-two, becoming the thirty-second depression of the season. The following day, May 22, at 18:00 UTC, the depression strengthened into a tropical storm and given the next name on the Greek list, Epsilon, becoming the twenty-sixth named storm of the season. With low wind shear and high sea surface temperatures, Epsilon was able to strengthen steadily as it was striking the Caribbean Islands. On May 25, Epsilon reached its initial peak intensity with winds of 71 mph (116 km/h) north of Hispaniola. The following day, May 26, wind shear began to increase causing the system to weaken as it approached Cuba. On May 29, Epsilon entered an area of weak sterring currents, causing it to make a two-day cyclonic loop, similar to Typhoon Muifa (Unding) in the West Pacific back in November 2004 but it strengthened and weakened while Epsilon maintained its intensity. On June 1, Epsilon entered an area of stronger steering currents, accelerating its movement while emerging into the Straits of Florida and into the Gulf of Mexico. Shortly afterward, wind shear decreased allowing, the system to rapidly intensify. The following day, June 2, at 18:00 UTC, Epsilon finally strengthened into a Category 1 hurricane, becoming the twentieth hurricane of the season. Two days later, on June 4, at 00:00 UTC, the hurricane strengthened into a Category 2 hurricane. A few hours after reaching peak intensity, Epsilon reached its peak intensity. The following day, Epsilon started to slowly weaken due to land interaction and its eye was cloud filled. On June 6, Epsilon made landfall over San Bernard National Wildlife Refuge, Texas with winds of 99 mph (158 km/h). Later that day, it weakened to a Category 1. It rapidly weakened for the system's last two days and on June 8, it became a remnant low. It dissipated later that day.

In the Leeward Antilles, tropical storm force winds were in St. Kitts and Nevis, Antigua, and Guadeloupe. All the islands experienced torrential rainfall, the highest in Antigua with rainfalls topping up to 8.99-9.59 inches of rainfall on May 24-25, killing 21 people; 7 direct, 14 indirect. In the Greater Antilles, Cuba and Hispaniola had tropical storm force winds. The heaviest rainfalls were in Cayo Fragoso, Cuba with rainfall of 14 inches. The rest of the Greater Antilles had torrential rainfall but not as heavy as Cuba. The system killed 10 people; 4 direct, 6 indirect. In The Bahamas, when the system completed the loop, torrential rainfall occured over the islands. Nassau had the heaviest rainfall, topping up to 15.60-16 inches of rainfall over the capital. It killed 14 people; all indirect from non-tropical rains created by Epsilon. In Florida, mostly the Florida Keys and South Florida, Miami had the heaviest rainfall, also when the storm was in its stalling phase, topping up to 14.50 inches. It killed 4 people in the Florida Keys; all directly. In the US Gulf Coast, Texas was the hardest hit, with a gust recorded of 109 mph (174 km/h) in Galveston and hurricane force winds in the eyewall during landfall on June 6. The rest of the deaths were in Texas. In Lousiana, tropical storm force winds affected the western part of the state and also torrential rainfall but no deaths reported. In Oklahoma the remains brought heavy rainfall but no deaths reported also. The system caused $35.9 (2019 USD) in all the areas it affected and damaged.

Hurricane Eta (33L)
On May 22, a tropical wave left West Africa. A week later, on May 29, at 06:00 UTC, the wave organized into Tropical Depression Thirty-three, becoming the thirty-third depression of the season. Twelve hours later, the system turned eastward due to a Fujiwhara interaction with a disturbance over the Lesser Antilles. The following day, May 30, it absorbed the disturbance. It turned back to the northwest after absorbing the disturbance on June 1. Early on June 3, the depression strengthened into a tropical storm after moving ashore Hispaniola and was given the next name on the Greek list, Eta, becoming the twenty-seventh named storm of the season. Despite land interaction, it maintained its strength over land. Later that day, it emergend back out to sea and rapidly intensfied to an initial peak intensity to winds of 50 mph (85 km/h) and a pressure of 998 mbar while moving north. A few hours after reaching its initial peak intensity, it fluctated in strength. On June 6, Eta weakened into a tropical depression due to moderate wind shear. Eta had no change in intensity as wind shear slowly started increasing. One June 9, Eta headed northeast. On June 10 at 23:00 UTC, Eta had degenerated into a remnant low as strong wind shear took toll. The STCC expected Eta to dissipate on June 12 as it continued to head northeast. However, the following day, June 11, at 06:00 UTC, the remnants of Eta had regenerated into a tropical depression as wind shear unexpectedly decreased due to a high pressure area turning the system east-northeast unexpectedly, also. Eta intensified and the following day, June 12 at 14:00 UTC, Eta restrengthened into a tropical storm. Two days later, on June 14, at 06:00 UTC, Eta strengthened into a Category 1 hurricane, becoming the twenty-first hurricane of the season. Eta intensified rapidly and on June 16, Eta strengthened further to a Category 2 hurricane. At this point, Eta's intensification slowed down as sea surface temperatures slightly decreased. On June 18, Eta rapidly strengthened to a Category 3 major hurricane, becoming the nineteenth major hurricane of the season. The following day, June 19, Eta rapidly strengthened even further to a Category 4 major hurricane. The following day, June 20, Eta rapidly intensified to reach its peak intensity. Shortly after reaching its peak intensify, an eyewall replacement cycle started to weaken Eta and on June 22 at 00:00 UTC, Eta briefly weakened to a Category 3 major hurricane. Six hours later, Eta restrengthened to a Category 4 major hurricane and reached a secondary peak intensity with winds of 130 mph (215 km/h) and a pressure of 942 mbar. Twelve hours later, Eta weakened to a Category 3, again due to a brief period of upwelling. The following day, June 23 at 06:00 UTC, Eta regained Category 4 intensity for the final time. Later that day, it reached a fourth peak intensity with winds of 135 mph (215 km/h) and a pressure of 940 mbar. Just after reached that peak intensity, it underwent another eyewall replacement cycle and the following day, June 24 at 06:00 UTC, it weakened to a Category 3, again. The following day, June 25 at 06:00 UTC, the system restrengthened to a Category 4 major hurricane. A few hours later, Eta reached its fifth and final peak intensity with winds of 135 mph (215 km/h) and a pressure of 941 mbar. On June 30 it completed a counter-clockwise loop. It had remained its final peak intensity until rapidly decreasing sea surface temperatures took toll on the system on July 4. The system also started extratropical transition on the same day. The system was absorbed by a frontal system on July 8.

In Hispaniola, tropical storm force winds up to 40-50 mph (65-85 km/h) were experienced in the Dominican Republic. There was also torrential rainfall over the eastern part of the islands, with the heaviest of 15 inches in San Pedro de Macoris, Dominican Republic. The system killed 3 people; 1 directly, 2 indirectly. In Haiti, the outer edges dumped torrential rainfall in the whole country except for the peninsulas on the west surrounding the Gulf of Gonave. The heaviest was 14.50 inches in Port-au-Prince, Haiti. The system killed 4 people; all directly. In the Turks and Caicos Islands, torrential rainfall occurred, the heaviest occurring on Cockburn Town with rainfall amounts topping up to 15.61 inches. The system killed a person indirectly. In Bermuda, hurricane force winds and torrential rainfall up to 16 inches in the whole islands killed 4 people indirectly. In Atlantic Canada, large swells and rip currents hit the southern coastlines of Newfoundland but no deaths were reported. In Ireland, the system, in its extratropical phase, dumped torrential rainfall on the western part of the country but not deaths reported. The system caused $12.6 million (2019 USD) in all the areas it affected and damaged.

