1990 Azkali cyclone - Revision history

EnigmaticLucas at 04:23, 31 December 2025

2025-12-31T04:23:53Z

← Older revision		Revision as of 04:23, 31 December 2025
Line 4:		Line 4:

	== Meteorological history ==		== Meteorological history ==
	On the 24th of Uni, 1990 (Sunterian time), a tropical wave moved from northern [[Tyrosia]] northeast into the [[Volic Gulf]]. It was monitored by the [[Ari Island Volunteer Meteorological Center]] for several days, but was discontinued from being monitored as it failed to produce atmospheric convection. Over the coming days thereafter, however, the tropical wave slowly organized, and on the 3rd of Agotzo, the wave organized into Tropical Depression 1. Despite the wave's organizing, the AIVMC failed to further monitor the storm until the 10th of Agotzo. [[File:Tropical Cyclone Hudah 2000.jpg\|thumb\|Satellite view of the cyclone at 8:00 AM on the 9th of Agotzo (24th of Snoiguia) as a cyclone, just before it explosively intesified.\|248x248px]]Over the next three days, the tropical depression moved nortwest, entering into a zone with anomalously warm water temperatures and little wind shear. By the 6th of Agotzo, the depression had organized further, and began to be monitored by the [[Sunterian Office of Meteorology\|Sunterian Office of Meteorology (Hedieuž)]] The same day, Hedieuž categorized the depression as a Severe Tropical Storm. At noon on the 7th of Agotzo, hurricane hunters reported the intensification of the cyclone from a Severe Tropical Storm to a Cyclone, with sustained winds of 95 miles per hour, with recorded gusts of up to 110 miles per hour. A mid-level ridge to the north of the cyclone steered it west along an elongated arcing path, into waters with cooler water temperatures. The cyclone stalled and weakened slightly into a Severe Tropical Storm starting at around 10:00 PM on the 7th.		On the 24th of Uni, 1990 (Sunterian time), a tropical wave moved from northern [[Tyrosia]] northeast into the [[Volic Gulf]]. It was monitored by the [[Ari Island Volunteer Meteorological Center]] for several days, but was discontinued from being monitored as it failed to produce atmospheric convection. Over the coming days thereafter, however, the tropical wave slowly organized, and on the 3rd of Agotzo, the wave organized into Tropical Depression 1. Despite the wave's organizing, the AIVMC failed to further monitor the storm until the 10th of Agotzo. [[File:Tropical Cyclone Hudah 2000.jpg\|thumb\|Satellite view of the cyclone at 8:00 AM on the 9th of Agotzo (24th of Snoiguia) as a cyclone, just before it explosively intesified.\|248x248px]]Over the next three days, the tropical depression moved nortwest, entering into a zone with anomalously warm water temperatures and little wind shear. By the 6th of Agotzo, the depression had organized further, and began to be monitored by the [[Sunterian Office of Meteorology\|Sunterian Office of Meteorology (Hedieuž)]]. The same day, Hedieuž categorized the depression as a Severe Tropical Storm. At noon on the 7th of Agotzo, hurricane hunters reported the intensification of the cyclone from a Severe Tropical Storm to a Cyclone, with sustained winds of 95 miles per hour, with recorded gusts of up to 110 miles per hour. A mid-level ridge to the north of the cyclone steered it west along an elongated arcing path, into waters with cooler water temperatures. The cyclone stalled and weakened slightly into a Severe Tropical Storm starting at around 10:00 PM on the 7th.

	Around this time, Western Azkali and Kalilonde were experiencing significant amounts of rainfall, on average approximately 3 inches. This rain, perpretrated by an extratropical system that had moved from the Talo sea into Kalilonde and Western Azkali, would be responsible for the later reintensification of the system over Kalilonde.		Around this time, Western Azkali and Kalilonde were experiencing significant amounts of rainfall, on average approximately 3 inches. This rain, perpretrated by an extratropical system that had moved from the Talo sea into Kalilonde and Western Azkali, would be responsible for the later reintensification of the system over Kalilonde.

