The 2024-25 Roambatoane hurricane season was a hyperactive and exceptionally impactful Roambatoane hurricane season that ranks as the costliest and second-most active on record. Additionally, 21 storms reached hurricane intensity this season, the most on record. The season officially began on October 16, 2024 and ended on April 26, 2025, though the last storm of the season, Fromidar, formed on April 28, 2025 and dissipated 5 days later. On October 10, 2024, the Teelmondo Tropospheric Surveillance Center (TTSC) stated that the ongoing 2023-25 Oceanic Subsurface Temperature Anomaly (OSTA) and a relative lack of strong low-level wind shear will contribute to "what could be the most active season since 1993-94". The season was defined by an aggressive start, severe impacts, and near-constant activity.
The 2024-25 Roambatoane hurricane season produced 35 depressions, 33 tropical storms (including one unnamed tropical storm), a record-breaking 21 hurricanes, and 12 major hurricanes. Additionally, a record 5 systems this season intensified into Category 5 hurricanes, of which 3 of them (Calron, Flaas, and Hoama) formed before the month of December. Several storms caused severe impacts this season. Calron, Hoama, Reltiu, and Axaly all caused over $10 billion (2024 USD) in damages each, while the former two plus Flaas and Ezanti all claimed over 100 lives. Calron, in particular, became one of the most devastating tropical cyclones in the basin's history; with over $191 billion (2024 USD) in damages and more than 4,500 fatalities, the hurricane became the costliest and deadliest in Vaerhuban history, as well as the third-costliest and second-deadliest tropical cyclone in the basin overall. Hurricane Xalu spent more time at Category 5 intensity than any other system in the basin, spending an accumulated total of 128 hours at that intensity.
Seasonal forecasts[]
| Source | Date | Tropical storms | Hurricanes | Major hurricanes | Refs |
| Average | 20.8 | 12.2 | 6.2 | [Note 2] | |
| Record high activity | 34 | 21† | 14 | ||
| Record low activity | 11 | 5 | 1 | ||
| TTSC | October 10, 2024 | 24-27 | 15-18 | 9-13 | |
| CWCB | October 15, 2024 | 20-24 | 11-14 | 7-10 | |
| CWCB | November 4, 2024 | 21-24 | 12-15 | 7-10 | |
| TTSC | November 11, 2024 | 23-27 | 17-20 | 10-13 | |
| STWC | November 22, 2024 | 23-30 | 12-17 | 8-12 | |
| SHC | November 23, 2024 | 19 | N/A | N/A | |
| AOTSS | November 24, 2024 | 22-25 | 13-16 | 6-9 | |
| CHC | November 26, 2024 | 26-32 | 12-16 | 6-8 | |
| TTSC | November 26, 2024 | 24-27 | 17-20 | 10-14 | |
| TACO | November 30, 2024 | 13 | 7 | 4 | |
| AOTSS | November 30, 2024 | 22-25 | 13-16 | 6-9 | |
| DTCHTC | November 30, 2024 | 25 | 10 | 5 | |
| TACO | December 4, 2024 | 19 | 15 | 6 | |
| SHC | December 7, 2024 | 20 | 14 | 8 | |
| Actual activity | 33 | 21 | 12 |
Each season, various weather prediction centres issue their forecasts concerning the season's activity. The first forecast was issued by the Teelmondo Tropospheric Surveillance Center (TTSC) on October 10, 2024 and predicted a hyperactive season with 24-27 named storms, 15-18 hurricanes, and 9-13 major hurricanes. They cited, among other factors, the ongoing 2023-24 Oceanic Subsurface Temperature Anomaly (OSTA), which increases ocean surface temperatures in the Roambatoane Ocean and stifles the development of oceanic wind shear, as contributing to what will likely be "the most active season in many years, possibly decades". On October 15, the CW Cyclone Bureau (CWCB) released their first prediction for the season, calling for an above-average season with 20-24 named storms, 11-14 hurricanes, and 7-10 major hurricanes. The CWCB updated their forecasts on November 4, increasing the number of named storms and hurricanes to reflect the active start to the season. On November 11, the TTSC issued updated predictions, calling for 23-27 named storms, 17-20 hurricanes, and 10-13 major hurricanes. On November 22, the Soilaf Tropical Warning Center (STWC) predicted a potentially near-record season with 23-30 named storms, 12-17 hurricanes, and 8-12 major hurricanes. A day later, the Spikikonian Hurricane Center (SHC) predicted that 19 named storms would form during the season. The Archaeian Ocean Tropical Surveillance System (AOTSS) issued their outlook on November 24, foreseeing an active season with 22-25 named storms, 13-16 hurricanes, and 6-9 major hurricanes. Furthermore, the AOTSS predicted additional impacts across Sotoray, Vaerhubo, and Malrom Island, as well as at least 1 additional Category 5 hurricane, possibly approaching Flaas in strength. The Catalanotto Hurricane Center (CHC) issued their forecast on November 26, calling for a hyperactive season with 26-32 named storms, 12-16 hurricanes, and 6-8 major hurricanes. They predicted that the season would also witness 3-4 additional Category 5 hurricanes, as well as a rare landfall in Teelmondo. The same day, the TTSC updated their predictions slightly, calling for slightly more major hurricanes due to the aggressive pace of activity. November 30 saw the issuance of 3 predictions; The Aviation Control Optimizer (TACO) unexpectedly called for an extremely quiet season with just 13 named storms, 7 hurricanes, and 4 major hurricanes, while the AOTSS reiterated their previous prediction of 22-25 named storms, 13-16 hurricanes, and 6-9 majors. Finally, the DTC Hurricane Tracking Center (DTCHTC) predicted an unusual season with 25 named storms, 10 hurricanes, and 5 major hurricanes, the latter two being below-average. TACO updated its forecasts significantly on December 4, now predicting a near-normal season with 19 named storms, 15 hurricanes, and 6 major hurricanes. Following 3 days later, the SHC updated their predictions, now calling for an overall active year producing 20 named storms, 14 hurricanes, and 8 major hurricanes.
Seasonal summary[]
Hurricane Calron moving towards Vaerhubo between October 28 and 31
Early season[]
| Costliest Roambatoane hurricane seasons | |||||
|---|---|---|---|---|---|
| Rank | Season | Damage | Refs | ||
| 1 | 2024-25 | >$371.13 billion | |||
| 2 | 2000-01 | $272.88 billion | |||
| 3 | 2015-16 | $255 billion | |||
| 4 | 2016-17 | $173.19 billion | |||
| 5 | 2023-24 | $158.302 billion | |||
| 6 | 2013-14 | ≥$144.47 billion | |||
| 7 | 1987-88 | $125 billion | |||
| 8 | 1991-92 | $115 billion | |||
| 9 | 1997-98 | >$114.2 billion | |||
| 10 | 2010-11 | $96.03 billion | |||
The 2024-25 Roambatoane hurricane season officially began on October 16, 2024. However, Hurricane Avatama, the season's first system, did not materialize until 4 days later. It slowly intensified and then hit Malrom Island on October 23. A day later, Tropical Storm Buar formed. Buar struggled with environmental inhibitions, which resulted in the storm remaining weak and disorganized its entire life. As Buar was degenerating into a remnant low, Hurricane Calron formed on October 27 and quickly intensified thereafter, reaching Type 5 Tropical System intensity late on October 30. The storm then weakened before making landfall in Vaerhubo on November 1 and stalling for the next couple days. The same day that Calron made landfall marked the formation of short-lived Tropical Storm Delain. Delain quickly moved eastward before making landfall in Oorvelm early on November 3. The system dissipated a day later. After a momentary halt in activity, Hurricane Eleni formed. Slowly strengthening, Eleni became a hurricane on November 11 as it sped to the northeast. Two days later, Hurricane Flaas formed and explosively intensified into a Category 5 hurricane on November 15, before further strengthening into the strongest system in the basin in the month of November early the next day. Less than a day after Flaas formed, Area of Convection 1A developed into Tropical Depression 07, but failed to intensify beyond that before dissipating on November 18. After more than a week with no tropical cyclogenesis, Tropical Storm Geu formed on November 22, bringing heavy rainfall to Vaerhubo, Malrom Island, and the island of Sasastalu-Cleelai. Hurricane Hoama formed on November 25 and began intensifying south of Sotoray, becoming a Category 5 hurricane on November 29. Hoama then made landfall in Malrom Island on December 1, followed by another, much weaker, landfall in Sasastalu the next day. After a short hiatus in tropical cyclone activity, Tropical Storm Ivindi formed on December 6, wandering westward then northeastward for approximately a week before dissipating off the coast of Malrom Island. December 12 saw the formation of Hurricane Jokalom, which churned in the open Roambatoane Ocean for the better part of a week before dissipating. 2 systems formed on December 17: Hurricanes Karisto and Lilio. The storms interacted with one another, causing Lilio to shove Karisto northward. Karisto ultimately had no impact on land, while Lilio stalled just off the coast of Oorvelm, causing moderate flooding in parts of the continent of Ekai. Hurricane Mamasha formed on December 27 and persisted into 2025. Mamasha caused severe damage in Malrom Island after making several landfalls in the country. The last tropical cyclone to form in 2024 during the season was Tropical Storm Ninoom, which formed on December 30 and dissipated the next day after making landfall in eastern Malrom Island.
