This is the imagery archive for all satellite or surface analysis or radar images for Danulean storms that are currently available.
The peak intensity of relatively disorganized Hurricane Anguilla, late on June 24th, while it was passing in between Nikorru and Odileland.
Weak and disheveled Subtropical Depression Two at peak intensity, in the Darafura Sea, late on June 28th.
Tropical Storm Barthelemy making landfall in Banglamore at peak intensity with orderly cloud banding, very early on June 29th.
Resembling a blob of convection, Caroline makes landfall in the southern United States of Danula as a strong tropical storm, very early on July 4th.
Well developed Major Hurricane Daniel at peak intensity as a 115 mile per hour category 3 hurricane with a remarkably clear eye, north of the Turkland coastline, late on July 7th.
Disorganized Tropical Depression Ninety Seven, operationally Invest Ninety Seven, at peak intensity, just as it made landfall in Nikorru early on July 9th.
Hurricane Emilia at peak intensity showing its shallow eye, passing just south of Nikorru, early on July 18th.
Frederic at peak intensity as a high end category 2 hurricane with a well pronounced eye, while passing through the waters of Odileland, late on July 19th.
Visually unremarkable Severe Tropical Storm Gertrude at peak intensity, while making landfall along the southern coastline of the United States of Danula, early on July 24th.
Disorderly but damaging Harvey at peak intensity, as a severe tropical storm making landfall near Floodston City with heavy rainfall, causing catastrophic flooding in the area, late on July 27th.
Strengthening and well organized Severe Tropical Storm Irene, making landfall in Banglamore at peak intensity, late on August 1st.
Intense and organized Hurricane Jose at its category 6 peak strength with a well defined eye, north of the Waleston coastline, late on August 5th.
Extremely powerful Hurricane Katherine at its category 7, 180 mile per hour, peak intensity in the Damarian Sea with very good banding and eye structure, threatening Odileland's coastlines, late on August 11th.
Another image of Katherine, at the same time, but composited from radar data instead, taken from recon aircraft, maritime and surface radar, and satellite rainfall observations.
Somewhat orderly Severe Subtropical Storm Lenny at peak intensity in the middle of the Damala Ocean with 65 mile per hour winds, late on August 16th.
Heavily sheared Subtropical Storm Margharet at peak intensity with a partially exposed circulation, in the southwestern Darafura Sea, late on August 9th.
Powerful Hurricane Nathan at peak intensity in the middle of the Damala Ocean, showing a well developed pinhole eye, as a 130 mile per hour category 4 hurricane, late on August 22nd.
In this image taken late on August 27th, powerful hurricanes Opal and Philippe are reaching their peak intensities of 170 miles per hour and 180 miles per hour respectively, as the two category 7 hurricanes have a Fujiwhara interaction of minimal impact.
Category 7 hurricane Opal reaches its 170 mile per hour peak intensity, with a well organized center and eye, as it continues moving east through the empty ocean, late on August 27th.
Strong hurricane Philippe attains its 180 mile per hour peak strength, well organized and in favorable conditions, while threatening parts of Odileland and Turkland, late on August 27th.
Extratropical-like hurricane Rita at its peak intensity as a tropical cyclone, very early on September 2nd, with a structure showing signs of deterioration, as it was threatening the country of Germania.
Major hurricane Stan at its secondary peak strength, as a category 5 hurricane with 145 mile per hour winds, while it was threatening the St. Kitts and Nevis islands, as well as Waleston, late on September 10th.
Hurricane Tammy at its category 3, 110 mile per hour peak intensity, as it moved east-northeast in the open Damala Ocean, late on September 12th, presenting an overall well organized structure.
Small scale hurricane Vince at its peak intensity, as it made landfall in Banglamore with 75 mile per hour winds, late on September 15th.
The tertiary (and most powerful), and (at the time) record breaking peak intensity of hurricane Stan, with extremely good organization including a pinhole eye and powerful banding, as it slowly moved through the Gulf of Floodston, threatening the city itself, late on September 16th.
Hurricane Whitney reaching its peak intensity as a minimal category 3 hurricane in the open ocean, early on September 19th, showing a relative lack of a strong center.