Hurricane Theta (34L)
Late on May 30, a tropical wave left West Africa. On June 2, the wave organized into Tropical Depression Thirty-four, becoming the thirty-fourth depression of the season. On June 4, at 18:00 UTC, the depression strengthened to a tropical storm and given the next name on the Greek list, Theta, becoming the twenty-eighth named storm of the season. Theta slowly intensified and on June 7, Theta strengthened to a Category 1 hurricane, becoming the twenty-second hurricane of the season. On June 9 at 18:00 UTC, Theta intensified at a slightly faster rate to a Category 2 hurricane. 24 hours later; which is at June 10 at 18:00 UTC, Theta rapidly strengthened to a Category 3 major hurricane, becoming the twenty-fifth major hurricane of the season. On June 12, Theta strengthened to a Category 4 major hurricane and reached its initial peak intensity with winds of 130 mph (215 km/h) and a pressure of 938 mbar. Six hours later; which is the following day, June 13, at 00:00 UTC, upwelling caused the system to weaken back to a Category 3 major hurricane due to its slow movement. However, 12 hours later; which is at 18:00 UTC, it restrengthened to a Category 4 storm. It rapidly intensified and on June 15 at 18:00 UTC, it reached its peak intensity. Shortly after reaching its peak intensity, an eyewall replacement cycle and increasing wind shear started to weaken Theta and on June 16 at 18:00 UTC, the system weakened to a Category 3 major hurricane. However, 12 hours later; which is June 17 at 06:00 UTC, Theta regained Category 4 intensity again despite increasing wind shear. Theta had reached a secondary peak intensity with winds of 135 mph (215 km/h) and a pressure of 935 mbar. Wind shear took toll on the system and on June 18 at 00:00 UTC, Theta briefly weakened to a Category 3. STCC expected the system to weaken before striking the Carolinas as a high-end Category 1 like Hurricane Florence back in September 2018 or low-end Category 2 as they expected increasing wind shear to take toll. Unexpectedly, 6 hours later, Theta restrengthened to a Category 4 and reached the same secondary peak intensity. It did the same thing for 12 hours until it started to strengthen as wind shear decreased unexpectedly and on the same day at 18:00 UTC, it regained Categoy 4 strength for the final time and reached its final peak intensity on June 19 with winds of 140 mph (220 km/h) and a pressure of 930 mbar. It slowly weakened while approaching the Carolinas and on June 20, it made landfall over Santee Coastal Reserve, South Carolina as a high-end Category 3 major hurricane with winds of 125 mph (205 km/h) and a pressure of 947 mbar. It rapidly weakened while moving further inland and on June 21, Theta degenerated into a remnant low. The following day, the remnants dissipate still over South Carolina.

In the Bahamas, its outer edges hit the northern part of the UK territory, not with gale force winds but with significant rainfall topping up to 13.92-14.51 inches in Crown Haven. It killed 19 people; 13 direct, 6 indirect. In the Eastern United States, the Carolinas with the hardest hit with Category 3-equivalent force winds, really significant rainfall topping up to 30-31 inches, the highest in Charleston, South Carolina. The rest of the deaths were direct from flash flooding. The system caused $2 billion in all the areas it affected and damaged.

Hurricane Iota (35L)
On June 10 at 00:00 UTC, a cluster of thunderstorms detached from the ITCZ. Later that day, it was a low-pressure area. On June 12, at 00:00 UTC, the low-pressure area organized into Tropical Depression Thirty-five, becoming the thirty-fifth depression of the season while tracking east-northeast. On June 13 at 06:00 UTC, the depression strengthened to a tropical storm and was given the next name on the Greek list, Iota, becoming the twenty-ninth named storm of the season. The following day, June 14 at 18:00 UTC, it turned northwest due to a high pressure area over the Azores. Intensification continued and on June 16 at 06:00 UTC, Iota strengthened to a Category 1 hurricane, becoming the twenty-third hurricane of the season. Iota continued strengthening and on June 18 at 18:00 UTC or 48 hours later, the hurricane intensifed into a Category 2 hurricane. It rapidly intensified and on the next day, June 19, Iota strengthened into a Category 3 major hurricane, becoming the twenty-first major hurricane of the season. On June 21, the hurricane rapidly strengthened to a Category 4 major hurricane. The next day, Iota reached the first of two initial peak intensities with winds of 135 mph (215 km/h) and a pressure of 934 mbar. Soon afterwards, increasing wind shear and an eyewall replacement cycle weakened Iota and on the next day, June 22, it weakened to a Category 3 hurricane. The STCC expected continued weakening and a northeast turn towards Newfoundland and become extratropical after striking Newfoundland but wind shear unexpectedly decreased, allowing Iota to restrengthen back to a Category 4 hurricane the next day, June 23. The next day, it reached the last of two initial peak intensities with winds of 130 mph (215 km/h) and a pressure of 936 mbar. Due to its slow movement, upwelling weakened Iota and on the next day, June 24, the hurricane rapidly weakened to a Category 3 major hurricane. On June 26, Iota restrengthened to a Category 4 for the third time. Iota continued intensifying and on June 28 at 00:00 UTC, Iota reached its peak intensity. Shortly after reaching its peak intensity, it began fluctuating in strength. On June 30, it moved south and 6 hours later, west-southwest, and 6 hours later, to the north and tracked normally again. On July 3, Iota weakened to a Category 3 due to decreasing sea surface temperatures. However, 6 hours later, it restrengthened to a Category 4 despite cool sea surface temperatures. It then reached its last and secondary peak intensity with winds of 135 mph (215 km/h) and a pressure of 929 mbar. Shortly afterward, land interaction weakened Iota to a Category 3 and on July 5, Iota made landfall near Atlantic City, New Jersey with winds of 125 mph (205 km/h) and a pressure of 948 mbar. It started a rapid extratropical transition after making landfall and on the same day, it rapidly weakened to a Category 1 hurricane. The next day, July 6 at 06:00 UTC, Iota weakened even further to a tropical storm and 6 hours later, it completed extratropical transition. The next day, July 7, it dissipated off the Canadian coast of Lake Erie.

In Bermuda, hurricane force winds hit the island as the storm turned south then west-southwest, bringing a 2-foot storm surge along the coastal areas of the island. The whole island was flooded due to torrential rainfall up to 6 inches. The hurricane killed 7 people from flooding. In the United States, New Jersery was the hardest hit when it experienced the strongest winds. Torrential rainfall fell with the higest in Atlantic City in which rainfall fell up to 19.85-20 inches. In the rest of the United States, particularly the Delmarva Peninsula, Connecticut, Rhode Island. Massachusetts, New York, and Pennsylvania encountered tropical storm to hurricane force winds and rainfall up to 9 inches, the highest aside from New Jersey. In the Great Lakes Region, the extratropical remnants brought tropical storm force winds in Pennsylvania and New York. Torrential rainfall fell in Pennsylvania, New York, and Ohio. The system killed 15 people in the United States from flying debris and flooding. In Ontario, torrential rainfall fell, killing a person. The system caused $1.3 billion (2019 USD) in all the ares it damaged and affected.