EnigmaticLucas at 04:23, 31 December 2025

2025-12-31T04:23:22Z

← Older revision		Revision as of 04:23, 31 December 2025
Line 1:		Line 1:

	[[File:Tropical Cyclone Edzani 2010-01-09.jpg\|thumb\|302x302px\|The cyclone at it's peak intensity, approaching the Azkali coast at noon on the 11th of Agotzo.]]		[[File:Tropical Cyclone Edzani 2010-01-09.jpg\|thumb\|302x302px\|The cyclone at it's peak intensity, approaching the Azkali coast at noon on the 11th of Agotzo.]]
	The '''1990 Azkali cyclone''' (usually referred to as the '''Naharretazakon''' in [[Azkali]]), known as '''Super''' '''Cyclone ~~116A~~''' (Oikan: ''Uperkuelhuetre ~~116A~~'') in [[Sunteria]], was a devestating off-season [[Volic gulf cyclone\|Volic Gulf cyclone]] that struck [[Azkali]] and [[Sunteria]] on 12 Agotzo 1990 (27 Snoiguia 3116). It remains the cyclone with the fastest recorded wind speed and lowest barometic pressure on record. It was the deadliest tropical cyclone in recorded history, and greatly exacerbated the at the time ongoing [[Azkali societal collapse]], resulting in one of the most devestating humanitarian disasters in the history of the world. It caused approximately 400,000 deaths, and possibly as much as 750,000. These casualties were almost solely in Azkali, and caused damages there estimated at $440 billion dollars. The 1990 Azkali cyclone was the first cyclonic storm of the [[1990 Volic cyclone season]].		The '''1990 Azkali cyclone''' (usually referred to as the '''Naharretazakon''' in [[Azkali]]), known as '''Super''' '''Cyclone 3116-A''' (Oikan: ''Uperkuelhuetre 3116-A'') in [[Sunteria]], was a devestating off-season [[Volic gulf cyclone\|Volic Gulf cyclone]] that struck [[Azkali]] and [[Sunteria]] on 12 Agotzo 1990 (27 Snoiguia 3116). It remains the cyclone with the fastest recorded wind speed and lowest barometic pressure on record. It was the deadliest tropical cyclone in recorded history, and greatly exacerbated the at the time ongoing [[Azkali societal collapse]], resulting in one of the most devestating humanitarian disasters in the history of the world. It caused approximately 400,000 deaths, and possibly as much as 750,000. These casualties were almost solely in Azkali, and caused damages there estimated at $440 billion dollars. The 1990 Azkali cyclone was the first cyclonic storm of the [[1990 Volic cyclone season]].

	== Meteorological history ==		== Meteorological history ==

EnigmaticLucas: /* Sunteria */

2025-11-23T16:22:28Z

Sunteria

← Older revision		Revision as of 16:22, 23 November 2025
Line 38:		Line 38:

	==== Kalilonde ====		==== Kalilonde ====
			The storm killed 212 people in Kalilonde.

			===== Pordmisktpelha =====
			The storm killed 17 people in [[Pordmisktpelha]], 8 directly and 9 indirectly. An entire family of four was killed while trying to escape floodwaters in their car. A young woman was killed when winds suddenly shattered a window in her apartment and a shard of glass struck her neck and severed a vein. A teenage boy was killed when winds blew over a bookcase, which fell on him and crushed him. A middle-aged couple was killed when a tree fell on their house while they were sleeping. Five people were killed in a duplex fire sparked by a faulty generator. Three elderly people across the city suffered heart attacks. A disabled elderly man was killed when his oxygen equipment lost power.

			===== Elsewhere =====
			The town of Rekazki was completely destroyed.

	==== Hnerteroika ====		==== Hnerteroika ====

EnigmaticLucas at 17:44, 4 October 2025

2025-10-04T17:44:13Z

← Older revision		Revision as of 17:44, 4 October 2025
Line 1:		Line 1:

	[[File:Tropical Cyclone Edzani 2010-01-09.jpg\|thumb\|302x302px\|The cyclone at it's peak intensity, approaching the Azkali coast at noon on the 11th of Agotzo.]]		[[File:Tropical Cyclone Edzani 2010-01-09.jpg\|thumb\|302x302px\|The cyclone at it's peak intensity, approaching the Azkali coast at noon on the 11th of Agotzo.]]
	The '''1990 Azkali cyclone''' (usually referred to as the '''Naharretazakon''' in [[Azkali]]), known as '''Cyclone 116A''' (Oikan: ''~~Kuelhuetre~~ 116A'') in [[Sunteria]], was a devestating off-season [[Volic gulf cyclone\|Volic Gulf cyclone]] that struck [[Azkali]] and [[Sunteria]] on 12 Agotzo 1990 (27 Snoiguia 3116). It remains the cyclone with the fastest recorded wind speed and lowest barometic pressure on record. It was the deadliest tropical cyclone in recorded history, and greatly exacerbated the at the time ongoing [[Azkali societal collapse]], resulting in one of the most devestating humanitarian disasters in the history of the world. It caused approximately 400,000 deaths, and possibly as much as 750,000. These casualties were almost solely in Azkali, and caused damages there estimated at $440 billion dollars. The 1990 Azkali cyclone was the first cyclonic storm of the [[1990 Volic cyclone season]].		The '''1990 Azkali cyclone''' (usually referred to as the '''Naharretazakon''' in [[Azkali]]), known as '''Super''' '''Cyclone 116A''' (Oikan: ''Uperkuelhuetre 116A'') in [[Sunteria]], was a devestating off-season [[Volic gulf cyclone\|Volic Gulf cyclone]] that struck [[Azkali]] and [[Sunteria]] on 12 Agotzo 1990 (27 Snoiguia 3116). It remains the cyclone with the fastest recorded wind speed and lowest barometic pressure on record. It was the deadliest tropical cyclone in recorded history, and greatly exacerbated the at the time ongoing [[Azkali societal collapse]], resulting in one of the most devestating humanitarian disasters in the history of the world. It caused approximately 400,000 deaths, and possibly as much as 750,000. These casualties were almost solely in Azkali, and caused damages there estimated at $440 billion dollars. The 1990 Azkali cyclone was the first cyclonic storm of the [[1990 Volic cyclone season]].

	== Meteorological history ==		== Meteorological history ==

EnigmaticLucas: /* Meteorological history */

2025-09-23T17:18:52Z

Meteorological history

← Older revision		Revision as of 17:18, 23 September 2025
Line 4:		Line 4:

	== Meteorological history ==		== Meteorological history ==
	On the 24th of Uni, 1990 (Sunterian time), a tropical wave moved from northern [[Tyrosia]] northeast into the [[Volic Gulf]]. It was monitored by the [[Ari Island Volunteer Meteorological Center]] for several days, but was discontinued from being monitored as it failed to produce atmospheric convection. Over the coming days thereafter, however, the tropical wave slowly organized, and on the 3rd of Agotzo, the wave organized into Tropical Depression 1. Despite the wave's organizing, the AIVMC failed to further monitor the storm until the 10th of Agotzo. [[File:Tropical Cyclone Hudah 2000.jpg\|thumb\|Satellite view of the cyclone at 8:00 AM on the 9th of Agotzo (24th of Snoiguia) as a cyclone, just before it explosively intesified.\|248x248px]]Over the next three days, the tropical depression moved nortwest, entering into a zone with anomalously warm water temperatures and little wind shear. By the 6th of Agotzo, the depression had organized further, and began to be monitored by the (~~Sunterian Meteorological agency~~). The same day, ~~the (SMA)~~ categorized the depression as a Severe Tropical Storm. At noon on the 7th of Agotzo, hurricane hunters reported the intensification of the cyclone from a Severe Tropical Storm to a Cyclone, with sustained winds of 95 miles per hour, with recorded gusts of up to 110 miles per hour. A mid-level ridge to the north of the cyclone steered it west along an elongated arcing path, into waters with cooler water temperatures. The cyclone stalled and weakened slightly into a Severe Tropical Storm starting at around 10:00 PM on the 7th.		On the 24th of Uni, 1990 (Sunterian time), a tropical wave moved from northern [[Tyrosia]] northeast into the [[Volic Gulf]]. It was monitored by the [[Ari Island Volunteer Meteorological Center]] for several days, but was discontinued from being monitored as it failed to produce atmospheric convection. Over the coming days thereafter, however, the tropical wave slowly organized, and on the 3rd of Agotzo, the wave organized into Tropical Depression 1. Despite the wave's organizing, the AIVMC failed to further monitor the storm until the 10th of Agotzo. [[File:Tropical Cyclone Hudah 2000.jpg\|thumb\|Satellite view of the cyclone at 8:00 AM on the 9th of Agotzo (24th of Snoiguia) as a cyclone, just before it explosively intesified.\|248x248px]]Over the next three days, the tropical depression moved nortwest, entering into a zone with anomalously warm water temperatures and little wind shear. By the 6th of Agotzo, the depression had organized further, and began to be monitored by the [[Sunterian Office of Meteorology\|Sunterian Office of Meteorology (Hedieuž)]] The same day, Hedieuž categorized the depression as a Severe Tropical Storm. At noon on the 7th of Agotzo, hurricane hunters reported the intensification of the cyclone from a Severe Tropical Storm to a Cyclone, with sustained winds of 95 miles per hour, with recorded gusts of up to 110 miles per hour. A mid-level ridge to the north of the cyclone steered it west along an elongated arcing path, into waters with cooler water temperatures. The cyclone stalled and weakened slightly into a Severe Tropical Storm starting at around 10:00 PM on the 7th.