Well-organized hurricane Acorn at its peak strength, as a 130 mile per hour category 4 hurricane in the middle of the Damala Ocean, moving east and threatening the United States of Danula in the long run, pictured late on September 25th.
The first of several peaks of hurricane Barry, this specific peak attaining 90 mile per hour sustained windspeeds as a disorganized category 2 hurricane in the Damala Ocean, late on September 25th.
Extremely strong and well organized hurricane Chandra at its 195 mile per hour peak strength, marking the end of a period of rapid strengthening, just as it made landfall along the shores of Turkland, early on October 1st.
Hurricane Barry at another of its peak intensities, this time as a 100 mile per hour major hurricane, still in the middle of the Damala Ocean, pictured on October 2nd.
Small but powerful hurricane Douglas at its category 3, 100 mile per hour peak intensity, displaying a lack of any visible eye feature despite its strength, just as it made landfall in the southern United States of Danula, early on October 5th.
Tropical Storm Evelyn displaying a sheared appearance with half of its low level circulation being exposed, at its short lived 40 mile per hour peak intensity in the Darafura Sea, late on October 13th.
An image taken late on October 18th, encompassing a large part of the Danulean basin, showing two category 6 hurricanes, (left to right) Fabio and Barry, at their peak intensities, both reaching 160 miles per hour, displaying their large size difference as well as their proximity to land.
Large and well organized hurricane Barry at the strongest of its peak intensities, as a 160 mile per hour category 6 hurricane moving east through the Damala Ocean and approaching its eventual landfall in the United States of Danula, late on October 18th.
Relatively small, yet relatively strong Fabio making landfall in Banglamore at its peak intensity as a 160 mile per hour category 6 hurricane with a prominent yet small eye and well organized banding and outflow, imaged late on October 18th.
Barry just hours before its devastating 150 mile per hour landfall along the United States of Danula coastline, displaying a well organized eye and signs of a potential eyewall replacement cycle, imaged late on October 20th.
Weak and disheveled Tropical storm Gloria at its controversial peak strength, late on November 1st, as it barely remained a tropical cyclone while approaching the country of Germania.
Well organized and intense hurricane Harmony as a category 5 cyclone with winds reaching 140 miles per hour, imaged late on November 9th, as it was threatening the northwestern United States of Danula coastline.
Tropical storm Isa at its peak intensity as a high end tropical storm in the middle of the Damala Ocean, showing moderate outflow and some impacts from shear, late on November 11th.
Strong and well organized hurricane Jazlyn as a category 6 hurricane late on November 29th, presenting a severe threat to the Andreaston metropolitan area of the United States of Danula.
A day later, Jazlyn, even stronger, now threatens to make landfall along the United States of Danula coast as a hurricane with winds exceeding 190 miles per hour, making it a possible category 8 landfalling hurricane if forecasts verify.
Jazlyn makes landfall as a 195 mile per hour category 8 major hurricane on late December 1st, inflicting devastating damages on the Andreaston metropolitan area and becoming the strongest and most intense landfalling December hurricane in the basin.
An experimental color image of Jazlyn captured at the same time as the previous image, using the prototype version of the geostationary GDOS - 2 imager flown on a low Danulean orbit satellite.
Category 3 hurricane Korra as imaged late on December 11th, just as it was reaching its peak intensity in the middle of the open ocean, displaying a rather well organized central dense overcast, good outflow, and a short lived pinhole eye.
An image taken by the GDOS - 1 satellite late on December 27th, showing weak hurricanes Layten and Michael in an extremely close Fujiwhara interaction, with their convection centers nearly merging together, and the two hurricanes almost appearing as one unusual storm.
Major hurricane Michael making landfall near Andreaston at peak intensity, early on December 29th, with a notable lack of any conventional features indicating major hurricane strength.
An image of hurricane Layten, at category 6 peak intensity with windspeeds reaching 150 miles per hour late on December 30th, showing a pinhole eye, good outflow, and overall good structure.
Hurricane Layten making landfall along the Iseland shoreline with winds reaching 110 miles per hour late on January 2nd, and a large, disorganized, and shallow eye.
Severe tropical storm Nacho at its peak intensity late on January 22nd with 60 mile per hour winds, displaying no interesting features structure and appearance wise.