Hurricane Kappa (36L)
Kappa was the third of five storms that failed to reach major hurricane strength. On June 19 at 00:00 UTC, a disturbance formed west-southwest of the Cape Verde islands. At first it moved southwest slowly, then south, then east due to a ridge west of the storm. The next day, June 20 at 12:00 UTC, the disturbance organized into Tropical Depression Thirty-six becoming the thirty-sixth depression of the season. The next day, June 21, the depression strengthened to a tropical storm and given the next name on the Greek list, Kappa, becoming the thirtieth named storm of the season. Kappa then continued northeast and had a slow movement due to an absence of significant steering currents. On June 26, Kappa intensified to a Category 1 hurricane, becoming the twenty-fourth hurricane of the season. Kappa then increased its movement speed and then decreased the movement speed. On June 30 at 00:00 UTC, it meandered offshore by completing a loop due to weak steering currents. However, this was brief as it began to track notheast again and on the next day, July 1, Kappa strengthened to a Category 2 hurricane. It maintained its intensity as a low-end Category 2 for several days until July 6 when Kappa reached its peak intensity. Shortly afterward, it underwent rapid extratropical transiton and early the next day, July 7, Kappa became extratropical. The extratropical remnants came to affect the northern part of the Iberian Peninsula and France just before dissipating over Northwestern France on July 16.

In Cape Verde, outflow caused heavy rainfall but no damage occured. In the Canary Islands, its rainbands brought rainfall up to only 2 inches in the westernmost part of the archipelago. In the Azores and Madeira, tropical storm force winds occured in the Azores but outflow caused only an inch of rainfall to fall over the island. In the Iberian Peninsula, this was the hardest hit from the storm with tropical storm force winds over the Northwestern part of the peninsula. In France, light to moderate rainfall occured. The system caused $56,100 (2019 USD) in all the areas it affected and damaged.

Tropical Depression Thirty-seven (37L)
On June 21, a low-pressure area formed east of the Lucayan Archipelago. Two days later, on June 23, it organized into Tropical Depression Thirty-seven, becoming the thirty-seventh depression of the season while over the Abaco Islands. The STCC expected it to intensity to a tropical storm but 18 hours later or on the following day, June 24, it degenerated into a remnant low. It then made 2 landfalls over Florida and dissipated on June 26.

In the Bahamas and Florida, heavy rainfall occured. No damages and deaths occured.

Hurricane Lambda (38L)
On June 28, a tropical wave left West Africa, then later that day, it interacted with an upper-level low, gaining subtropical characteristics. The next day, June 29 at 00:00 UTC, the wave organized into Subtropical Depression Thirty-eight, becoming the thirty-eighth depression of the season. It then meandered around due to weak steering currents. On July 1, it strengthened to a tropical storm and was given the next name on the Greek list, Lambda, becoming the thirty-first named storm of the season. The next day, it transitioned into a tropical storm. Lambda slowly strengthened and on July 8 at 06:00 UTC, it intensified into a Category 1 hurricane, becoming the twenty-fifth hurricane of the season but weakened to a tropical storm six hours later. However, it restrengthened to a Category 1 hurricane. On July 10, it strengthened to a Category 2 hurricane. Then the next day, July 11, it intensified rapidly to a Category 3 major hurricane becoming the twenty-second major hurricane of the season. On July 13, it strengthened even further to a Category 4 major hurricane but weakened to a Category 3 hurricane a few hours later. On July 15, it regained Category 4 hurricane strength but weakened again to a Category 3 major hurricane but 18 hours later, it restrengthened to a Category 4 major hurricane. Then, on July 18, it reached its peak intensity. It began weakening and in 24 hours it rapidly weakened to a Category 1 hurricane. Late on July 21, it made landfall over Clam Harbour, Nova Scotia, Canada with winds of 80 mph (130 km/h) and a pressure of 974 mbars. It then underwent extratropical transition. On the next day, it made landfall over Charlottetown, Prince Edward Island, Canada with the same wind speed at landfall in Nova Scotia but with a pressure of 979 mbars. Then shortly after landfall it transitioned to an extratropical cyclone. It then struck Labrador and Greenland. The extratropical remnants dissiapted on August 4.

In Bermuda, large swells and rip currents occured in the northern coast of the island. It killed 5 people indirectly from high surf. In Atlantic Canada, Nova Scotia was the hardest hit with torrential rainfall and strong winds in the southern part of the province, killing 8 people; all direct. Meanwhile, in Newfoundland, heavy rainfall occured in the western portion of the island. In Prince Edward Island, hurricane force winds occured and torrential rainfall also occured. In Labrador, tropical storm force winds occured and rainfall up to 14 inches occured in the heavily hit areas. 12 people were killed indirectly from diseases such as leptospirosis from flooding from the torrential rainfall. In Greenland, not that much happened. Only heavy rainfall. The system caused $450 million (2019 USD) in all the areas it affected and damaged.

Tropical Depression Thirty-nine (39L)
On July 3, a disturbance detached from the ITCZ and moved northeast. The next day, July 4, it meandered then turned west towards Florida. Later that day at 18:00 UTC, it organized into Tropical Depression Thirty-nine, becoming the thirty-ninth depression of the season. The next day, July 5, Thirty-nine made landfall over Canaveral National Seashore, Florida. It maintained tropical depression intensity until later that day, when it degenerated into a remnant low. It emerged in the Gulf of Mexico. Regeneration was expected but moderate wind shear inhibited redevelopment and on July 6 at 18:00 UTC, it made its second landfall over Pensacola, Florida. It turned northeast on July 7 and dissipated at 06:00 UTC on the same day.

In the Bahamas, its precursor dumped moderate to heavy rainfall over the Abaco Islands. No deaths occured. In Florida, it dumped heavy rainfall over the areas near its landfall area. One indirect death occured from a heart attack when rescuers were rescuing a man and died suddenly. In Alabama, heavy rainfall occured in Mobile mostly. Despite this, minimal damage occured in all the areas it affected and damaged.

Hurricane Mu (40L)
On July 5 a tropical wave emerged off the coast of West Africa. It moved northwest and on July 10, it moved southeast due to weak steering currents. Later that day, it organized into Tropical Depression Forty, becoming the fortieth depression of the season. The next day, July 11 at 00:00 UTC, it strengthened into a tropical storm and was given the next name on the Greek list, Mu, becoming the thirty-second named storm of the season. It then moved eastward and then east-northeastward. On July 15 at 18:00 UTC, it strengthened to a Category 1 hurricane, becoming the twenty-sixth hurricane of the season. 24 hours later, it strengthened to a Category 2 hurricane and turned southeast due to an interaction with a tropical wave. Later that day, it absorbed the wave and turned northeast and 24 hours later, again. It strengthened to a Category 3 major hurricane, becoming the twenty-third major hurricane it turned west a few hours later. On July 18, it strengthened to a Category 4 major hurricane while moving west. 12 hours later, it moved north. On July 19, it reached its peak intensity. Shortly after reaching peak intensity, an eyewall replacement cycle and upwelling weakened Mu to a Category 2 in just 6 hours. 12 hours later, Mu regained Category 3 strength. On July 24, it restrengthened to a Category 4 but weakened to a Category 3 12 hours later before regaining Category 4 strength, it stalled due to weak sterring currents. It kept stalling while fluctuating between Category 3 and 4 strength multiple times. On August 11, it increased its movement speed. On August 12, it made landfall over Qassimiut, Southern Greenland with winds of 115 mph (185 km/h) and a pressure of 936 mbars, becoming the strongest storm and only hurricane to make landfall over Greenland. It rapidly weakened to a Category 1 and became extratropical on August 13. The extratropical remnants dissipated two days later, August 15.