Peak season[]
WIP
Systems[]
Hurricane Avatama[]
Type 1 Tropical System (TTSS) Category 1 hurricane (SSHWS) 
Duration October 20 – October 26 Peak intensity 75 mph (120 km/h) (1-min)
989 mbar (hPa)
On October 13, the Teelmondo Tropospheric Surveillance Center (TTSC) began monitoring a developing tropical system located far southeast of Malrom Island. Radar scans indicated that the system was consolidating on October 19, with a weak band of convection developing around a poorly-defined core. At 21:00 UTC that day, the TTSC designated the system 1x. At 12:00 UTC on October 20, storm data collection flights found winds of 40 mph, and 1x was upgraded to Tropical Storm Avatama an hour later. Based on pressure reading during that flight that suggested a minimum pressure of 1007 mbar, Avatama was upgraded to a Type 1 Tropical System at the same time. As Avatama continued tracking generally west-northwest, the system's circulation slowly became better organized. At 14:00 UTC on October 21, the TTSC issued Tropical Storm Watches and Warnings for the southwest coast of Malrom Island, as well as a Tropical Storm Watch for the entire coast of Simabo. Throughout the afternoon hours of October 21, the TTSC closely monitored Avatama, noting that minor consolidation of the storm's convection had occurred and therefore the storm had slightly intensified. At 18:00 UTC, the TTSC reminded residents of southwestern Malrom Island that regardless of whether the storm made landfall or not, Avatama would likely pass close enough to the shore to produce locally heavy rainfall across the region. By 00:00 UTC the next day, Avatama's wind speed had risen to 50 mph while its pressure had fallen to 10:00 mbar. As the storm showed no signs of weakening, the TTSC extended the Tropical Storm Warnings on Malrom Island east to Zaracook Inlet. A Tropical Storm Watch was also issued for southern portions of coastal Brimphola at the same time. At 00:00 UTC on October 23, Avatama reached peak intensity with winds of 75 mph, though operationally it was thought to have been slightly weaker. Land interaction caused the storm to quickly fall to 60 mph just 6 hours later. At 16:30 UTC, Avatama made landfall at that intensity near East Waysand Beach, Malrom Island. After landfall, Avatama weakened as its circulation was severely disrupted and it fell below tropical storm strength on October 25 while approximately halfway between Malrom Island and Brimphola. Avatama became post-tropical on October 26 as its circulation degenerated, though the TTSC continued monitoring the system until it was absorbed by a larger cold front the next day.
Prior to landfall, heavy rain from Avatama's rainbands caused flooding across southern Malrom Island. A section of the E52 in Toomalav flooded, forcing the temporary closure of the expressway to all traffic. Toomalav International Airport also saw flooding on the tarmac, causing flight delays and cancellations. Strong winds downed trees and power lines throughout the city of Sebasunc, causing 45 percent of the city to lose power and one person to be electrocuted. Several households were inundated by floodwaters that sparked at least 5 major electrical fires, including one that killed an elderly man. 4 people died after their house was swept away by floodwaters in Klizmakoo. Heavy rainfall resulted in destructive floods in Turony; at least 100 structures in the town were severely damaged, and 15 people drowned after the Turony River burst its banks. 4 people were killed by intense rip currents in East Waysand Beach, while 30 others were rescued. Offshore, a fishing vessel with 6 people onboard capsized on October 23. 3 of the crew were rescued a week later, while the other 3 were confirmed dead. Avatama wrought $1.05 billion (2024 USD) in damages to Malrom Island, while a total of 29 people were killed.
Tropical Storm Buar[]
| Type 1 Tropical System (TTSS) | |
|---|---|
| Tropical Storm (SSHWS) | |
  | |
| Duration | October 24 – October 28 |
| Peak intensity | 40 mph (65 km/h) (1-min) 1005 mbar (hPa) |
On October 23, the TTSC noted a disorganized area of convective thunderstorms developing off the coast of Oorvelm. The system became better defined and was upgraded to Tropical Depression 02 at 19:00 UTC on October 24. The next day at 17:00 UTC, 02 was found to have attained sustained winds of 40 mph, as well as a distinct circulation, though one that was displaced to the northeast of the center. Therefore, the system was immediately named Buar. At that time, Buar's lowest pressure, as indicated by satellite and radar imagery, was estimated at 1006 mbar, resulting in Buar being designated a Type 1 Tropical System. Buar consistently struggled with unfavourable conditions, resulting in the storm becoming heavily sheared and poorly-organized. By 14:00 UTC on October 27, the TTSC noted that Buar had begun weakening as wind shear and cool sea surface temperatures started taking their toll on the storm's convection. Buar weakened below tropical storm strength at 18:00 UTC, though the now ragged and disorganized system still exhibited weak convection 24 hours later. That convection quickly fizzled out, however, and Buar degenerated into a remnant low at 20:00 UTC on October 28.