Hurricane Olivia at its first peak intensity with winds reaching 80 miles per hour late on February 3rd, and its large size showing its subtropical origins, as it threatened to cause significant damages in the Banglamore region.
Olivia at its second and highest peak intensity late on February 8th, this time as a category 3 major hurricane with winds reaching 100 miles per hour, as it accelerated towards the Nikorru island.
Hurricane Pauline around midday on March 1st, showing its impressive appearance prior to its intial peak intensity, which occurred 6 hours later.
Category 6 hurricane Pauline at its initial peak strength, late on March 1st, showing a well organized structure as it was threatening the St. Kitts and Nevis islands, just prior to weakening due to an eyewall replacement cycle.
Pauline at its second and highest peak intensity, late on March 3rd, as a 160 mile per hour category 6 hurricane with a pressure of 907 mbar, becoming the record most intense storm in the basin in March, while making landfall in the northern islands of Waleston.
Major hurricane Rebecca showing its extratropical origins with disorganized convection, and overall a non-tropical appearance at its peak intensity, late on March 31st, a day before it fully completed its transition into an extratropical cyclone.
Well organized hurricane Sienna at its peak intensity late on April 25th, with winds reaching 140 miles per hour, as it makes landfall along the coastline of Turkland with destructive impacts in the area.
160 mile per hour, category 6 major hurricane Troy at its peak intensity late on April 26th, showing a well organized central dense overcast, strong outflow, and a prominent eye, as it slowly travels through the open Damala Ocean.
Weak and small tropical storm Vixen at its peak intensity, late on May 16th, showing the impacts of shear on its convection and structure.
Extremely intense and powerful hurricane Winnie at its short lived peak intensity, late on May 17th, with winds reaching 190 miles per hour, and the pressure dropping to 877 mbar, after 24 hours of some of the fastest tropical cyclone strengthening ever recorded.
Invest 90D, just two days after the season began, on June 2nd, several days before it eventually developed into Anthony, presenting a generally disorganized structure.
Hurricane Anthony at peak intensity, early on June 12th, just as it made landfall in the southwestern United States of Danula.
Anthony at around the same time, but in enhanced infrared imagery, showing its rather disheveled structure.
Belinda at peak intensity early on June 28th, as a weak and disheveled tropical storm.
Invest 92D on July 6th, presenting some potential for tropical cyclone genesis, but overall unlikely to reach tropical cyclone status.
Invest 92D on July 7th, at its closest to being a tropical cyclone, but still showing clear signs of a lack of proper tropical cyclogenesis.
Powerful Chris at peak intensity late on July 15th, as the first major hurricane of the season.
Tropical Depression Four, just as it was designated, late on July 31st.
Invest 94D, barely hours before being named Delilah, late on July 31st.
Tropical Depression Four at peak intensity, on August 1st, just hours before degenerating into a remnant low.
Strong Delilah at peak intensity, late on August 3rd, as a category 5 hurricane on the Lucarius Wind Scale.
Disintegrating Delilah a few days after peak intensity, late on August 6th, barely holding on to hurricane status.
Severe Tropical Storm Delilah, prior to restrengthening back to hurricane status, late on August 7th.
Completely reorganized, Delilah is now a hurricane again, late on August 8th.
Delilah quickly approaching landfall late on August 9th, with an unusually rapid motion that caused some shear on the system on its own.
Delilah making its destructive landfall near Floodston City, on August 10th, with 80 mph winds and incredible rainfall.
Disorganized Erick at 'peak' intensity, late on August 14th, after having maintained minimal tropical storm strength for a day.
Newly named Tropical Storm Fern, late on August 25th, already displaying well organized banding.
Fern, now a hurricane, displaying a developing eyewall late on August 26th.
Compact Major Hurricane Fern, with a well visible eye, as it menacingly bore down on the nearby coastline, late on August 27th.
Minimal Tropical Storm Gabe just after getting named, late on August 27th.
Fern, ever stronger and more organized, late on August 28th, just as it was approaching landfall.
Severe Tropical Storm Gabe at peak intensity, despite its worse visual appearance than when it was named, late on August 28th.