In Cape Verde, large swells and rip currents killed 40 people; 30 direct, 10 indirect. This was mostly due to people having a vacation and seeing rip currents and then dying in the rip currents for the 30 people. For the 10 people, these were mostly due to seasickness after the rip current event. In the Azores, its large outer edges brought heavy rainfall across the westernmost islands, killing 10 people; all directly from drowning in floods. In Greenland, Southern Greenland was the hardest hit with heavy rainfall, the heaviest ever seen in Southern Greenland. It also experienced major hurricane force winds, the first ever recorded. It killed 390 people; 350 people directly and 40 people indirectly. The direct deaths were from flying debris, drowning, and lightning strikes during the thunderstorm event after landfall. Indirect deaths were from diseases and violence in its aftermath. The system caused $24 million (2019 USD) in all the areas it affeced and damaged.

Tropical Depression Forty-one (41L)
On July 12 at 00:00 UTC, a disturbance developed in the southern Gulf of Mexico. It moved east then northwest and on the next day, the disturbance developed into Tropical Depression Forty-one, becoming the forty-first depression of the season despite strong wind shear. However, strong winds shear took toll on the depression and 12 hours later, the depression degenerated into a remnant low. The low turned southwest the next day and dissipated on the same day.

In Mexico, not that much occured. Only heavy rainfall in Campeche. The system caused no damages and deaths.

Tropical Depression Forty-two (42L)
On July 14, a tropical wave emerged off the coast of West Africa. It gained more organization as it approached the Lesser Antilles. On July 22 at 18:00 UTC, it organized into Tropical Depression Forty-two, becoming the forty-second depression of the season. The next day, July 23 at 06:00 UTC, it reached its peak intensity. Shortly afterward, wind shear slowly increased causing fluctuations in strength. On July 25 at 18:00 UTC, it degenerated into a remnant low but six hours later, it regenerated into a tropical depression. The STCC expected it to strengthen to a tropical storm but increased wind shear took toll on the system again but it reached its secondary peak intensity with winds of 30 mph (45 km/h) and a pressure of 1004 mbars. On July 28, it degenerated into a remnant low. The remnants dissipated the next day, July 29.

In the Leeward Islands, heavy rainfall fell over St. Kitts and Nevis, the highest rainfall by the storm, with 5 inches. No deaths occured. In Puerto Rico, moderate to heavy rainfall fell over the northern parts of the US territory. No deaths occured. In the Lucayan Archipelago, buildings were damaged and heavy rainfall occured. The system caused $2,780 in all the areas it affected and damaged.

Hurricane Nu (43L)
Nu was the fourth of five storms that failed to reach major hurricane strength. On July 29, a tropical wave departed West Africa. On August 3 at 00:00 UTC, the wave organized into Tropical Depression Forty-three, becoming the forty-third depression of the season. The depression slowly gained more strength and on August 6 at 00:00 UTC, the depression strengthened to a tropical storm and was given the next name on the Greek list, Nu, becoming the thirty-third named storm of the season. Again, it intensified slowly but as it moved closer to the Carolinas, it strengthened to a Category 1 hurricane on August 9 at 12:00 UTC, becoming the twenty-seventh hurricane of the season. It only lasted for 18 hours. It made landfall near Charleston, South Carolina at peak intensity on August 10 at 00:00 UTC. It rapidly weakened and degenerated into a remnant low on the same day. The remnants dissipated the next day, August 11.

In the United States East Coast, the Carolinas were the hardest hit with hurricane force winds in South Carolina and torrential rainfall over both North and South Carolina, killing 3 people directly in South Carolina and 3 people indirectly in North Carolina. In Virginia, its outer rainbands brought heavy rainfall and sickness in the aftermath, killing 4 people indirectly. The system caused $12.5 million (2019 USD) in all the areas it affected and damaged.

Tropical Storm Xi (44L)
On August 10, a low-pressure area was doing a cyclonic loop. On August 12 at 00:00 UTC, the low-pressure area developed into Tropical Depression Forty-four becoming the forty-forth depression of the season. 24 hours later or on August 11 at 00:00 UTC, the depression strengthened into a tropical storm and was given the next name on the Greek list, Xi, becoming the thirty-fourth named storm of the season despite strong wind shear affecting the storm. Wind shear slowly decreased and on August 14 at 12:00 UTC, Psi reached its peak intensity. Shortly after reaching its peak intensity, wind shear slowly increased, weakening Xi before making landfall over Melbourne, Florida on August 17 at 10:00 UTC as a minimal tropical storm and a partially exposed LLCC with winds of 40 mph (65 km/h) and a pressure of 1002 mbars. Xi then weakened to a tropical depression 2 hours later. On August 18 at 00:00 UTC, Xi emerged in the Gulf of Mexico, wind shear was even stronger in the gulf, exposing Xi's LLCC, causing it to degenerate into a remnant low later that day. The next day, a high pressure area moved the remnants northeast, making another landfall over Pensacola, Florida as a remnant low. It dissipated the next day, August 19 over Alabama.

In the Bahamas, its displaced convection brought heavy rainfall and tropical storm force winds over the northernmost islands a preson was killed directly. In Florida, this was the hardest hit with torrential rainfall, tropical storm force winds, and flash flooding killed 4 people; 3 direct and 1 indirect. In Alabama, its remnants brought moderate rainfall. The system caused $935,000 (2019 USD) in all the areas it affected and damaged.

Tropical Depression Forty-five (45L)
On August 14, a Central American gyre formed off the coast of Costa Rica. It meandered while taking a northerly track in an area of strong wind shear. On August 16 at 18:00 UTC, the gyre developled into Tropical Depression Forty-five, becoming the forty-fifth depression of the season despite strong wind shear. Not long after, strong wind shear took toll on the depression and 12 hours later, it degenerated into a remnant low. The remnants continued northeast and dissipated on August 18.

In Central America, the gyre that later organized into the depression brought heavy rainfall in Central America, mostly in Costa Rica, Nicaragua, and Honduras, damaging structures but no deaths occurred. In the Cayman Islands, heavy rainfall and flash flooding occurred, damaging structures but no deaths occurred. In Cuba, the remnants brought torrential rainfall but not much occurred and no deaths were reported. Despite this, the system caused minimal damage in all the areas it affected and damaged.

Hurricane Omicron (46L)
Omicron was the last of five stroms that failed to reach major hurricane strength. On August 21 a non-tropical low moved southeast. It then moved west-northwest due to a ridge east of it. The next day, August 22 at 06:00 UTC, the low developed into Tropical Depression Forty-six, becoming the forty-sixth depression of the season. It moved west-northwest rapidly and slowly strengthened. On August 24 at 00:00 UTC, 46L strengthened to a tropical storm and was given the next name on the Greek list, Omicron becoming the thirty-fifth named storm of the season. It was expected to intensity to a powerful hurricane as it approached the Carolinas according to the STCC and NHC but low to moderate wind shear caused it to intensify slowly. However, on August 26 at 12:00 UTC, Omicron strengthened to a Category 1 hurricane, becoming the twenty-eighth hurricane of the season. A few hours later, it made landfall over Sapelo Island, Gerogia. Then, 6 hours later, it weakened to a tropical storm. It survived further inland as a weakening tropical storm then on August 27 at 18:00 UTC, it weakened to a tropical depression. 6 hours later, it degenerated into a remnant low. The remnants dissipated the next day, August 28 over inland Alabama.

In the Bahamas, its outer edges brought moderate to heavy rainfall over Grand Bahama and the Abaco Islands but no deaths occurred. In the United States East Coast, Georgia was the hardest hit with hurricane force winds, killing 5 people directly. In South Carolina, its inner rainbands brought tropical storm force winds to the southern cities and districts, killing 1 person directly. In Alabama, tropical storm force winds occurred, killing 3 people; 1 direct, 2 indirect from torrential rainfall, flash flooding and diseases. The system caused $15 million (2019 USD) in all the areas it affected and damaged.