Hurricane Calron[]
- See also: Effects of Hurricane Calron in Vaerhubo
| Type 5 Tropical System (TTSS) | |
|---|---|
| Category 5 major hurricane (SSHWS) | |
  | |
| Duration | October 27 – November 4 |
| Peak intensity | 160 mph (260 km/h) (1-min) 918 mbar (hPa) |
At 18:00 UTC on October 27, the TTSC issued a Special Tropical Cyclone Development Advisory (STCDA) for a highly reactive convective system located far from land, designated 1x. Just 2 hours later, 1x had developed a well-defined circulation and robust thunderstorm activity near its center, resulting in the storm being upgraded to Tropical Depression 03 by the TTSC. At this time, the TTSC issued the first High-Risk Tropical Cyclone Warning (HRTCW) since 2020, when they issued one for Hurricane Glenalio. At 23:00 UTC, 03 strengthened into Tropical Storm Calron. The storm then began rapidly intensifying as it entered a favourable environment, becoming the first hurricane of the season at 13:00 UTC on October 28. At this time, the storm maintained a robust structure with well-organized convection and began developing an eye. Calron intensified to a Type 2 Tropical System at 16:00 UTC, followed by a Category 2 storm at 00:00 UTC the next day, then a Type 3 Tropical System 12 hours later. As the storm's convection tightened around its core, its eye became large but remained ragged. A Hurricane Emergency was issued for regions of Vaerhubo and Sotoray at 22:00 UTC as Calron's winds increased to 125 mph. Late on October 30, Calron reached peak intensity with winds of 160 mph (260 km/h) and a minimum central pressure of 918 mbar. Operationally, Calron was estimated to have been a Category 4 hurricane at peak, with winds of 145 mph (230 km/h) and a minimum central pressure of 921 mbar. After reaching peak intensity, the upper-level steering current that was causing Calron to accelerate northwest suddenly degenerated, resulting in some uncertainty as to where the storm would track next. At 12:00 UTC the next day, Calron began weakening as an eyewall replacement cycle initiated. Due to a lack of prominent steering currents in the area, Calron's forward movement speed began to fall on November 1, and the storm made landfall near Clearwater Bayou at 18:00 UTC that day as a Category 3 major hurricane. Thereafter, the storm stalled in the vicinity of eastern Vaerhubo for over a day while dropping torrential rainfall. Land interaction and dry air penetration rapidly disrupted Calron's circulation, resulting in the system dropping below hurricane status by 20:00 UTC on November 2. By 12:00 UTC the next day, Calron dropped to tropical depression status due to rapid degeneration of its circulation. The TTSC issued their final advisory for Calron late on November 4 as it was, operationally, considered to have been absorbed by a nearby frontal low. The remnants of Calron were found to have still been active on November 6, but were quickly absorbed by the frontal low later that day,
Tropical storm-force winds began affecting parts of Vaerhubo late on October 31, followed by hurricane-force winds the next day. A wind gust of 137 mph was recorded in Clearwater Bayou late on November 1 as Calron was making landfall. Impacts across Vaerhubo were catastrophic; more than 3,500 people are estimated to have died in the country, with over 2.3 million, or approximately 20% of the population, severely affected. Widespread historic flooding occurred throughout Vaerhubo, most notably in Clearwater Bayou, Murray Beach, Massanami Beach, Masswood, Templeton, and Denfield Hill. Economic losses are estimated to be at least $134 billion (2024 USD). Malrom Island also received flooding rainfall that led to 10 fatalities and destroyed hundreds of homes and businesses. More than 2,000 hectares of crops, equalling approximately 5% of the country's annual soy harvest, were ruined. Damages in Malrom Island reached at least $700 million (2024 USD). An additional fatality in Sotoray was reported after a person was killed by a falling tree.
Tropical Storm Delain[]
| Type 1 Tropical System (TTSS) | |
|---|---|
| Tropical Storm (SSHWS) | |
  | |
| Duration | November 1 – November 4 |
| Peak intensity | 40 mph (65 km/h) (1-min) 999 mbar (hPa) |
A tropical wave originating from the Southeast Gyre on October 26 began showing signs of development 3 days later and the TTSC began tracking it as 1x. Initial organization of the large system's thunderstorm activity was limited, though by October 31 the TTSC noted that the system had developed a warm core and increased convection. The next day, it was upgraded to Tropical Depression 04. Early forecasts showed no additional development for 04 as it was located in an unfavourable environment with moderate wind shear and cool sea surface temperatures left over from Tropical Storm Buar several days prior. However, the large size of 04 allowed it to intensify despite the unfavourable conditions, and it intensified into a tropical storm on November 2. Upon 04 reaching tropical storm status, the TTSC issued Tropical Storm Warnings for Oorvelm and Sembung on short notice. For the next 12 hours, Delain experienced no change in wind speed but saw its pressure drop from 1004 mbar to 999 mbar and its trajectory curve to the north. At 00:00 UTC on November 3, the storm made landfall at peak intensity near Laz Dlem, Oorvelm and began weakening thereafter. Delain weakened to a remnant low on November 4, at which point the TTSC ceased tracking the system.
The large size of Delain at landfall caused a large portion of the continent of Ekai to experience rainfall. Modest street flooding was reported in Limov, Oorvelm and Doonsy, Wazgol. Locally gusty winds cut power to about 10,000 customers across Sembung. Overall damage was minor, and no casualties were reported.
Hurricane Eleni[]
Type 2 Tropical System (TTSS) Category 1 hurricane (SSHWS) 
Duration November 7 – November 15 Peak intensity 80 mph (130 km/h) (1-min)
978 mbar (hPa)
Rigorous convection was noted in an area of low pressure on November 7. The TTSC began tracking the system as Hurricane Hunter flights reported developing outflow and favourable conditions for intensification. At 18:00 UTC that day, the TTSC began issuing advisories on Tropical Depression 05 after the system began displaying a warm core. Early on November 9, the system strengthened into a tropical storm and was given the name Eleni. Traversing a relatively favourable environment with warm ocean temperatures, modest vertical wind shear, and minimal dry air, Eleni steadily intensified over the next day, becoming better organized and more condensed. By 12:00 UTC on November 11, Hurricane Hunter flights found sustained winds of 76 mph in Eleni's well-defined inner circulation, and the storm was promptly upgraded to Category 1 intensity. At 02:00 UTC the next day, Eleni reached peak intensity with winds of 80 mph and a minimum barometric pressure of 978 mbar. Soon thereafter, a trough began pushing Eleni northward. The hurricane entered unfavourable conditions and began weakening at approximately 12:00 UTC, and the TTSC downgraded Eleni to a tropical storm 7 hours later. Early on November 14, Eleni made its closest approach to Brimphola before pulling away. Thereafter, weakening upper-level steering currents caused Eleni to start moving erratically. Further weakening resulted in Eleni weakening to a tropical depression at 12:00 UTC on November 14. Immediately thereafter, the system initiated a nearly 180-degree curve to the southwest as it began transitioning into an extratropical cyclone, which it completed at 19:00 UTC the next day. The extratropical remnants of Eleni persisted until November 17, whereupon it opened up into a trough.
Passing just offshore, Eleni brought gusty winds and moderate rainfall to Simabo, Brimphola, and Malrom Island. Street flooding and power outages were reported in a few cities in southeastern Brimphola and western Malrom Island, while a rare EF1 tornado damaged 2 farmhouses near Wathuma. No fatalities occurred due to Eleni, though 4 people were injured by flying debris in Duwara. The TTSC reported that parts of Malrom Island that were still recovering from Avatama less than a month prior "dodged a bullet" by being missed by the heaviest rainfall, thereby avoiding further flooding. Total damages from Eleni are estimated to be around $25 million (2024 USD).