Fern making its catastrophic landfall on August 29th, with 160 mph winds and a pressure of 913 mbar, making it a category 6 hurricane on the Lucarius Wind Scale.
Tiny Invest 98D, which eventually failed to attain tropical cyclone status despite getting high chances of tropical cyclogenesis, late on September 8th.
Pre-Helena late on September 12th, showing some general clustering of convection around a low pressure in the monsoonal trough.
Potential Tropical Cyclone Nine late on September 13th, just a day before strengthening into Subtropical Storm Helena, showing signs of a surface circulation.
Subtropical Storm Helena late on September 14th as a marginal subtropical storm, showing a very disorganized core, and somewhat questionable structure, leading to debates over its subtropical status at that point.
Subtropical Storm Helena, hours before becoming a true tropical cyclone, at its initial peak strength as a 50 mph storm, late on September 15th.
Helena, slightly weaker, and now a true tropical cyclone, late on September 16th, as it struggled to reintensify for the next couple of days.
Helena at its secondary peak intensity, as a 50 mph tropical storm, late on September 18th, just 6 hours before landfall in Turkland.
Weak and non-tropical looking subtropical storm Isla late on September 18th, at its 50 mph peak intensity.
Relatively badly organized Hurricane James, with recon-confirmed 70 mph winds inside its center, late on September 18th.
James, now a major hurricane, still struggling to maintain a satellite presentation worthy of its recon-verified windspeed, late on September 19th.
James on September 20th as a 145 mph category 5 hurricane, showing a notable lack of a visible, clear eye.
150 mph James, recently upgraded to category 6 strength, finally manages to present a satellite visual worthy of its intensity, as an eye rapidly forms within the hurricane, and it enters a burst of rapid strengthening, late on September 20th.
James, now a catastrophic hurricane with winds reaching 195 mph, just as it directly hit one of the outlying islands of the United States of Danula, late on September 21st.
James at its record peak intensity, with winds reaching 215 mph, and the pressure dropping to an astonishing 870 mbar, late on September 22nd, just as it scorched several other outlying islands of the United States of Danula.
Animated imagery of James at around the same time, showing its well organized structure, and slow movement speed. The animation spans 2 hours, from 18Z to 20Z September 22nd.
James at around the same time, but in Dvorak enhanced infrared imagery, showing its cold cloud tops and warm eye.
James, now rapidly weakening due to upwelling and deteriorating conditions, as a strong category 5 major hurricane with winds reaching 145 mph late on September 23rd.
James, continuing its weakening trend, now nearly a minimal category 3 hurricane with winds reaching 105 mph, late on September 24th.
James, just barely holding on to hurricane status in highly hostile conditions, late on September 25th.
Now only a weak and collapsing tropical storm, James nears degeneration into a remnant low, late on September 26th.
Potential Tropical Cyclone Twelve late on October 15th, just a day before it developed into Tropical Storm Kelly, showing clear signs of tropical transition.
Tropical Storm Kelly just as it was designated, late on October 16th, clearly showing its extratropical roots.
Kelly, now a hurricane, showing its unusual structure, late on October 17th, as preparations and precautions were taken in southern Waleston.
Now a category 2 hurricane, with windspeeds reaching 90 mph, Kelly begins its two day long battering of the country of Waleston, as it begins a transition to extratropical status, late on October 18th.
Kelly at its peak intensity while a tropical cyclone, with winds reaching 95 mph, just 6 hours before it transitioned into an extratropical cyclone and made landfall in Waleston, early on October 19th.
Kelly, in an unusual manner, reaches major hurricane force winds as an extratropical cyclone, late on October 19th, just after it came ashore.
Tiny Lauren already as an 80 mph hurricane, late on December 2nd, just 12 hours after being designated as a tropical cyclone.
Lauren at peak intensity, as a 90 mph hurricane with a pressure of 983 mbar, late on December 3rd, only a day before degenerating back into an extratropical cyclone.
Tropical Depression One at peak intensity just after formation, late on June 11th, as a weak and short lived tropical depression with winds of 35 mph and a pressure of 1008 mbar.
Tropical Depression Two just after formation, late on July 8th, as a disorganized tropical cyclone positioned in an unfavorable environment.