	Around this time, Western Azkali and Kalilonde were experiencing significant amounts of rainfall, on average approximately 3 inches. This rain, perpretrated by an extratropical system that had moved from the Talo sea into Kalilonde and Western Azkali, would be responsible for the later reintensification of the system over Kalilonde.		Around this time, Western Azkali and Kalilonde were experiencing significant amounts of rainfall, on average approximately 3 inches. This rain, perpretrated by an extratropical system that had moved from the Talo sea into Kalilonde and Western Azkali, would be responsible for the later reintensification of the system over Kalilonde.

EnigmaticLucas: /* Meteorological history */

2025-09-23T17:15:57Z

Meteorological history

← Older revision		Revision as of 17:15, 23 September 2025
Line 4:		Line 4:

	== Meteorological history ==		== Meteorological history ==
	On the 24th of Uni, 1990 (Sunterian time), a tropical wave moved from northern [[Tyrosia]] northeast into the [[Volic Gulf]]. It was monitored by the [[Ari Island Volunteer Meteorological Center]] for several days, but was discontinued from being monitored as it failed to produce atmospheric convection. Over the coming days thereafter, however, the tropical wave slowly organized, and on the 3rd of Agotzo, the wave organized into Tropical Depression 1. Despite the wave's organizing, the AIVMC failed to further monitor the storm until the 10th of Agotzo. [[File:Tropical Cyclone Hudah 2000.jpg\|thumb\|Satellite view of the cyclone at 8:00 AM on the 9th of Agotzo (24th of Snoiguia) as a cyclone, just before it explosively intesified.\|248x248px]]Over the next three days, the tropical depression moved nortwest, entering into a zone with anomalously warm water temperatures and little wind shear. By the 6th of Agotzo, the depression had organized further, and began to be monitored by the (Sunterian Meteorological agency). The same day, the (SMA) categorized the depression as a Severe Tropical Storm ~~- however, it was not given a name, being several months before the start of the cyclone season~~. At noon on the 7th of Agotzo, hurricane hunters reported the intensification of the cyclone from a Severe Tropical Storm to a Cyclone, with sustained winds of 95 miles per hour, with recorded gusts of up to 110 miles per hour. A mid-level ridge to the north of the cyclone steered it west along an elongated arcing path, into waters with cooler water temperatures. The cyclone stalled and weakened slightly into a Severe Tropical Storm starting at around 10:00 PM on the 7th.		On the 24th of Uni, 1990 (Sunterian time), a tropical wave moved from northern [[Tyrosia]] northeast into the [[Volic Gulf]]. It was monitored by the [[Ari Island Volunteer Meteorological Center]] for several days, but was discontinued from being monitored as it failed to produce atmospheric convection. Over the coming days thereafter, however, the tropical wave slowly organized, and on the 3rd of Agotzo, the wave organized into Tropical Depression 1. Despite the wave's organizing, the AIVMC failed to further monitor the storm until the 10th of Agotzo. [[File:Tropical Cyclone Hudah 2000.jpg\|thumb\|Satellite view of the cyclone at 8:00 AM on the 9th of Agotzo (24th of Snoiguia) as a cyclone, just before it explosively intesified.\|248x248px]]Over the next three days, the tropical depression moved nortwest, entering into a zone with anomalously warm water temperatures and little wind shear. By the 6th of Agotzo, the depression had organized further, and began to be monitored by the (Sunterian Meteorological agency). The same day, the (SMA) categorized the depression as a Severe Tropical Storm. At noon on the 7th of Agotzo, hurricane hunters reported the intensification of the cyclone from a Severe Tropical Storm to a Cyclone, with sustained winds of 95 miles per hour, with recorded gusts of up to 110 miles per hour. A mid-level ridge to the north of the cyclone steered it west along an elongated arcing path, into waters with cooler water temperatures. The cyclone stalled and weakened slightly into a Severe Tropical Storm starting at around 10:00 PM on the 7th.