Hurricane Pi (47L)
On August 22 at 00:00 UTC, a disturbance detached from the ITCZ moving eastwards, similar to Iota's precursor. On August 24 at 18:00 UTC, the disturbance developed into Tropical Depression Forty-seven, becoming the forty-seventh depression of the season. It then moved east-northeast. The next day, August 25 at 12:00 UTC. the depression strengthened to a tropical storm and was given the next name on the Greek list, Pi, becoming the thirty-sixth named storm of the season. It then moved northeast for a brief time before moving east-northeast then east. On August 28 at 12:00 UTC, Pi strengthened to a Category 1 hurricane, becoming the twenty-ninth hurricane of the season. It moved northeast and accelerated its movement. Between August 30 and 31, it started a counter-clockwise loop northwest of the Cabo Verde islands due to several influences which caused it to loop. On September 1 at 00:00 UTC, Pi strengthened to a Category 2 hurricane after completing the loop. It continued northeast and then moved northwest. On September 3 at 18:00 UTC, the hurricane strengthened even further into a Category 3 major hurricane, becoming the twenty-forth major hurricane of the season. On September 7 at 18:00 UTC, Pi strengthened into a Cateogry 4 hurricane but weakened to a Category 3 12 hours later. It fluctuated between Category 3 to low-end Category 4 eight more times. On September 17 at 18:00 UTC, Pi reached its peak intensity. It underwent an eyewall replacement cycle before landfall. The next day, September 18, Pi made landfall over Eastern Passage, Nova Scotia in Canada with winds of 120 mph (195 km/h) and a pressure of 942 mbars, becoming the strongest storm to make landfall over Nova Scotia. It rapidly weakened and became extratropical still over Nova Scotia. It then moved westwards and dissipated over Ontario on September 20.

In the Northeastern United States, its large size brought tropical storm force winds over Maine. In the rest of the region, torrential rainfall occurred, killing 12 people; 5 direct, 7 indirect. In Atlantic Canada, Nova Scotia felt the hardest and strongest brunt of it all, with Category 3-equivalent winds, torrential rainfall, a 20-foot storm surge, and flash flooding across the province killed 25 people; 18 direct, 7 indirect. In New Brunswick, tropical storm force winds and torrential rainfall along with flash flooding killed 2 people indirectly. In Quebec and Ontario, torrential rainfall killed 18 people in both provinces combined. The system caused $678 million (2019 USD) in all the areas it affected and damaged.

Hurricane Rho (48L)
On August 26, a tropical wave left West Africa. It rapidly developed and on August 27 at 12:00 UTC, the wave developed into Tropical Depression Forty-eight, becoming the forty-eighth depression of the season. It moved northwest rapidly. Between August 30 and 31 it completed a clockwise loop. On September 1 at 00:00 UTC, the depression strengthened to a tropical storm and was given the next name on the Greek list, Rho, becoming the thirty-seventh named storm of the season. It continued west-northwest and on September 5 at 12:00 UTC, Rho strengthened to a Category 1 hurricane, becoming the thirtieth hurricane of the season. Shortly afterward, it passed north of Antigua and Barbuda and then made its first landfall over St. Kitts and Nevis with winds of 75 mph (120 km/h) and a pressure of 981 mbars but rapidly strengthened after emerging in the Caribbean Sea. On September 6 at 00:00 UTC, it strengthened to a Category 2 hurricane but six hours later, it weakened to a Category 1 hurricane just before making its second landfall over Puerto Rico with winds of 90 mph (145 km/h) and a pressure of 974 mbars at 07:00 UTC. A few hours later, it moved back at sea and restrengthened to a Category 2 hurricane at 12:00 UTC north of Puerto Rico but weakened to a Category 1 hurricane 6 hours later but restrengthened to a Category 2 on September 7 at 00:00 UTC and made landfall over Samana Bay, Dominican Republic in Hispaniola with winds of 100 mph (155 km/h). Despite making landfall, it continued to strengthen. 18 hours later, Rho strengthened to a Category 3 major hurricane, becoming the twenty-fifth major hurricane of the season. On September 8 at 06:00 UTC, it made its landfall near Baracoa, Cuba with winds of 115 mph (185 km/h) and a pressure of 954 mbars. 6 hours later, it weakened to a Category 2 hurricane. 12 hours later, it restrengthened to a Category 3 of the coast of Cuba. It then made its second Cuba landfall over Sancti Spiritus, Cuba with the same intensity it made landfall over Baracoa. On September 9 at 06:00 UTC it weakened to a Category 2 hurricane but 6 hours later, it regained Category 3 strength as it moved in the Gulf of Mexico and then Category 4 six hours later but weakened to a Category 3 six hours later and then did the same strengthening procedure again. On September 11 at 00:00 UTC, Rho reached its peak intensity. On September 12 at 06:00 UTC, Rho made its final landfall over Texas with winds of 130 mph (215 km/h) and a pressure of 948 mbars. It rapidly weakened from a Category 4 to a tropical storm in just 12 hours. The next day, September 13, it degenerated into a remnant low and then stalled over Mexico and Texas it dissipated the next day, September 14.

In the Lesser Antilles, the Leeward Islands experienced heavy rainfall, flash floods, and damages similar to Irma 2 years ago in the real world but not as damaging as Irma but the Windward Islands were hit also. It killed 105 people; 56 direct, 49 indirect. In the Greater Antilles, Cuba was the hardest hit with 115 mph winds in the areas affected, Hispaniola and Puerto Rico had also harsh conditions at landfall, killing 253 people; 235 people directly, 18 people indirectly from flash floods, storm surge, flying debris, and diseases. In the Cayman Islands, hurricane force winds occurred but no deaths occurred. In the Lucayan Archipelago, its outer edges brought heavy rainfall which killed 5 people directly. In the Florida Keys and Florida, hurricane force winds, torrential rainfall, flash floods, flying debris, and destroyed houses killed, killing 34 people directly. In the United States Gulf Coast, Texas was the hardest hit with effects similar to Harvey 2 years ago in the real world but was not as destructive as Harvey was but it killed 107 people directly from flash floods and flying debris. In Mexico, when its remnants stalled, it brought heavy rainfall that killed 2 people indirectly from landslide in Coahuila. The system caused $1.52 billion (2019 USD) in all the areas it affected and damaged.

Hurricane Tau (49L)
On August 26, a tropical wave left West Africa. On August 28 at 12:00 UTC, the wave developed into Tropical Depression Forty-nine, becoming the forty-ninth depression of the season. It failed to strengthen due to moderate shear from the larger Tropical Depression Forty-eight (which later became Hurricane Rho). On August 30 and 31, the system stalled due to a Fujiwhara interaction with 48L. It then moved back west on September 1 but moderate shear took toll on the storm. Wind shear decreased shortly afterward. On September 3, the depression strengthened into a tropical storm and was given the next name on the list, Tau, becoming the thirty-ninth named storm since the name after Rho, Sigma, was given to System 50L. Tau then moved west-northwest and on September 5, it made its first landfall over Grenada with winds of 60 mph (95 km/h) and a pressure of 991 mbars. The next day, September 6 at 06:00 UTC, it strengthened to a Category 1 hurricane, becoming the thirty-first hurricane of the season. On September 7 at 06:00 UTC, Rho strengthened to a Category 2 hurricane then a Category 3 major hurricane 6 hours later, becoming the twenty-sixth major hurricane of the season. It continued west-northwest and then on September 8 at 18:00 UTC, it strengthened to a Category 4 major hurricane but six hours later, it weakened back to a Category 3. It then regained Category 4 strength but weakened again to a Category 3 in 12 hours. It then regained Category 4 strength for the final time 6 hours later. Then, it moved northwest. On September 10, Tau made landfall over Quintana Roo, Mexico with winds of 140 mph (220 km/h) and a pressure of 934 mbars. It weakened slightly but when it emerged in the Gulf of Mexico, it strengthened again and on September 12 at 00:00 UTC, Tau reached its peak intensity. It then moved northwest and then underwent an eyewall replacement cycle. It then weakened and on September 13, it made its final landfall over Tamaulipas as a Category 2 hurricane with winds of 100 mph (155 km/h) and a pressure of 967 mbars. It rapidly weakened and then dissipated on September 14 still over Mexico.