Hurricane Flaas[]
Type 5 Tropical System (TTSS) Category 5 major hurricane (SSHWS) Duration November 13 – November 27 Peak intensity 185 mph (295 km/h) (1-min)
901 mbar (hPa)
A tropical wave developed into Potential Tropical Cyclone 2A on November 13. At 12:00 UTC, the system was found to have transitioned into Tropical Storm Flaas while located far southeast of Jacksonville, Sotoray. Despite traversing through a cold wake left by Hurricane Eleni just a few days prior, Flaas continued intensifying throughout the day. Late that day, Flaas began rapidly deepening due to the onset of a Tropical Development Event (TDE), becoming a hurricane at 00:00 UTC on November 14. Travelling slowly to the west, Flaas' convection rapidly developed large, potent rainbands and a large eye began to form. As the system quickly organized and condensed, explosive intensification began at 22:00 UTC, after which TTSC Hurricane Hunters found that Flaas had strengthened from Category 2 to Category 4 intensity in 3 hours. While this explosive rate of intensification was short-lived, Flaas continued to intensify throughout the morning hours of November 15, as noted by a TTSC Hurricane Hunters surveillance flight that found 1-minute sustained winds of 155 mph in Flaas' eastern eyewall at 12:00 UTC that day. Just 7 hours later, Flaas's 1-minute sustained winds had increased to 175 mph, therefore making it a Category 5 hurricane. At 03:00 UTC on November 16, Flaas reached peak intensity with winds of 185 mph and a minimum pressure of 901 mbar, making it the strongest tropical cyclone in the basin in the month of November on record. Soon after, however, the onset of an eyewall replacement cycle caused the storm to weaken to a Category 4 storm at 20:00 UTC. The storm's forward movement speed fell to just 5 mph on November 17 as a nearby frontal low inhibited local steering currents, causing upwelling that, along with the ongoing Eyewall Replacement Cycle, quickly degraded Flaas' convective field. A TTSC Hurricane Hunter flight into Flaas at 10:00 UTC found the hurricane's eye clouding over and confirmed that the new eyewall was almost completely formed. Due to instruments measuring maximum 1-minute sustained winds of 125 mph at that time, Flaas was downgraded to a Category 3 hurricane. The next day at 00:00 UTC, Flaas weakened below major hurricane intensity as its Eyewall Replacement Cycle was completed.[1] Soon after, the hurricane began turning to the southwest and accelerating due to the influence of a nearby trough. Radar scans indicated that the system had ceased weakening around 02:00 UTC; its 1-minute sustained winds had fallen to 105 mph, while its minimum central pressure had risen to 971 mbar. The storm began reintensifying just hours later and reattained major hurricane status at 14:00 UTC.[2] At 13:00 UTC on November 20, Flaas reached a secondary peak intensity as a Category 4 storm with winds of 145 mph (230 km/h) and a minimum pressure of 935 mbar (hPa). At this time, the hurricane's movement had also begun taking a more westerly course that brought it into less favourable conditions. The storm started weakening again at 18:00 UTC due to moderate vertical wind shear, cool sea surface temperatures of only 24-27 degrees Celsius, and the onset of a second Eyewall Replacement Cycle, the latter of which was confirmed by TTSC weather satellites that observed a second eyewall developing.[3] By 20:00 UTC on November 21, Flaas weakened below major hurricane intensity. The system further weakened to tropical storm intensity 24 hours later, and passed just off the coasts of Oorvelm and Sembung on November 24. Very early the next day, Flaas made landfall near Sumbrayol, Sireyalo Major as a minimal tropical storm. As the system pulled away from the Sireyalo Islands late on November 25, satellite data indicated unexpected bursts of convection in Flaas' northeastern quadrant, and Hurricane Hunter flights found 1-minute sustained winds of 65 mph the next day at 01:00 UTC. This second bout of reintensification, and Flaas' long-lived and powerful nature as a whole, caused the TTSC to dub it "the Immortal Gale", a term that began circulating widely online. Becoming a Category 1 hurricane at 12:00 UTC, Flaas made landfall 3 hours later near Simaphola, Brimphola with 1-minute sustained winds of 85 mph. Inland, the system began rapidly weakening over the mountainous Brimpholan terrain; by 12:00 on November 27, Flaas had weakened to a tropical depression over central Brimphola. 6 hours later, Flaas degenerated into a remnant low while situated over southern Nobora.
Rough surf began affecting parts of the Oorvelmish coast late on November 22, resulting in several reports of coastal erosion. Hurricane Flaas caused damaging flash flooding in Oorvelm, Sembung, Wazgol, the Sireyalo Islands, Teelmondo, Simabo, and Brimphola, with economic losses from the storm estimated to be at least $3.02 billion (2024 USD). The large size of Flaas' wind field on November 24 resulted in sustained tropical storm-force winds being recorded in Teelmondo for the first time since 2002. A total of 137 fatalities were attributed to Flaas: 1 in Vaerhubo due to rip currents, 30 in Oorvelm, 10 in Sembung, 4 in Wazgol, 62 in the Sireyalo Islands, 1 in Teelmondo, 2 in Simabo, and 27 in Brimphola.
Initially, Flaas' minimum barometric pressure was estimated by the TTSC to have been 889 mbar at its lowest; however, skepticism over the TTSC' estimates for the storm's intensity developed, mostly focused on the fact that the organization claimed that the storm reached peak intensity at 06:00 UTC on November 16 despite the fact that satellite data from that time indicated that Flaas was already undergoing an Eyewall Replacement Cycle at that time. Due to mounting pressure from the public, the Teelmondo government ordered an entire reanalysis on the storm. The findings, revealed in the post-season report, found that the storm's pressure had been vastly inflated by the TTSC in an attempt to "make people take the storm seriously". The real data revealed that Flaas had actually reached a peak intensity of 901 mbar at 03:00 UTC on November 16; these findings were reflected in the post-season analysis on July 10, 2025. The TTSC' decision to intentionally overstate the intensity of Flaas led to public outrage and demands for the resignation of TTSC chairman CyclonicWrath765. CyclonicWrath765 soon issued a public apology on behalf of the TTSC, expressing "deep regret" for the "gross mishandling of vital facts". This scandal led to calls for the founding of more weather bureaus, considering the fact that the entire Roambatoanian basin is monitored almost exclusively by the TTSC.
Tropical Storm 07[]
| Type 1 Tropical System (TTSS) | |
|---|---|
| Tropical Storm (SSHWS) | |
  | |
| Duration | November 14 – November 18 |
| Peak intensity | 40 mph (65 km/h) (1-min) 1008 mbar (hPa) |
A tropical wave originating far out to sea on November 10 tracked westward over the next several days before showing signs of gradual development. The TTSC began monitoring the system for tropical cyclogenesis at 04:00 UTC on November 14. After remote data collecting modules dropped into the system found evidence of a developing warm core, the TTSC designated the system Tropical Depression 07 at 11:00 UTC. Further development was minimal due to dry air wearing at the system's convection. However, the system was found to have briefly attained tropical storm status and was upgraded to a tropical storm in the final post-season report. At 23:00 UTC, 07's pressure bottomed out at 1008 mbar. Increasingly hostile conditions started slowly weakening 07 on November 15 as it slowly tracked towards Oorvelm. A high-pressure system situated over southern Oorvelm resulted in 07 beginning to accelerate westward on November 16, then abruptly curve to the north early on November 18 as the system weakened into a remnant low. At that point, the TTSC issued its last advisory on the system.[4]
Tropical Storm Geu[]
Type 1 Tropical System (TTSS) Tropical Storm (SSHWS) Duration November 22 – November 25 Peak intensity 45 mph (75 km/h) (1-min)
1001 mbar (hPa)
An Area of Convection located near Vaerhubo developed into Potential Tropical Cyclone 5A late on November 22. At 00:00 UTC on November 23, 5A developed tropical characteristics and was designated Tropical Depression 08 by the TTSC. By 12:00 UTC, 08 had strengthened into Tropical Storm Geu while located north of Final Point, Malrom Island. A subtropical ridge to the south caused Geu to turn north on November 24. Amid increasingly hostile conditions, Geu transitioned into an extratropical cyclone at 12:00 UTC on November 25.
As Area of Convection 5A, Geu brought heavy rainfall to areas of Vaerhubo still recovering from Calron less than a month prior. Flash flooding was reported in Massanami Beach and Tonnagor, while over 1,000 people lost power in Clearwater Bayou. 4 people perished in Vaerhubo.
Hurricane Hoama[]
Type 5 Tropical System (TTSS) Category 5 major hurricane (SSHWS) Duration November 25 – December 3 Peak intensity 180 mph (285 km/h) (1-min)
899 mbar (hPa)
A tropical depression formed far south of Sotoray on November 25. The TTSC noted favourable atmospheric conditions and predicted significant intensification. While the depression, designated as 09 by the TTSC, initially struggled to organize, it reached tropical storm status at 11:00 UTC on November 26 and was given the name Hoama. Thereafter, the system turned due west and began intensifying at a quicker pace, becoming a hurricane early the next day. Around this time, Hoama turned slightly to the north due to a frontal ridge to its south. As the system tracked to the northwest throughout November 28, conditions became significantly more conductive for development, and Hoama initiated a period of rapid intensification at 17:00 UTC. Two hours later, it attained major hurricane status as convection tightened around a developing eye. Continuing to rapidly intensify, Hoama reached Category 5 intensity at 16:00 UTC on November 29, becoming the second-strongest tropical cyclone in the basin in the month of November in terms of 1-minute sustained winds, only behind Flaas. As Hoama turned more to the north, the storm's circulation grew to 690 miles in diameter; one TTSC forecaster mentioned that it was "probably the most massive system in years". At 13:00 UTC on December 1, Hoama made landfall near Toomalav Beach, Malrom Island with 1-minute sustained winds of 175 mph and a minimum central pressure of 919 mbar. Thereafter, the storm rapidly weakened, dropping to Category 1 status by 00:00 UTC on December 2. Late on December 2, Hoama made a second landfall near Renabyem, Sasastalu as a minimal tropical storm. By 10:00 UTC the next day, it became post-tropical over northern Sasastalu. Very shortly thereafter, Hoama was absorbed by a large extratropical low just off the coast of Cleelai.