Tropical Depression Two at peak intensity, late on July 9th, as a tropical depression barely qualifying for tropical cyclone status with winds of 35 mph and a pressure of 1007 mbar.
Tropical Depression Two during its weakening phase caused by unfavorable conditions, late on July 10th, despite its better appearance on satellite imagery.
Tropical Depression Three a few hours after formation, late on July 20th, with a relatively organized structure for a cyclone of monsoonal nature.
Tropical Depression Three as a well organized tropical depression late on July 21st, showing significant structural improvement over 24 hours.
Tropical Storm Anguilla just after formation late on July 21st, presenting a well organized structure for a 40 mph tropical storm, with a tight core and central convection.
Tropical Storm Barthelemy after suffering a significant structural degradation late on July 22nd, now lacking organized convection and a well defined center, and more closely resembling a monsoonal depression.
Anguilla after strengthening into the first hurricane of the season late on July 22nd, with a central dense overcast, good banding structure, and a developing eyewall.
Barthelemy after some strengthening late on July 23rd, presenting more convection and better structure as it reaches its peak intensity as a 45 mph tropical storm with a pressure of 996 mbar.
Major Hurricane Anguilla after rapidly strengthening to its peak intensity of 150 mph and 926 mbar late on July 23rd, presenting a semi-clear eye, an intense central dense overcast, and good outflow.
Tropical Storm Barthelemy after weakening a little late on July 24th, still presenting a generally well organized structure, with only a small increase in pressure signifiying weakening.
Anguilla after weakening down to a strength of 130 mph late on July 24th, having undergone severe structural degradation since its peak intensity, despite remaining strong.
Barthelemy after suffering from significant structural degradation late on July 25th, showing a collapse of convection and structure, and weakening from 45 mph to 40 mph over the last 24 hours.
Anguilla after weakening further to 110 mph late on July 25th, despite a better satellite imagery appearance than 24 hours prior, with a clear eye and eyewall.
Hurricane Anguilla 12 hours after weakening below major hurricane status late on July 26th, having increased in size while its structure waned.
Hurricane Anguilla as a minimal hurricane with winds of 70 mph late on July 27th, with an even weaker structure and asymmetric convection.
Tropical Storm Caroline as a minimal 40 mph tropical storm late on July 30th, with a decent structure and good convection, as it threatened the country of Iseland and the State of Floodston with the possibility of a major hurricane force landfall.
Severe Tropical Storm Caroline as a strengthening 60 mph severe tropical storm late on July 31st, with a small and continuously improving core, as its threat of a major hurricane force landfall increased, and land areas began final preparations for a destructive landfall.
Hurricane Caroline as a strengthening 80 mph hurricane north of Iseland late on August 1st, with a small core and an emerging pinhole eye, as it came ever closer to landfall.
Hurricane Caroline at its peak intensity as a major hurricane with winds of 145 mph late on August 2nd, with a well defined structure and an obvious, well defined pinhole eye, as it was just hours away from landfall in the State of Floodston.
Tropical Depression Six late on August 2nd, just after formation, displaying a somewhat well organized structure, and deep convection over its circulation, while in conditions favorable for strengthening.
Caroline as a weakening major hurricane late on August 3rd, with a severely degraded structure due to land interaction and unfavorable conditions, including a collapsed eye, as it moved further and further away from land.
Tropical Storm Dawson late on August 3rd, just after reaching tropical storm status, displaying impressive banding, and yet more convection over its circulation, while in conditions still favorable for significant strengthening.
Hurricane Caroline as a weakening Category 2 hurricane late on August 4th, with winds reaching up to 85 mph, showing some improvements in structure, however, recon flights confirmed that it continued steadily weakening after its peak intensity.
Tropical Storm Dawson late on August 4th with 50 mph winds, after some strengthening during the previous 24 hours, displaying a developing core, while it neared hurricane strength.
Severe Tropical Storm Caroline as a weakening storm late on August 5th, showing signs of rapid extratropical transition, while moving into cooler waters and a less favorable environment.
Hurricane Dawson late on August 5th as a 70 mph Category 1 hurricane, displaying a developing eye, and a well organized core and structure, while it continued its strengthening trend.