In Venezuela and Colombia, tropical storm force winds occurred in Colombia but no deaths occurred. In the Lesser Antilles, Grenada was the hardest hit with tropical storm force winds, storm surge, and flash flooding killing 16 people; 7 direct, 9 indirect. The ABC Islands were the hardest hit also with gusty winds, storm surge, and flying debris killing 24 people; 10 direct, 14 indirect. In the Greater Antilles, rip currents along with Hurricane Rho killed 16 people indirectly. In the Cayman Islands, hurricane force winds occurred but no deaths occurred. In Central America, hurricane force winds occurred in Honduras while tropical storm force winds occurred in Belize. Flash floods, coastal flooding, storm surge, and flying debris killed 13 people; 4 direct, 9 indirect. In Mexico, Quintana Roo was the hardest hit with gusty winds, flash floods, storm surge and flying debris killing 29 people, 14 direct, 15 indirect. In Texas, its outer edges brought flash floods in South Texas but no deaths occurred. The system caused $4.03 billion (2019 USD) in all the areas it affected and damaged.

Tropical Storm Sigma (50L)
On August 26, a trio of tropical waves left West Africa. Two of the waves developed into Hurricanes Rho and Tau. The third one developed on September 1 at 18:00 UTC in the Gulf of Mexico west of Florida, becoming the fiftieth depression of the season. The next day, September 2 at 12:00 UTC, the depression strengthened to a tropical storm and was given the next name on the list, Sigma, becoming the thirty-eighth named storm of the season. It moved west-northwest and on September 4 at 18:00 UTC, it reached its peak intensity. It continued west-northwest and then maintained its intensity until it approached Texas where land interaction began weakening the system. On September 6 at 12:00 UTC, Sigma made landfall near Freeport, Texas. 6 hours later, it weakened to a tropical depression. Then on September 7 at 00:00 UTC, it degenerated into a remnant low. The remnants dissipated 18 hours later.

In the Florida Keys and Florida, it brought heavy rainfall and flash floods that damaged structures but no deaths occurred. In the Gulf Coast of the United States, Texas has the hardest hit with gusty winds, flash floods, and damaged structures but no deaths occurred. The same thing occurred in Louisiana. The system caused $955,000 (2019 USD) in all the areas it affected and damaged.

Hurricane Upsilon (51L)
On September 10, a tropical wave emerged off the coast of West Africa. Then, the next day, September 11 at 18:00 UTC, the wave developed into Tropical Depression Fifty-one, becoming the fifty-first depression of the season. It moved west-northwest at a fast speed and on September 13 at 06:00 UTC, the depression strengthened to a tropical storm and was given the next name on the Greek list, Upsilon, becoming the fortieth named storm of the season. It continued west-northwest at a fast speed and began to fluctuate in movement. On September 14 at 18:00 UTC, Upsilon made its first landfall over Grenada with winds of 65 mph (100 km/h) and a pressure of 990 mbars which was much stronger than Tau's landfall a few weeks ago. 24 hours later, it strengthened to a Category 1 hurricane, becoming the thirty-second hurricane of the season. It accelerated but decelerated slightly a few hours later. On September 6 at 00:00 UTC, it strengthened to a Category 2 hurricane and then 6 hours later, it became a Category 3 major hurricane, becoming the twenty-seventh major hurricane of the season. But, it weakened to a Category 2 hurricane six hours later. Then, on the next day, September 7 at 06:00 UTC, it regained Category 3 intensity again. Then, 6 hours later, it reached its peak intensity and made landfall over Belize and then weakened to a Category 2 six hours later due to land interaction. Then the next day, September 18, it emerged in the Bay of Campeche. Then, on the same day at 18:00 UTC, it weakened to a Category 1 hurricane just before making landfall over Veracruz. It then weakened to a tropical storm 6 hours later. It weakened to a tropical depression at 12:00 UTC and moved east-northeast and as it reemerged in the Gulf of Mexico, it stalled but had a fast speed. It made two more landfall still over Veracruz and dissipated on September 20 at 18:00 UTC.

In Venezuela and Colombia, it brought heavy rainfall, storm surge, and flash floods which killed 7 people; 4 direct, 3 indirect. In the Lesser Antilles, Grenada was the hardest hit after Tau hit the areas but was stronger and killed 8 people; 7 direct, 1 indirect due to floods and flying debris. In Central America, Belize and Honduras was the hardest hit though Guatemala was hit by its remnants and also Nicaragua by its outer edges. Flooding, storm surge, flying debris, and diseases killed 30 people; 18 direct, 12 indirect mostly in Belize. In the Yucatan Peninsula, its outer edges also brought torrential rainfall and strong winds but no deaths occurred. In Mexico, Veracruz was the hardest hit with gusty winds, torrential rainfall, mudslides, and flash floods killing 6 people directly even in its stalling phase as a remnant low. The system caused $498 million (2019 USD) in all the areas it affected and damaged.

Hurricane Phi (52L)
On September 24 a tropical wave left West Africa. On the same day at 18:00 UTC, it organized into Tropical Depression Fifty-two, becoming the fifty-second depression of the season. It moved northwest then west-northwest. Dry air began affecting the system, causing it to degenerate into a remnant low on September 26 at 12:00 UTC but regenerated 6 hours later as it moved away from the dry air zone. Then, on September 28 at 18:00 UTC, the depression strengthened to a tropical storm and was given the next name on the list, Phi, becoming the forty-first named storm of the season. It briefly stalled on September 30 at 00:00 UTC but moved back northwest 24 hours later. It strengthened and on October 2 at 18:00 UTC, it was upgraded to a Category 1 hurricane, becoming the thirty-third hurricane of the season. It continued west-northwest and strengthened. Then, on October 5 at 00:00 UTC, it strengthened to a Category 2 hurricane. Intensification continued and on October 7 at 18:00 UTC, it strengthened to a Category 3 major hurricane, becoming the twenty-eighth major hurricane of the season. 6 hours later, it strengthened to a Category 4 major hurricane and changed course by moving northwest. Shortly afterward, it reached an initial peak intensity with winds of 135 mph (215 km/h) and a pressure of 937 mbars. It then underwent an eyewall replacement cycle, weakening to a Category 3 storm on October 9 at 12:00 UTC but regained Category 4 strength 6 hours later. Then, on the next day, October 10, it reached the same initial peak intensity it reached 3 days ago. Upwelling weakened Phi and on the next day, October 11, it weakened to a Category 3 though it restrengthened to a Category 4 on the same day. Then on October 12 at 00:00 UTC, it reached its peak intensity. It continued to move north still as a Category 4 hurricane and continued to fluctuate in intensity while it paralleled the coast of Massachusetts, becoming one of the strongest to hit the coastline. On October 14 at 06:00 UTC, it weakened to a Category 3 hurricane and stalled off the coast of Maine. On October 16, it made landfall over Portland, Maine with winds of 115 mph (185 km/h) and a pressure of 950 mbars. It maintained its intensity despite making landfall but late on the same day, it weakened to a Category 2 hurricane and began to move northeast. The next day, October 17 at 18:00 UTC, it weakened to a category 1 hurricane but 18 hours later, it became extratropical. it moved south then northwest as it began to hit Quebec and Labrador. The extratropical remnants were absorbed by another extratropical cyclone on October 23.