As an extremely powerful hurricane, Hoama brought widespread and devastating impacts to Malrom Island throughout December 1, the full extent of which were covered up by the Malromian government for over a year. 856 fatalities have been confirmed in the country, though the TTSC estimates that over 2,500 people may have perished. Significantly more limited effects occurred in Sasastalu and Cleelai, though Hoama did produce a storm surge in Arybuche, Sasastalu that damaged 14 beachfront properties and contributed to ongoing coastal erosion started by Tropical Storm Geu in late November. Additionally, a person in Cleelai was killed by rip currents.
Tropical Storm Ivindi[]
| Type 2 Tropical System (TTSS) | |
|---|---|
| Tropical Storm (SSHWS) | |
  | |
| Duration | December 6 – December 13 |
| Peak intensity | 70 mph (110 km/h) (1-min) 983 mbar (hPa) |
An Area of Convection, designated 6A by the TTSC, was spawned by the Southeast Gyre late on December 5 and quickly began organizing, resulting in the TTSC declaring it a potential tropical cyclone at 00:00 UTC on December 6. 12 hours later, the southwestward-traveling system transitioned into a tropical depression as it experienced moderately favourable atmospheric conditions. Early the next day, it further strengthened into a tropical storm and was named Ivindi by the TTSC. This was quickly followed by an abrupt turn to the north due to Ivindi interacting with the Southeast Gyre's outer air circulation. On December 9, Ivindi reached peak intensity with 1-minute sustained winds of 70 mph and a minimum central pressure of 983 mbar, equivalent to a Type 2 Tropical System. The system turned to the northeast throughout December 10 while slowly weakening. By December 13, Ivindi had lost all tropical characteristics and was declared post-tropical while located west-southwest of Malrom Island.
The post-tropical remnants of Ivindi brought minor rainfall to areas of Malrom Island already well-saturated from Avatama and Hoama. However, overall rainfall from the remnants of Ivindi was negligible and caused no impacts.
Hurricane Jokalom[]
| Type 4 Tropical System (TTSS) | |
|---|---|
| Category 4 major hurricane (SSHWS) | |
  | |
| Duration | December 12 – December 18 |
| Peak intensity | 145 mph (230 km/h) (1-min) 940 mbar (hPa) |
On December 11, the TTSC noted an area of scattered thunderstorms located well southeast of Vaerhubo. Hindered by poor atmospheric conditions, the low pressure area initially failed to develop robust convection as it crept westward. However, conditions started improving by 16:00 UTC the next day, and the system strengthened into a tropical depression 2 hours later. Bursts of convection were noted on December 13 as the depression travelled over the warmer waters located east of the Southeast Gyre. By 14:00 UTC that day, the depression was showing signs of increased development and was named Jokalom. Jokalom proceeded to rapidly intensify as conditions became favourable, with minimal wind shear, warm sea surface temperatures, and little to no dry air intrusion. By 20:00 UTC, Jokalom was upgraded to a Category 1 hurricane, followed by Category 2 status 4 hours later. The storm's rapid intensification phase continued for another 12 hours; at 12:00 UTC on December 14, Hurricane Jokalom started to encounter stronger wind shear and slightly cooler sea surface temperatures. At that time, Jokalom was confirmed to have reached peak intensity as a mid-range Category 4 hurricane. The increasingly harsh conditions soon caused Jokalom to weaken, with the storm dropping below major hurricane strength by 06:00 UTC on December 15. A few hours later atmospheric conditions improved slightly, but not enough to stop Jokalom's weakening trend. Over the next couple of days, the storm gradually weakened while crawling slowly westward. By 18:00 UTC on December 17, Jokalom dropped below hurricane strength as its central core began to collapse. By 12:00 UTC the next day, the system weakened to a tropical depression, and was declared a remnant low 6 hours later, having never affected land during its existence.
Hurricane Karisto[]
| Type 2 Tropical System (TTSS) | |
|---|---|
| Category 2 hurricane (SSHWS) | |
  | |
| Duration | December 17 – December 20 |
| Peak intensity | 100 mph (155 km/h) (1-min) 972 mbar (hPa) |
A sprawling area of low pressure located in the middle of the Roambatoane Ocean unexpectedly developed into a tropical depression early on December 17. The TTSC began monitoring the system, noting the possibility of rapid intensification as it traversed through warm waters and minimal wind shear. By 10:00 UTC, the system was upgraded to tropical storm status and given the name Karisto. The storm quickly intensified, reaching hurricane status by 22:00 UTC. At this point, Karisto was a large system, with gale-force winds spanning approximately 450 miles across. By 08:00 UTC on December 18, Karisto briefly attained Category 2 status, subsequently peaking with winds of 100 mph (155 km/h). By 12:00 UTC, the system entered a cold wake left behind by Jokalom, causing its northern eyewall to erode. The hurricane began weakening, with radar scans failing to detect hurricane-force winds by 20:00 UTC; the storm was therefore downgraded to tropical storm strength. Hurricane Lilio, located several hundred miles to the southwest, forced Karisto slightly northward, then abruptly eastward. Travelling northeastward at 00:00 UTC on December 19, Karisto's weakening halted as the system entered more favourable conditions, though inflow from Lilio ultimately began eroding Karisto's core later that day. By 18:00 UTC, Karisto weakened to a tropical depression as it began losing its convection. The storm managed to produce a few small bursts of convection throughout the early hours of December 20, but fell apart as a nearby stationary front began absorbing Karisto. Karisto was declared a remnant low at 08:00 UTC and was fully absorbed by the front 12 hours later.
Hurricane Lilio[]
Type 3 Tropical System (TTSS) Category 3 major hurricane (SSHWS) Duration December 17 – December 23 Peak intensity 115 mph (185 km/h) (1-min)
960 mbar (hPa)
A tropical wave located well east-southeast of Oorvelm developed into a tropical depression on December 17. Moving slowly westward, the depression steadily intensified, becoming Tropical Storm Lilio at 12:00 UTC that day. Influenced by relatively weak mid-level currents, Lilio continued to drift westward through warm waters and minimal wind shear. By 20:00 UTC, Lilio was upgraded to a Category 1 hurricane while located 400 miles east of Oorvelm. At 14:00 UTC on December 18, Lilio reached Category 2 intensity and began interacting with a weakening Karisto, pushing the weaker system to the northeast. Lilio reached peak intensity at 21:00 UTC as a Category 3 major hurricane. The storm's movement slowed to a crawl, causing it to stall approximately 150 miles east of Limov, Oorvelm. Lilio remained just offshore for the next 48 hours, barely moving while maintaining peak intensity. Finally, the system began weakening on December 22 due to upwelling, dropping below hurricane status by 18:00 UTC that day. Lilio began drifting slowly to the northeast early on December 23, displaying a disorganized and exposed core with limited convection. The TTSC declared Lilio post-tropical at 12:00 UTC after the system's convection collapsed entirely.
Despite never making landfall, Lilio dropped heavy rainfall over parts of the continent of Ekai as it stalled just offshore. Moderate flooding occurred in Oorvelm and Sembung, while more limited effects were felt in Wazgol. Rainfall peaked at 210 mm in Dykegreen, Oorvelm, where the Eastwood River overtopped its banks and flooded thousands of hectares of farmland. The Yarsi River in Sembung also overflowed, wrecking many hectares of crops. Damage to the agricultural sector in Oorvelm and Sembung totalled $235 million (2024 USD). A total of 7 fatalities were confirmed, all in Oorvelm.