Hurricane Dawson late on August 6th, just as it was upgraded to a 100 mph major hurricane, now with a relatively large and well formed eye, deep convection all around its center, and a large northern band.
Hurricane Dawson at its peak intensity early on August 7th, as a 110 mph Category 3 hurricane with a pressure of 958 mbar, displaying a CDO with a prominent eye at its center, while it began encountering increasingly unfavorable conditions.
Disorganized Dawson late on August 7th, as a minimal 100 mph major hurricane, while it was in its weakening phase, showing a completely collapsed structure and disorganized convection, with its strong northern band now almost completely missing.
Small Dawson late on August 8th, as a weakening 80 mph hurricane, despite showing improvement in its structure due to it becoming more compact, as it headed into more unfavorable conditions.
Weak and disorganized Severe Tropical Storm Dawson late on August 9th, with winds reaching 60 mph, presenting an extratropical looking structure, just days from its eventual dissipation in colder waters.
Strong Tropical Storm Emilia late on August 21st, with winds reaching as high 50 mph, showing a well developed structure for strengthening, as it brought rainfall to the country of Nihon, and threatened to bring hurricane force winds and severe rainfall to eastern Nikorru.
Well organized Hurricane Emilia late on August 22nd, as a 90 mph Category 2 hurricane, displaying a prominent eye feature, with good organization and structure, as it caused the authorities of Nikorru to prepare for a destructive hurricane.
Major Hurricane Emilia at its peak intensity late on August 23rd, with winds reaching up to 130 mph and a pressure of 942 mbar, with a large and well organized eye, a good central dense overcast, and a strong southern band, just before it began weakening and closing in to its landfall.
Weakening Emilia as it made landfall in southeastern Nikorru late on August 25th, with winds reaching 90 mph, and a pressure of 971 mbar, displaying a massive amount of strong convection around its center, and bringing extreme winds and rainfall to southeastern Nikorru.
Well organized Frederic as an 80 mph hurricane late on August 26th, displaying a well developed core and a strong, tightly wrapped band, as it threatened multiple island nations with a potential strong major hurricane landfall.
A disorganized and weak Tropical Storm Emilia as it made landfall in eastern Nikorru late on August 27th, with winds reaching 40 mph, presenting a notable lack of convection around its center, and bringing some more rainfall to eastern Nikorru, as it was mere hours from its dissipation.
Major hurricane Frederic with 130 mph winds late on August 27th as a category 4 hurricane, now showing a developing small eye, and significant structural improvement since yesterday with a large central dense overcast, as warned areas braced for severe, destructive and deadly impacts.
A satellite loop of Frederic strengthening over the 6 hours leading up to its initial landfalls in the outlying parts of St. Kitts and Nevis on August 28th, covering the time period between 09Z and 15Z.
Strengthening Frederic on August 28th, with a large, circularizing and clearing eye, and a powerful, round central dense overcast with an extremely strong eyewall, as it was about to hit some islands with 170 mph winds, and a pressure of 919 mbar.
Annular Frederic with winds reaching 180 mph just 6 hours before its peak intensity, late on August 28th, with a large, circular and clear eye, and a relatively rounded central dense overcast with two strong northern and southern bands, as it battered some outlying islands of St. Kitts and Nevis with its powerful eyewall.
A satellite loop of the 6 hours leading up to Frederic's landfall on the main island of St. Kitts and Nevis early on August 29th as a 185 mph hurricane, covering its peak intensity at 00Z of 185 mph and 907 mbar, up until 0530Z, when it was practically making landfall, after some slight rise in pressure.
Powerful hurricane Frederic 6 hours after its peak intensity of 185 mph and 907 mbar, with winds still reaching 185 mph and a pressure of 909 mbar, early on August 29th, with a well organized and clear eye, and strong, wide reaching outflow, as it made its most powerful landfall on the main island of St. Kitts and Nevis.
Frederic on August 29th, with a powerful but disrupted eye, as it was located over the main island of St. Kitts and Nevis, and weakened due to land interaction, with land observations confirming winds reaching 175 mph, and a pressure reaching 916 mbar.