In West Africa, it brought heavy rainfall but no deaths occurred. In Cape Verde, torrential rainfall brought flash floods which killed a person directly. In Bermuda, gusty winds were experienced but the most dangerous threat was storm surge though flash flooding killed 25 people; 17 direct, 8 indirect. In the East Coast of the United States, the Northeastern United States was the hardest hit with the strongest hit since Sandy in the real world last 2012. It killed 24 people from storm surge and floods. In Atlantic Canada, gusty winds also killed a person in Nova Scotia from flying debris. In Quebec and Labrador tropical storm force winds killed a person due to heavy rainfall and flash floods. The system caused $2.34 billion (2019 USD) in all the areas it affected and damaged.

Hurricane Chi (53L)
On September 27 at 00:00 UTC, a tropical wave left West Africa, 18 hours later, the wave developed into Tropical Depression Fifty-three, becoming the fifty-third depression of the season. It stalled on September 30 but the track "returned back to normal" on October 1 at 00:00 UTC. On the next day, October 2 at 06:00 UTC, 53L strengthened to a tropical storm and was given the next name on the Greek list, Chi, becoming the forty-second named storm of the season. It slowly strengthened due to moderate wind shear and 27 degrees Celsius SSTs. However, on October 7 at 18:00 UTC, Chi strengthened to a Category 1 hurricane becoming the thirty-fourth and last hurricane of the season. Wind shear decreased and SSTs increased, allowing faster intensification. Then, on October 9 at 18:00 UTC or "48 hours later", it strengthened to  a Category 2 hurricane. Rapid intensification continued and on the next day, October 10 at 06:00 UTC, Chi gained Category 3 major hurricane strength, becoming the twenty-ninth and last major hurricane of the season. 18 hours later, it strengthened to a Category 4 hurricane (October 11 at 00:00 UTC) but weakened to a Category 3 six hours later. 18 hours later, it regained Category 4 intensity. It maintained this intensity for 24 hours until it weakened to a Category 3 hurricane. It moved north but curved back west-northwest. On October 14 at 12:00 UTC, it regained Category 4 strength for the final time. The next day, October 15 at 06:00 UTC, it reached its peak intensity. It began another stalling phase due to a frontal system and a high pressure area. It weakened slightly due to cooling SSTs and land interaction. Early on October 17, Chi made two landfall over Massachusetts. On the same day at 18:00 UTC, it weakened to a Category 3 hurricane. On October 19 at 00:00 UTC, it weakened to a Category 2. Then, six hours later, it rapidly weakened to a tropical storm and became extratropical. The extratropical system dissipated on October 21.

In West Africa, the precursor dumped heavy rainfall over The Gambia and Senegal. In Cape Verde, torrential rainfall brought flash floods which killed a person directly from drowning. In Bermuda, hurricane force gusts, strong winds, torrential rainfall brought flash floods, storm surge, and thunderstorms which killed 4 people; 2 directly, 2 indirectly. In the East Coast of the United States, Massachusetts, Connecticut, Rhode Island, New Hampshire, and the Eastern United States received gusty winds, East Coast received flash floods and storm surges, and etc., which killed 21 people directly. In Atlantic Canada, Quebec, and Ontario strong winds and heavy rainfall killed crops and livestock but no human deaths occurred. The system caused $372 million (2019 USD) in all the areas it affected and damaged.

Tropical Depression Fifty-four (54L)
On September 20, a tropical wave left West Africa. On September 29 at 18:00 UTC, the wave organized into Tropical Depression Fifty-four becoming the fifty-fourth depression of the season. It then moved eastwards then northwest. On October 1 at 00:00 UTC, it degenerated into a remnant low due to land interaction in Hispaniola just before making landfall over Bani, Dominican Republic. 12 hours later, it regenerated to a tropical depression. It then moved north after reformation. STCC Atlantic expected it to move north then northeast and continue strengthening to a tropical storm according to the NHC. But, an upper-level low and high pressure area brought strong wind shear, causing the system to degenerate into a remnant low on October 2 at 00:00 UTC. It then moved west-southwest and then south. It made landfall over Guantanamo, Cuba on October 3 at 06:00 UTC, the remnants dissipated 6 hours later.

In Hispaniola, over 25 inches of rain fell over mountainous areas which brought flash floods that killed 105 people; 100 direct from being washed away and drowning, 5 indirect from diseases. In the Turks and Caicos Islands heavy rainfall fell over the areas it passed near but no deaths occurred. In Cuba, Guantanamo was the hardest hit with heavy rainfall and floods but no deaths occurred. The system caused $512 million (2019 USD) in all the areas it affected and damaged.

Tropical Depression Fifty-five (55L)
On October 3 at 12:00 UTC, a low pressure area formed. It moved northwest but 12 hours later, moved eastwards. It then made landfall over Campeche in the Yucatan Peninsula on the next day, October 4 at 18:00 UTC. It moved back out a 12 hours later. It then moved south then southwest into the Caribbean Sea. Then, on October 8 at 18:00 UTC, it developed into Tropical Depression Fifty-five, becoming the fifty-fifth named storm of the season. It then moved east-northeast. STCC Atlantic and NHC expected 55L to strengthen to a tropical storm and move northeast to strike Cuba in 5 days but 18 hours later, it degenerated into a remnant low due to its close proximity to Honduras. It then moved south-southwest and made landfall on October 10 at 00:00 UTC over Honduras and dissiapted 12 hours later.

In Mexico, the precursor dumped heavy rainfall over Veracruz but no deaths occurred. In the Yucatan Peninsula in its middle stages of development, especially its landfall, it dumped torrential rainfall over 4 inches in Campeche, Yucatan, and Quintana Roo but no deaths were reported. In Cuba, its outer edges brought heavy rainfall in Pinar Del Rio but no deaths were reported. In Central America, Honduras has the hardest hit though Nicaragua, Belize, El Salvador, and Guatemala were hit too. Torrential rainfall and flash floods caught the lives of 13 people in total, 12 directly and 1 indirectly. The system caused $8.51 million (2019 USD) in all the areas it affected and damaged.

Tropical Storm Psi (56L)
On October 5, tropical wave left West Africa. it moved northwest then west. On October 11 at 12:00 UTC, the wave developed into Tropical Depression Fifty-six, becoming the fifty-sixth depression of the season. It moved slowly at first then its movement accelerated. Then, on October 13 at 00:00 UTC, 56L strengthened to a tropical storm and was given the next name on the Greek list, Psi, becoming the forty-third named storm of the season. It slowly strengthened and 18 hours later, it reached its initial peak intensity with winds of 45 mph (75 km/h) and a pressure of 998 mbars. Then, wind shear slowly increased, causing Psi to briefly weaken to a tropical storm on October 16 at 12:00 UTC. Wind shear decreased, causing it to reintensify to a tropical storm 6 hours later. It intensified again and on October 19, it reached its peak intensity at 12:00 UTC. Then, 6 hours later, it made landfall over Brunswick, Georgia with winds of 65 mph (100 km/h) and a pressure of 992 mbars. The next day, October 20 at 06:00 UTC, Psi weakened to a tropical depression. It degenerated into a remnant low 18 hours later. It moved inland and dissipated over Mississippi on October 22 at 06:00 UTC.