Hurricane Mamasha[]
Type 3 Tropical System (TTSS) Category 4 major hurricane (SSHWS) Duration December 27, 2024 – January 1, 2025 Peak intensity 140 mph (230 km/h) (1-min)
944 mbar (hPa)
An Area of Convection formed on December 27 300 miles southeast of Sotoray. Throughout the day, the system, dubbed 1XA by the TTSC, slowly built up convection, though it remained weak and disorganized. By 20:00 UTC, 1XA had developed tropical characteristics and was subsequently upgraded to a tropical depression. The system passed just off the Sotoran coast early on December 28, simultaneously intensifying into Tropical Storm Mamasha. As Mamasha moved away from Sotoray, it encountered a favourable environment and began rapidly intensifying; by 12:00 UTC, Mamasha was upgraded to Category 1 intensity, followed by Category 2 intensity 4 hours later. A building ridge located near Vaerhubo shoved Mamasha southward around 22:00 UTC, at which time the hurricane was upgraded to Category 3 intensity. Subsequently, Mamasha developed a pinhole eye and robust rainbands as it trekked southwestward. At 04:00 UTC on December 29, Mamasha reached peak intensity while located 120 miles south of Vaerhubo. After maintaining that intensity for the next 8 hours, Mamasha began an Eyewall Replacement Cycle (ERC) at 12:00 UTC. The storm's northern eyewall degraded rapidly, and the storm had weakened to high-end Category 2 intensity by 00:00 UTC the next day. Although the ERC was completed at that point, Mamasha was now entering a slightly more hostile environment with 20-knot vertical wind shear and sea surface temperatures of 26-27 degrees Celsius. Meanwhile, the ridge over Vaerhubo now drew Mamasha northward as the hurricane continued to interact with the pressure gradient. Mamasha's forwards movement speed fell quickly over the course of December 30, dropping from 16 mph at 02:00 UTC to just 6 mph at 12:00 UTC. At 17:00 UTC, Mamasha made its first landfall near Marrorway Beach, Malrom Island with sustained winds of 100 mph. Due to the direction Mamasha was travelling at the time, the storm's now-ragged eye only remained over land for an hour or so before reemerging over the Gulf of Redbird. Still travelling slowly west-northwestward, Mamasha dropped to Category 1 status at 03:00 UTC on December 31. 3 hours later, it made its second landfall near the city of Waysand Beach with winds of 80 mph. Again, Mamasha did not remain over land for very long, and its convective core entered Toomalav Bay around 08:00 UTC that day. Due to the inflow from Tropical Storm Ninoom, which was located only 300 miles to Mamasha's southeast, Mamasha was pulled slightly to the south, turning due west as it weakened to a tropical storm. Between 20:00 UTC on December 31 and 04:00 UTC on January 1, Mamasha abruptly turned back to the northwest while weakening to a minimal tropical storm, subsequently making its final landfall near Wiskaga Beach on January 1 at 06:00 UTC. Thereafter, Mamasha's convection quickly fell apart over Malrom Island's mountainous terrain, and Mamasha weakened to a remnant low by 15:00 UTC that same day.
Mamasha never strayed far from land during its lifetime, bringing widespread and torrential rainfall to Sotoray, Vaerhubo, and Malrom Island. Sotoray saw up to 175 mm of rain fall in some places while Mamasha passed south of the island early on December 28, though no damage or fatalities were reported. Although Vaerhubo saw moderate flooding and landslides from the outer bands of Mamasha, the southward turn late on December 28 spared the country from the worst of the storm. Several beachside houses in Tonnagor were inundated by Mamasha's storm surge, and the Whistling River burst its banks. By far the worst impacts were in Malrom Island, which was recovering from impacts from Hurricane Hoama a month prior. Mamasha's slow movement and interaction with Malrom Island's mountainous terrain caused flooding rain over much of the country. Waysand Beach, Turony, and Varzbruk were all severely impacted by Mamasha. The storm claimed 46 lives, of which 5 were in Vaerhubo and 41 were in Malrom Island. Total economic losses from Mamasha reached $6.93 billion (2024 USD), most of which was wrought upon Malrom Island.
Tropical Storm Ninoom[]
| Type 1 Tropical System (TTSS) | |
|---|---|
| Tropical Storm (SSHWS) | |
  | |
| Duration | December 30 – December 31 |
| Peak intensity | 50 mph (85 km/h) (1-min) 1009 mbar (hPa) |
The TTSC noted an Area of Interest located south-southwest of Vaerhubo on December 29. Throughout the day, the system curved to the north, driven by a pressure gradient and inflow from Hurricane Mamasha. Early the next day, the system started to develop more robust convection and subsequently intensified into a tropical depression at 06:00 UTC. The storm steadily intensified, becoming a tropical storm around 12:00 UTC. Approaching eastern Malrom Island from the south, Ninoom reached peak intensity at 16:00 UTC and made landfall in White Ray Lagoon, Malrom Island an hour later, still at peak intensity. Inland, Ninoom's convection steadily deteriorated, and the storm was declared a remnant low at 08:00 UTC on December 31. The remnants of Ninoom accelerated to the northeast and opened into a trough late that day.
Ninoom brought modest impacts to eastern Malrom Island; flooding claimed 2 lives and caused $100 million (2024 USD) in damages.
Hurricane Opasko[]
| Type 3 Tropical System (TTSS) | |
|---|---|
| Category 3 major hurricane (SSHWS) | |
  | |
| Duration | January 2 – January 6 |
| Peak intensity | 115 mph (185 km/h) (1-min) 961 mbar (hPa) |
At 16:00 UTC on January 1, the TTSC noted an Area of Convection containing scattered thunderstorms. Located far southeast of Meisiow, the system gradually intensified, though it remained disorganized; by 06:00 UTC on January 2, the system had sustained winds of 40 mph but hadn't developed tropical characteristics. It finally developed into a tropical cyclone at 11:00 UTC and was given the name Opasko. Thereafter, Opasko proceeded to steadily intensify in a favourable environment. A mounting high-pressure system pulled Opasko slightly northward as it intensified into a hurricane early on January 3. At 06:00 UTC, Opasko reached Category 2 status, followed by Category 3 intensity at 14:00 UTC, at which time a well-defined eye had developed. Simultaneously, Opasko peaked as a low-end Category 3 hurricane with sustained winds of 115 mph. Although Opasko maintained this intensity for 10 hours, it was entering a less favourable environment with cooler sea surface temperatures and moderate wind shear. At 00:00 UTC on January 4, Opasko dropped back down to Category 2 intensity as its eye began to cloud over and its convection started to become displaced to the south. However, Opasko only slowly weakened over the course of the next few days. Early on January 5, now at Category 1 intensity, Opasko started a broad curve to the northeast while entering even colder waters to the south of Meisiow. At 12:00 UTC, now travelling almost due north, the storm was downgraded to tropical storm intensity and continued to weaken while pulling eastward. By 04:00 UTC on January 6, Opasko had weakened to a tropical depression and soon thereafter began transitioning to an extratropical cyclone. It completed this transition by 20:00 UTC, persisting as an extratropical cyclone for the next 24 hours before being absorbed into a cold front the next day.
Tropical Storm Pyreum[]
| Type 1 Tropical System (TTSS) | |
|---|---|
| Tropical Storm (SSHWS) | |
 | |
| Duration | January 11 – January 15 |
| Peak intensity | 60 mph (95 km/h) (1-min) 994 mbar (hPa) |
A tropical depression formed south-southeast of Sotoray on January 11. Travelling west-northwestward, the depression slowly intensified and became Tropical Storm Pyreum at 06:00 UTC the next day. Influenced by a subtropical ridge to the north of Sotoray, Pyreum's forward movement speed slowed as the system reached peak intensity. At 18:00 UTC, Pyreum made landfall near Blue Inlet, Sotoray with winds of 60 mph. Pyreum weakened over land, dropping to tropical depression status on January 13 at 04:00 UTC. Pyreum then turned due west and pulled away from Sotoray. Entering the warm waters of the Fragmentia Sea, Pyreum restrengthened to tropical storm intensity at 18:00 UTC. As it passed just north of Land's End Point, Vaerhubo at 00:00 UTC the next day, Pyreum reached its secondary peak intensity with winds of 45 mph and a minimum central pressure of 998 mbar. Soon thereafter, influenced by a pressure boundary located south of Sasastalu, Pyreum began displaying subtropical characteristics and initiated a wide loop. Weakening to a subtropical depression late on January 14, Pyreum transitioned into an extratropical cyclone the next day while located north of Vaerhubo. The extratropical remnants of Pyreum completed the cyclonic loop on January 16 and dissipated thereafter.