	Around this time, Western Azkali and Kalilonde were experiencing significant amounts of rainfall, on average approximately 3 inches. This rain, perpretrated by an extratropical system that had moved from the Talo sea into Kalilonde and Western Azkali, would be responsible for the later reintensification of the system over Kalilonde.		Around this time, Western Azkali and Kalilonde were experiencing significant amounts of rainfall, on average approximately 3 inches. This rain, perpretrated by an extratropical system that had moved from the Talo sea into Kalilonde and Western Azkali, would be responsible for the later reintensification of the system over Kalilonde.

EnigmaticLucas at 17:12, 23 September 2025

2025-09-23T17:12:40Z

← Older revision		Revision as of 17:12, 23 September 2025
Line 1:		Line 1:

	[[File:Tropical Cyclone Edzani 2010-01-09.jpg\|thumb\|302x302px\|The cyclone at it's peak intensity, approaching the Azkali coast at noon on the 11th of Agotzo.]]		[[File:Tropical Cyclone Edzani 2010-01-09.jpg\|thumb\|302x302px\|The cyclone at it's peak intensity, approaching the Azkali coast at noon on the 11th of Agotzo.]]
	The '''1990 Azkali cyclone''' (usually referred to as the '''Naharretazakon''' in [[Azkali]]) was a devestating off-season [[Volic gulf cyclone\|Volic Gulf cyclone]] that struck [[Azkali]] and [[Sunteria]] on 12 Agotzo 1990 (27 Snoiguia 3116). It remains the cyclone with the fastest recorded wind speed and lowest barometic pressure on record. It was the deadliest tropical cyclone in recorded history, and greatly exacerbated the at the time ongoing [[Azkali societal collapse]], resulting in one of the most devestating humanitarian disasters in the history of the world. It caused approximately 400,000 deaths, and possibly as much as 750,000. These casualties were almost solely in Azkali, and caused damages there estimated at $440 billion dollars. The 1990 Azkali cyclone was the first cyclonic storm of the [[1990 Volic cyclone season]].		The '''1990 Azkali cyclone''' (usually referred to as the '''Naharretazakon''' in [[Azkali]]), known as '''Cyclone 116A''' (Oikan: ''Kuelhuetre 116A'') in [[Sunteria]], was a devestating off-season [[Volic gulf cyclone\|Volic Gulf cyclone]] that struck [[Azkali]] and [[Sunteria]] on 12 Agotzo 1990 (27 Snoiguia 3116). It remains the cyclone with the fastest recorded wind speed and lowest barometic pressure on record. It was the deadliest tropical cyclone in recorded history, and greatly exacerbated the at the time ongoing [[Azkali societal collapse]], resulting in one of the most devestating humanitarian disasters in the history of the world. It caused approximately 400,000 deaths, and possibly as much as 750,000. These casualties were almost solely in Azkali, and caused damages there estimated at $440 billion dollars. The 1990 Azkali cyclone was the first cyclonic storm of the [[1990 Volic cyclone season]].

	== Meteorological history ==		== Meteorological history ==

Photosynthesis bisectors: /* Meteorological history */

2025-02-10T17:49:41Z

Meteorological history

← Older revision		Revision as of 17:49, 10 February 2025
Line 4:		Line 4:

	== Meteorological history ==		== Meteorological history ==
	On the 24th of Uni, 1990 (Sunterian time), a tropical wave moved from northern [[Tyrosia]] northeast into the [[Volic Gulf]]. It was monitored by the [[Ari Island Volunteer Meteorological Center]] for several days, but was discontinued from being monitored as it failed to produce atmospheric convection. Over the coming days thereafter, however, the tropical wave slowly organized, and on the 3rd of Agotzo, the wave organized into Tropical Depression 1. Despite the wave's organizing, the AIVMC failed to further monitor the storm until the 10th of Agotzo. [[File:Tropical Cyclone Hudah 2000.jpg\|thumb\|Satellite view of the cyclone at 8:00 AM on the 9th of Agotzo (24th of Snoiguia) as a cyclone, just before it explosively intesified.\|248x248px]]Over the next three days, the tropical depression moved ~~northeast~~, entering into a zone with anomalously warm water temperatures and little wind shear. By the 6th of Agotzo, the depression had organized further, and began to be monitored by the (Sunterian Meteorological agency). The same day, the (SMA) categorized the depression as a Severe Tropical Storm - however, it was not given a name, being several months before the start of the cyclone season. At noon on the 7th of Agotzo, hurricane hunters reported the intensification of the cyclone from a Severe Tropical Storm to a Cyclone, with sustained winds of 95 miles per hour, with recorded gusts of up to 110 miles per hour. A mid-level ridge to the north of the cyclone steered it west along an elongated arcing path, into waters with cooler water temperatures. The cyclone stalled and weakened slightly into a Severe Tropical Storm starting at around 10:00 PM on the 7th.		On the 24th of Uni, 1990 (Sunterian time), a tropical wave moved from northern [[Tyrosia]] northeast into the [[Volic Gulf]]. It was monitored by the [[Ari Island Volunteer Meteorological Center]] for several days, but was discontinued from being monitored as it failed to produce atmospheric convection. Over the coming days thereafter, however, the tropical wave slowly organized, and on the 3rd of Agotzo, the wave organized into Tropical Depression 1. Despite the wave's organizing, the AIVMC failed to further monitor the storm until the 10th of Agotzo. [[File:Tropical Cyclone Hudah 2000.jpg\|thumb\|Satellite view of the cyclone at 8:00 AM on the 9th of Agotzo (24th of Snoiguia) as a cyclone, just before it explosively intesified.\|248x248px]]Over the next three days, the tropical depression moved nortwest, entering into a zone with anomalously warm water temperatures and little wind shear. By the 6th of Agotzo, the depression had organized further, and began to be monitored by the (Sunterian Meteorological agency). The same day, the (SMA) categorized the depression as a Severe Tropical Storm - however, it was not given a name, being several months before the start of the cyclone season. At noon on the 7th of Agotzo, hurricane hunters reported the intensification of the cyclone from a Severe Tropical Storm to a Cyclone, with sustained winds of 95 miles per hour, with recorded gusts of up to 110 miles per hour. A mid-level ridge to the north of the cyclone steered it west along an elongated arcing path, into waters with cooler water temperatures. The cyclone stalled and weakened slightly into a Severe Tropical Storm starting at around 10:00 PM on the 7th.

	Around this time, Western Azkali and Kalilonde were experiencing significant amounts of rainfall, on average approximately 3 inches. This rain, perpretrated by an extratropical system that had moved from the Talo sea into Kalilonde and Western Azkali, would be responsible for the later reintensification of the system over Kalilonde.		Around this time, Western Azkali and Kalilonde were experiencing significant amounts of rainfall, on average approximately 3 inches. This rain, perpretrated by an extratropical system that had moved from the Talo sea into Kalilonde and Western Azkali, would be responsible for the later reintensification of the system over Kalilonde.