Category 7 hurricane Frederic with winds of 170 mph, after weakening a little due to its landfall and subsequent crossing of St. Kitts and Nevis, late on August 29th, still showing a clear and round eye, and a relatively large central dense overcast with more wide reaching outflow, as it threatened Waleston with a powerful landfall of a large hurricane.
Hurricane Frederic showing little change in strength and still possessing winds of 170 mph, though beginning to show a consistent weakening trend due to an eyewall replacement cycle, late on August 30th, with an even smaller eye, and slightly reduced cloud cover and influence, as it began its final approach to landfall in Waleston.
Category 6 hurricane Frederic making landfall in Waleston with winds of 150 mph late on August 31st, with a large and ragged eye due to its eyewall replacement cycle, and a greatly expanded influence with massive outflow and a wide central dense overcast and banding, as it brought high storm surge and widespread destruction to the coastline.
Major hurricane Frederic after enduring some significant weakening due to landfall late on September 1st, with a much smaller structure and eye, and undergoing yet more weakening, as it set sights on the northern coastline of Iseland, luckily expected to be much weaker than its previous landfalls.
Minimal hurricane Frederic after weakening some more late on September 2nd, now barely hanging on to hurricane status with its collapsing structure and 70 mph winds, and likely to weaken to severe tropical storm strength within the next 6 hours, as it approached its tropical storm strength landfall on the coastline of Iseland.
Weak tropical storm Gertrude just after reaching tropical storm strength late on September 18th, with 40 mph winds and a somewhat disorganized structure, albeit with decent outflow, as it threatened to make landfall along the northern coastline of Iseland as a severe tropical storm, with hurricane watches taking effect in the same area.
Tropical storm Gertrude after some strengthening late on September 19th, now a 50 mph high end tropical storm with slightly better structure, but significantly impacted by moderate northerly shear, as hurricane watches were dropped in Iseland due to the threat of a near-hurricane strength landfall diminishing.
Strong tropical storm Gertrude still as a high end tropical storm late on September 20th, with 50 mph winds, but a slightly better structure, and a moderately improved core experiencing less shear, as it began its last 24 hours of strengthening until landfall in northwestern Iseland.
Severe tropical storm Gertrude as it made landfall in northwestern Iseland late on September 21st, with 60 mph winds and a pressure of 995 mbar, presenting a large amount of convection, a covered center, and strong winds near the center, while it brought rainfall and gale force winds to the areas it struck.
Tropical Storm Irene just after reaching tropical storm status late on September 30th, with winds of 40 mph and a pressure of 1005 mbar, and a non-notable structure.
Severe Tropical Storm Irene as it neared hurricane status, presenting a somewhat well organized center, a wrapping CDO, and overall a structure that supported further intensification, late on October 1st, with winds of 60 mph and a pressure of 999 mbar.
Hurricane Harris as it somewhat quickly strengthened well out to sea late on October 2nd, presenting a large eye with a rather well organized eyewall structure, as it reached winds of 85 mph and a pressure of 983 mbar.
Hurricane Irene as it rapidly approached major hurricane status late on October 2nd, with 90 mph winds and a pressure of 978 mbar, presenting a developing pinhole eye, extremely good banding, and a small CDO, all features supporting the occurrence of rapid strengthening.
Major hurricane Harris as it quickly strengthened well out to sea late on October 3rd, with a small and clouded eye, a well organized eyewall structure, a rounded CDO, and strong banding, as it reached winds of 105 mph and a pressure of 973 mbar.
Intense Hurricane Irene at its primary peak intensity, late on October 3rd, with a very small eye, extremely good organization, and a low pressure of 901 mbar, with its core packing 175 mph winds, just before it underwent an eyewall replacement cycle.
Major hurricane Harris as it appeared late on October 4th, with a very impressive structure featuring a clear eye, convective bursts in the eyewall, and an enlarged CDO, as it reached winds of 125 mph and a pressure of 951 mbar, with further strengthening ahead.
Major hurricane Irene after significantly weakening down from its peak intensity, late on October 4th, presenting a collapsed and clouded eye, but still possessing a well organized CDO and decent banding, with 115 mph winds and a pressure of 957 mbar.