Pyreum's slow movement coupled with preexisting thunderstorms over Sotoray led to heavy flooding in the country. Several rivers overflowed and flash flooding inundated many structures in the town of Crawfish Creek. At least 10 fatalities and $600 million (2024 USD) in economic losses were attributed to Pyreum.
Hurricane Qizaf[]
| Type 4 Tropical System (TTSS) | |
|---|---|
| Category 4 major hurricane (SSHWS) | |
 | |
| Duration | January 14 – January 20 |
| Peak intensity | 140 mph (220 km/h) (1-min) 931 mbar (hPa) |
The TTSC noted that a tropical depression had developed from a broad area of low pressure early on January 14 while located far southeast of Sotoray. Turning to the northwest, the system gradually became better organized and intensified into Tropical Storm Qizaf at 16:00 UTC that day. Due to modest wind shear, warm sea surface temperatures, and abundant moisture, Qizaf steadily intensified thereafter, becoming a hurricane at 06:00 UTC the next day. Still moving northwestward, Qizaf strengthened into a major hurricane by 22:00 UTC, though by then the TTSC noted that increasing wind shear was affecting the system, leading to a reduced rate of intensification. At 19:00 UTC on January 16, Qizaf reached peak intensity as a powerful Category 4 hurricane while located far south of Sotoray. A developing high-pressure ridge pushed Qizaf into a more westerly trajectory as it maintained peak intensity through the early hours of January 17. By 05:00 UTC, however, atmospheric conditions started to deteriorate, with dry air beginning to erode Qizaf's core. Additionally, the hurricane began an Eyewall Replacement Cycle, developing concentric eyewalls a few hours later. Weakening below major hurricane intensity by 00:00 UTC on January 18, Qizaf began a wide northward curve that brought it into even less favourable conditions. Qizaf weakened to a tropical storm at 20:00 UTC the same day, then turned due north and headed directly towards Malrom Island. 16 hours later, the storm weakened to a tropical depression as its convection collapsed. At 20:00 UTC on January 19, Qizaf made landfall near Glasgow Beach, Malrom Island, quickly transitioning into a remnant low by 10:00 UTC the next day.
Hurricane Reltiu[]
| Type 3 Tropical System (TTSS) | |
|---|---|
| Category 3 major hurricane (SSHWS) | |
 | |
| Duration | January 20 – January 28 |
| Peak intensity | 120 mph (195 km/h) (1-min) 953 mbar (hPa) |
Tropical Depression 20[]
| Type 1 Tropical System (TTSS) | |
|---|---|
| Tropical Depression (SSHWS) | |
 | |
| Duration | January 26 – January 27 |
| Peak intensity | 35 mph (55 km/h) (1-min) 1011 mbar (hPa) |
Subtropical Storm Sisomi[]
| Type 1 Tropical System (TTSS) | |
|---|---|
| Subtropical Storm (SSHWS) | |
 | |
| Duration | February 1 – February 3 |
| Peak intensity | 45 mph (75 km/h) (1-min) 1008 mbar (hPa) |
Hurricane Tythir[]
| Type 2 Tropical System (TTSS) | |
|---|---|
| Category 1 hurricane (SSHWS) | |
 | |
| Duration | February 1 – February 12 |
| Peak intensity | 75 mph (120 km/h) (1-min) 974 mbar (hPa) |
Hurricane Umiga[]
| Type 2 Tropical System (TTSS) | |
|---|---|
| Category 1 hurricane (SSHWS) | |
 | |
| Duration | February 3 – February 10 |
| Peak intensity | 90 mph (150 km/h) (1-min) 971 mbar (hPa) |
Tropical Storm Vilien[]
| Type 1 Tropical System (TTSS) | |
|---|---|
| Tropical Storm (SSHWS) | |
 | |
| Duration | February 16 – February 21 |
| Peak intensity | 60 mph (95 km/h) (1-min) 990 mbar (hPa) |
Tropical Depression 25[]
| Type 1 Tropical System (TTSS) | |
|---|---|
| Tropical Depression (SSHWS) | |
 | |
| Duration | February 19 – February 20 |
| Peak intensity | 35 mph (55 km/h) (1-min) 1008 mbar (hPa) |
Subtropical Storm Wukasti[]
| Type 1 Tropical System (TTSS) | |
|---|---|
| Subtropical Storm (SSHWS) | |
 | |
| Duration | February 25 – February 26 |
| Peak intensity | 45 mph (75 km/h) (1-min) 1006 mbar (hPa) |
Hurricane Xalu[]
| Type 5 Tropical System (TTSS) | |
|---|---|
| Category 5 major hurricane (SSHWS) | |
 | |
| Duration | February 28 – March 21 |
| Peak intensity | 185 mph (295 km/h) (1-min) 894 mbar (hPa) |
Hurricane Yenalt[]
| Type 2 Tropical System (TTSS) | |
|---|---|
| Category1 hurricane (SSHWS) | |
| Duration | March 4 – March 9 |
| Peak intensity | 85 mph (140 km/h) (1-min) 982 mbar (hPa) |
Tropical Storm Zourin[]
| Type 1 Tropical System (TTSS) | |
|---|---|
| Tropical Storm (SSHWS) | |
| Duration | March 6 – March 12 |
| Peak intensity | 70 mph (110 km/h) (1-min) 993 mbar (hPa) |
Hurricane Axaly[]
Type 3 Tropical System (TTSS) Category 4 major hurricane (SSHWS) Duration March 7 – March 14 Peak intensity 130 mph (215 km/h) (1-min)
954 mbar (hPa)
Hurricane Bula[]
| Type 2 Tropical System (TTSS) | |
|---|---|
| Category 1 hurricane (SSHWS) | |
| Duration | March 19 – March 26 |
| Peak intensity | 80 mph (130 km/h) (1-min) 982 mbar (hPa) |
Hurricane Carindor[]
| Type 5 Tropical System (TTSS) | |
|---|---|
| Category 5 major hurricane (SSHWS) | |
| Duration | March 24 – March 30 |
| Peak intensity | 160 mph (265 km/h) (1-min) 924 mbar (hPa) |
Hurricane Dresita[]
| Type 1 Tropical System (TTSS) | |
|---|---|
| Category 1 hurricane (SSHWS) | |
| Duration | April 8 – April 11 |
| Peak intensity | 75 mph (120 km/h) (1-min) 991 mbar (hPa) |
Hurricane Ezanti[]
| Type 2 Tropical System (TTSS) | |
|---|---|
| Category 1 hurricane (SSHWS) | |
| Duration | April 15 – April 26 |
| Peak intensity | 75 mph (120 km/h) (1-min) 988 mbar (hPa) |
Tropical Storm Fromidar[]
| Type 1 Tropical System (TTSS) | |
|---|---|
| Tropical Storm (SSHWS) | |
| Duration | April 28 – May 3 |
| Peak intensity | 60 mph (90 km/h) (1-min) 994 mbar (hPa) |
Storm names[]
In this basin, storms are given a name if they are determined to have 1-minute sustained winds of at least 40 mph (65 km/h). As opposed to previous seasons where names are retired during the post-season analysis, the TTSC has announced that, starting this season, it will retire the names of especially destructive or deadly storms as soon as they are deemed eligible for retirement. Replacement names will be announced alongside retired ones. The naming list used this season was the same list that was used during the 2018-19 season, as no names were retired that season. Names not retired this season will next appear in the naming list for the 2030-31 season.