In the Bahamas, it outer edges brought heavy rainfall over Grand Bahama and the Abaco Islands but no deaths were reported. In Florida, this was the second hardest hit area with strong winds, rainfall up to 5 inches in some areas, and floods but no deaths were reported, too. In Georgia, this was the hardest hit area at landfall with gusty winds, torrential rainfall, and flash floods. Families had to be evacuated but no deaths were reported, especially in the aftermath. in Alabama and Mississippi, heavy rainfall occurred but no damage and deaths were reported. The system caused $30 million (2019 USD) in all the areas it affected and damaged.

Tropical Depression Fifty-seven (57L)
On October 11 at 06:00 UTC, a non-tropical low formed in the Gulf of Mexico. It moved northeast then shifted to the west. It gained tropical characteristics and on October 13 at 18:00 UTC, the low developed into Tropical Depression Fifty-seven, becoming the fifty-seventh depression of the season. STCC Atlantic and the NHC expected it to dissipate in a few days. However, it only dissipated 18 hours later due to land interaction. It then made landfall over the Texas-Louisiana border as a remnant low on October 15 at 06:00 UTC. It continued inland and dissipated 36 hours later.

In the Gulf Coast, the precursor passed west of Florida dumping heavy rainfall over the western part of the state, especially the Panhandle. Louisiana was the hardest hit among all states. Rainfall up to 6 inches and flash floods killed a person directly. In Texas, the remnants summoned two tornadoes, an EF3 in Austin, Texas and an EF2 in Dallas, Texas. Both of these tornadoes killed a person, respectively. The system caused minimal damage only.

Tropical Storm Omega (58L)
On October 15, a tropical wave left West Africa. On October 19 at 12:00 UTC, the wave developed into Tropical Depression Fifty-eight, becoming the fifty-eighth depression of the season. Twelve hours later, the depression strengthened to a tropical storm and was given the next name on the list, Omega, becoming the forty-forth and last named storm of the season. It rapidly strengthened and on October 22 at 12:00 UTC, it reached its peak intensity. Soon afterward, increasing wind shear and cooling SSTs began to weaken Omega. Then, 48 hours later, Omega weakened to a tropical depression. It then moved westwards and produced intermittent convection despite the hostile conditions. After succumbing to the hostile conditions, it finally degenerated into a remnant low on October 28 at 12:00 UTC. It then made landfall over the Abaco Islands in the Bahamas the following day, October 29 at 06:00 UTC. It dissipated 6 hours later.

In the Bahamas, not much occurred apart from heavy rainfall. No deaths and damages were reported.

Tropical Depression Fifty-nine (59L)
On October 19 at 12:00 UTC, a disturbance detached from the ITCZ, it moved westwards then completed a counter-clockwise loop and then turned north. Forty-eight hours later, the disturbance developed into Tropical Depression Fifty-nine, becoming the fifty-ninth depression of the season. It reached its peak intensity on October 22 at 00:00 UTC. It then curved north and then northwest. It then curved east-northeast and then entered a hostile environment. It degenerated into a remnant low on October 28 at 06:00 UTC due to increasing wind shear and cooling SSTs. The remnants meandered and then dissiapted two days later at 18:00 UTC.

In Guyana, Suriname, and French Guiana, those areas were affected by the precursor by the heavy rainfall. No deaths and damage occurred, especially in its cyclone stage.

Tropical Depression Sixty (60L)
On October 19, a tropical wave left West Africa. It slowly developed and merged with a disturbance on October 23. The disturbance then moved towards the Bahamas with further developement occuring over the Bahamas. On October 26 at 18:00 UTC, the disturbance developed into Tropical Depression Sixty, becoming the sixtieth and last depression of the season. The depression then made landfall over Hollywood, Florida at peak intensity 6 hours later. It then degenerated into a remnant low another 6 hours. It then moved north and then moved out at sea. It then encountered unfavorable conditions and dissipated on October 29 at 18:00 UTC.

In the Bahamas and Florida, the system dumped heavy rainfall in some areas it passed over or near as a depression. No deaths were reported. Minimal damage was reported.

Function of the STCC Naming System
The following list of names was used for systems that reached tropical storm strength in the North Atlantic in 2019. The names that were not retired will be used again in 2025. Before, the NHC controlled the naming list but, when Andrea formed, STCC Atlantic took control of the naming list. This is List 1 of the STCC naming list. If the naming list reached W and a new system forms and strengthens to a tropical storm. We will move on to the Greek list. It first uses the latest naming list from the NHC. They have a new system of retiring names. They give the WMO names to use and tell them to create a poll for them to know what replacement name people want, if the probability is 5%-100%. If the name is retired, the name with the most votes will be used for the next season (2025).

Here is the chances of a storm getting retired:

Low chance (0%-40%): If a storm caused below $100 million in damage and/or below 100 deaths.

Medium chance (40%-60%): If a storm caused between $100-$1 billion in damage and/or between 100-200 deaths.

High chance (60%-100%): If a storm caused above $1 billion in damage and/or above 200 deaths.

STCC List 1 Names

 * Andrea (01L)
 * Barry (02L)
 * Chantal (03L)
 * Dorian (05L)
 * Erin (06L)
 * Fernand (07L)
 * Gabrielle (08L)
 * Humberto (09L)
 * Imelda (10L)
 * Jerry (11L)
 * Karen (12L)
 * Lorenzo (13L)
 * Melissa (14L)
 * Nestor (15L)
 * Olga (18L)
 * Pablo (19L)
 * Rebekah (21L)
 * Sebastien (22L)
 * Tanya (23L)
 * Van (24L)
 * Wendy (25L)

Greek Names

 * Alpha (26L)
 * Beta (27L)
 * Gamma (29L)
 * Delta (30L)
 * Epsilon (32L)
 * Zeta (31L)
 * Eta (33L)
 * Theta (34L)
 * Iota (35L)
 * Kappa (36L)
 * Lambda (38L)
 * Mu (40L)
 * Nu (43L)
 * Xi (44L)
 * Omicron (46L)
 * Pi (47L)
 * Rho (48L)
 * Sigma (50L)
 * Tau (49L)
 * Upsilon (51L)
 * Phi (52L)
 * Chi (53L)
 * Psi (56L)
 * Omega (58L)

Legend: Normal - Peaked as a tropical storm

Bold - Peaked as a hurricane

Bold and Italic - Peaked as a major hurricane

Chanches of Named Storms Getting Retired
This is a list of named storms getting retired, which only occurs for STCC List 1 Names and not for depressions and Greek named storms, even if they were damaging or deadly. The chance of a name being retired is listed in the function on the naming system.
 * Andrea - 25%
 * Barry - 55%
 * Chantal - 20%
 * Dorian - 45%
 * Erin - 0%
 * Fernand - 15%
 * Gabrielle - 35%
 * Humberto -50%
 * Imelda - 35%
 * Jerry - 30%
 * Karen - 15%
 * Lorenzo - 25%
 * Melissa - 45%
 * Nestor - 60%
 * Olga - 10%
 * Pablo - 45%
 * Rebekah - 75%
 * Sebastien - 60%
 * Tanya - 0%
 * Van - 80%
 * Wendy - 0%

Retirement
In the spring of 2020, the WMO will announce the retirement names. After the announcement, STCC Atlantic will be notified by the WMO about the names that were retired. STCC Atlantic will then give the WMO the replacement names of the retired names the most votes but the results will be finalized first. Then, they will give the WMO the name with the most votes. The WMO will then announce the replacement names.