Major hurricane Harris at its peak intensity late on October 5th, with winds reaching 145 mph and a pressure reaching 939 mbar, and a well organized, but clouded, eye, with a structure that was generally beginning to deteriorate as the system moved into less favorable conditions.
Strong Irene after some restrengthening from the previous day, late on October 5th, with a clearing and rounding eye, and wind speeds reaching 145 mph, with a pressure of 943 mbar.
Hurricane Harris late on October 6th, with a markedly worse structure than the previous day, having been torn apart by motion-induced shear and some cooling sea surface temperatures, but surprisingly still maintaining 135 mph winds and a pressure of 945 mbar.
Category 6 hurricane Irene at its secondary peak intensity, late on October 6th, with 160 mph winds, and a pressure of 931 mbar, presenting a large, clear, and round eye, a strong eyewall, and a widespread CDO with good banding.
Hurricane Irene late on October 7th, as a weakening major hurricane with winds reaching 120 mph and a pressure of 955 mbar, still presenting a distinct and rounded eye, with a fully formed eyewall, and a relatively wide CDO, as it approached landfall on the outlying western islands of St. Kitts and Nevis.
Major hurricane Harris late on October 10th, as it made landfall along the United States of Danula coastline, midway between Andreaston and Hotston, with 105 mph winds and a pressure of 959 mbar, featuring an unusually disheveled structure for a major hurricane.
Severe Tropical Storm Jose late on October 30th, with a very well organized structure, very small wind radii, and winds reaching 60 mph, with a pressure of 1004 mbar, as it approached peak intensity and its landfall in Turkland.
Hurricane Jose late on October 31st, as it made landfall in Turkland at its peak intensity, with winds reaching 80 mph and a pressure of 997 mbar, unusually high for a hurricane of its strength due to its small size, presenting a reasonably well organized core and overall a decent structure.
Subtropical Storm Kasey late on November 10th, showing an unusual structural arrangement with sheared southerly convection, a large gale force wind radius, and winds of 45 mph, with a pressure of 991 mbar.
Severe Tropical Storm Kasey late on November 11th, still presenting an unusual structure with a strong frontal-like band, and strong central convection, with winds reaching 65 mph and a pressure of 985 mbar.
Strong Hurricane Kasey late on November 12th, with a well defined eye and eyewall, and a core that was becoming increasingly separated from the outer reaches of the system, possessing 95 mph winds and a pressure of 953 mbar.
Hurricane Kasey at its peak intensity very early on November 13th, possessing a well defined eye, a strong core, and increasing tropical-only features, as it nearly hit major hurricane strength with winds reaching 95 mph and pressure reaching 951 mbar.
Hurricane Kasey after some weakening late on November 13th, showing a greatly diminished extratropical-like band, and general signs of transition into purely tropical cyclone territory, as the hurricane possessed winds reaching 90 mph and a pressure reaching 957 mbar.
Hurricane Kasey after some more tropical transition late on November 14th, now possessing a moderately large CDO, a partially clear eye, and strong southern banding, as it weakened down to 80 mph and 971 mbar in cooling sea surface temperatures and increasing shear.
Subtropical Storm Lenny early on December 7th, at its peak intensity of 45 mph and 993 mbar well out to sea, showing signs of extratropical transition, only a few hours before its completion and the system's dissipation.
Tropical Storm Margharet late on December 7th, at its peak intensity of 45 mph and 1002 mbar, showing a disorganized, but extremely good for December, tropical cyclone structure, with deep convection over its center, as it slowly meandered east-southeast.
Tropical Storm Nathan late on May 6th, just having gotten its name, as a moderately organized 40 mph tropical storm, approaching the United States of Danula with the threat of a hurricane force landfall in the next couple of days.
Moderately strong Nathan late on May 7th, before undergoing its final strengthening phase, with windspeeds reaching 50 mph and a pressure of 995 mbar, with an improving appearance, as it was 12 hours away from its hurricane force landfall in the United States of Danula.
Hurricane Nathan early on May 8th, at its peak intensity of 70 mph and 989 mbar, showing its best appearance, but still somewhat disorganized for its strength, as it battered the coast of the United States of Danula with its hurricane force winds during landfall.