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Auxiliary naming list[]
In case the original naming list is exhausted, the TTSC begins naming storms using an auxiliary naming list. There's only a single auxiliary naming list, so the same list gets used whenever it is necessary. The name Carindor was used for the first time this season after replacing the name Cromsen, which was retired after the 2015-16 season.
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Retirements[]
The TTSC announced the retirement of 8 names this season; Calron, Flaas, Hoama, Mamasha, Reltiu, Vilien, Axaly, and Ezanti due to the amount of damage and deaths they caused, and as such those names will never be used to name Roambatoanian tropical cyclones again. They were replaced with Criasu, Fopaii, Hobisan, Mimboral, Rubana, Vevinar, Ayari, and Erifer, respectively. All replacement names will first appear on the 2030-31 naming list with the exception of the latter two, due to there only being a single auxiliary naming list. With 8 names retired, this season is tied with 2000-01 for the most names retired in a single season.
Season effects[]
| Storm name |
Dates active | Storm category at peak intensity |
Max 1-min wind mph (km/h) |
Min. press. (mbar) |
Areas affected | Damage (USD) |
Deaths | |||
|---|---|---|---|---|---|---|---|---|---|---|
| Avatama | October 20 - 26 | Category 1 hurricane | 75 (120) | 989 | Malrom Island, Simabo, Brimphola | $1.05 billion | 26 (3) | |||
| Buar | October 24 - 28 | Tropical storm | 40 (65) | 1005 | None | None | None | |||
| Calron | October 27 - November 4 | Category 5 hurricane | 160 (260) | 918 | Vaerhubo, Sotoray, Malrom Island, Sasastalu | ≥$192.17 billion | 4,603+ | |||
| Delain | November 1 - 4 | Tropical storm | 40 (65) | 999 | Oorvelm, Sembung, Wazgol, Sireyalo Islands, Teelmondo | Minimal | None | |||
| Eleni | November 7 - 15 | Category 1 hurricane | 80 (130) | 978 | Brimphola, Simabo, Malrom Island, Nobora, Sasastalu, Cleelai | $25 million | None | |||
| Flaas | November 13 - 27 | Category 5 hurricane | 185 (295) | 901 | Vaerhubo, Oorvelm, Sembung, Wazgol, Sireyalo Islands, Teelmondo, Simabo, Brimphola, Nobora | ≥$3.02 billion | 137 | |||
| 07 | November 14 - 18 | Tropical storm | 40 (65) | 1008 | None | None | None | |||
| Geu | November 22 - 25 | Tropical storm | 45 (75) | 1001 | Vaerhubo, Malrom Island, Sasastalu, Cleelai | $55 million | 4 | |||
| Hoama | November 25 - December 3 | Category 5 hurricane | 180 (285) | 899 | Malrom Island, Sasastalu, Cleelai | ≥$76 billion | 857-2,589+ | |||
| Ivindi | December 6 - 13 | Tropical storm | 70 (110) | 983 | Malrom Island | None | None | |||
| Jokalom | December 12 - 18 | Category 4 hurricane | 145 (230) | 940 | None | None | None | |||
| Karisto | December 17 - 20 | Category 2 hurricane | 100 (155) | 972 | None | None | None | |||
| Lilio | December 17 - 23 | Category 3 hurricane | 115 (185) | 960 | Oorvelm, Sembung, Wazgol | $235 million | 7 | |||
| Mamasha | December 27, 2024 - January 1, 2025 | Category 4 hurricane | 140 (220) | 944 | Sotoray, Vaerhubo, Malrom Island | $6.93 billion | 46 | |||
| Ninoom | December 30 - 31 | Tropical storm | 50 (85) | 1009 | Malrom Island | $100 million | 2 | |||
| Opasko | January 2 - 6 | Category 3 hurricane | 115 (185) | 961 | None | None | None | |||
| Pyreum | January 11 - 15 | Tropical storm | 60 (95) | 994 | Sotoray, Vaerhubo | $600 million | 10 | |||
| Qizaf | January 14 - 20 | Category 4 hurricane | 140 (220) | 931 | Malrom Island | Minimal | None | |||
| Reltiu | January 20 - 28 | Category 3 hurricane | 120 (195) | 953 | Vaerhubo, Malrom Island, Brimphola, Simabo, Nobora | $27.6 billion | 19 | |||
| 20 | January 26 - 27 | Tropical depression | 35 (55) | 1011 | Vaerhubo | ≥$95 million | 12 | |||
| Sisomi | February 1 - 3 | Subtropical storm | 45 (75) | 1008 | Cleelai | None | None | |||
| Tythir | February 1 - 12 | Category 1 hurricane | 75 (120) | 974 | Oorvelm, Sembung, Wazgol, Sireyalo Islands, Teelmondo | Minimal | 1 | |||
| Umiga | February 3 - 10 | Category 1 hurricane | 90 (150) | 971 | None | None | None | |||
| Vilien | February 16 - 21 | Tropical storm | 60 (95) | 990 | Oorvelm, Sembung | ≥$4.75 billion | 90 | |||
| 25 | February 19 - 20 | Tropical depression | 35 (55) | 1008 | None | None | None | |||
| Wukasti | February 25 - 26 | Subtropical storm | 45 (75) | 1006 | Nobora | $12 million | 5 | |||
| Xalu | February 28 - March 21 | Category 5 hurricane | 185 (295) | 894 | Brimphola, Simabo | ≥$59 million | None | |||
| Yenalt | March 4 - 9 | Category 1 hurricane | 85 (140) | 982 | None | None | None | |||
| Zourin | March 6 - 12 | Tropical storm | 70 (110) | 993 | None | None | None | |||
| Axaly | March 7 - 14 | Category 4 hurricane | 130 (215) | 954 | Sireyalo Islands, Teelmondo, Simabo | ≥$52 billion | 23 | |||
| Bula | March 19 - 26 | Category 1 hurricane | 80 (130) | 982 | Brimphola, Simabo | Minimal | None | |||
| Carindor | March 24 - 30 | Category 5 hurricane | 160 (260) | 924 | Vaerhubo, Malrom Island, Simabo, Nobora | ~$10 million | 6 | |||
| Dresita | April 8 - 11 | Category 1 hurricane | 75 (120) | 991 | None | None | None | |||
| Ezanti | April 15 - 26 | Category 1 hurricane | 75 (120) | 988 | Vaerhubo, Malrom Island | $5.16 billion | 402 | |||
| Fromidar | April 28 - May 3 | Tropical storm | 60 (95) | 994 | Nobora, Sasastalu, Cleelai | ~$2 billion | 15 | |||
| Season aggregates | ||||||||||
| 35 systems | October 20, 2024 - May 3, 2025 | 185 (295) | 894 | >$371.13 billion | 6,265-7,997+ (3) | |||||
Notes[]
References[]
- ↑ Fool, Blustering (November 18, 2024). Teelmondo Tropical Surveillance System Broadcast 102 ADVISORY 12 FOR HURRICANE FLAAS. Teelmondo Tropical Surveillance System. Hypothetical Hurricanes Wiki. Retrieved on November 18, 2024.
- ↑ Fool, Blustering (November 18, 2024). Teelmondo Tropical Surveillance System Broadcast 105 ADVISORY 13 FOR HURRICANE FLAAS. Teelmondo Tropical Surveillance System. Hypothetical Hurricanes Wiki. Retrieved on November 18, 2024.
- ↑ Fool, Blustering (November 20, 2024). Teelmondo Tropical Surveillance System Broadcast 112 ADVISORY 16 FOR HURRICANE FLAAS. Teelmondo Tropical Surveillance System. Hypothetical Hurricanes Wiki. Retrieved on November 20, 2024.
- ↑ Fool, Blustering (November 18, 2024). Teelmondo Tropical Surveillance System Broadcast 103 FINAL ADVISORY FOR TROPICAL DEPRESSION 07. Teelmondo Tropical Surveillance System. Hypothetical Hurricanes Wiki. Retrieved on November 18, 2024.