Photosynthesis bisectors at 16:27, 7 February 2025

2025-02-07T16:27:23Z

@@ Line 1: / Line 1: @@
 [[File:Tropical Cyclone Edzani 2010-01-09.jpg|thumb|302x302px|The cyclone at it's peak intensity, approaching the Azkali coast at noon on the 11th of Agotzo.]]
@@ Line 40: / Line 6: @@
 On the 24th of Uni, 1990 (Sunterian time), a tropical wave moved from northern [[Tyrosia]] northeast into the [[Volic Gulf]]. It was monitored by the [[Ari Island Volunteer Meteorological Center]] for several days, but was discontinued from being monitored as it failed to produce atmospheric convection. Over the coming days thereafter, however, the tropical wave slowly organized, and on the 3rd of Agotzo, the wave organized into Tropical Depression 1. Despite the wave's organizing, the AIVMC failed to further monitor the storm until the 10th of Agotzo. [[File:Tropical Cyclone Hudah 2000.jpg|thumb|Satellite view of the cyclone at 8:00 AM on the 9th of Agotzo (24th of Snoiguia) as a cyclone, just before it explosively intesified.|248x248px]]Over the next three days, the tropical depression moved northeast, entering into a zone with anomalously warm water temperatures and little wind shear. By the 6th of Agotzo, the depression had organized further, and began to be monitored by the (Sunterian Meteorological agency). The same day, the (SMA) categorized the depression as a Severe Tropical Storm - however, it was not given a name, being several months before the start of the cyclone season. At noon on the 7th of Agotzo, hurricane hunters reported the intensification of the cyclone from a Severe Tropical Storm to a Cyclone, with sustained winds of 95 miles per hour, with recorded gusts of up to 110 miles per hour. A mid-level ridge to the north of the cyclone steered it west along an elongated arcing path, into waters with cooler water temperatures. The cyclone stalled and weakened slightly into a Severe Tropical Storm starting at around 10:00 PM on the 7th.
-Around this time, Western Azkali and Kalilonde were experiencing significant amounts of rainfall, on average approximately 3 or 4 inches so.
+Around this time, Western Azkali and Kalilonde were experiencing significant amounts of rainfall, on average approximately 3 inches. This rain, perpretrated by an extratropical system that had moved from the Talo sea into Kalilonde and Western Azkali, would be responsible for the later reintensification of the system over Kalilonde.
 The next day, the cyclone started again west, into an environment with ocean temperatures exceptionally conductive to explosive intensification. By 4:00 AM on the 8th, it had re-intensified into a cyclone, but was prevented from strengthening that day due to significant wind shear in the cyclone's path. Wind shear gradually dissipated over the day, and by 11:00 PM on the 8th, the cyclone weakened slightly once more to a severe tropical storm, before explosively intensifying into a Super Cyclone, starting at 9:00 AM on the 9th of Agotzo. Hurricane hunters around this time reported the increase of the cyclone's 10 minute sustained wind speed from approximately 85 miles an hour to 200 miles an hour in six hours, an intensification of 115 miles an hour within 6 hours, or approximately an increase of 20 an hour.
@@ Line 46: / Line 12: @@
 In the days before landfall, the cyclone intensified to its record breaking maximum wind speed, an estimated 230 miles an hour. In the hours before it made landfall, it slightly weakened, leaving it's landfall wind speed at a staggering 220 miles an hour.
-The cyclone made landfall at 11:40 AM on the 12th of Agotzo, in the village of [[Hengatzeisu (township)|Hengatzeisu]]. As it made landfall onto the southern Azkali coast, the cyclone stalled for several days, causing catastrophic rainfall; the maximum recorded being in the village of [[Ngetetz]], a suburb of [[Retzal]], with a record breaking 212 inches of rainfall over thirty-six hours, a world record. The cyclone slowly weakened from a super cyclone to a cyclone, still sustaining winds of over 100 miles an hour until the 16th of Agotzo. On the 17th, the cyclone began to weaken further and headed northwest, reentering the Volic Gulf on the 18th. It curved northeast, quickly intensifying into a Super Cyclone with winds of 160 miles an hour, before making a second landfall at [[Ichatzoaka]]. However, before making landfall, Tthe cyclone weakened into a severe tropical storm, and as it made landfall, curved northwest, heading into [[Kalilonde]]. The cyclone continued to drop catastrophic levels of rainfall as it stayed over land, and the cyclone even re-intensified into a proper cyclone as it continued into Kalilonde, perpetuated by the massive amount of rainfall that had occured in western Azkali and Kalilonde days before; a textbook example of the [[W:Brown ocean effect|Brown ocean effect]].
+The cyclone made landfall at 11:40 AM on the 12th of Agotzo, in the village of [[Hengatzeisu (township)|Hengatzeisu]]. As it made landfall onto the southern Azkali coast, the cyclone stalled for several days, causing catastrophic rainfall; the maximum recorded being in the village of [[Ngetetz]], a suburb of [[Retzal]], with a record breaking 212 inches of rainfall over thirty-six hours, a world record. The cyclone slowly weakened from a super cyclone to a cyclone, still sustaining winds of over 100 miles an hour until the 16th of Agotzo. On the 17th, the cyclone began to weaken further and headed northwest, reentering the Volic Gulf on the 18th. It curved northwest, quickly intensifying into a Super Cyclone with winds of 160 miles an hour, before making a second landfall at [[Ichatzoaka]]. However, before making landfall, the cyclone weakened into a severe tropical storm, and as it made landfall, curved northwest, heading into [[Kalilonde]]. The cyclone continued to drop catastrophic levels of rainfall as it stayed over land, and the cyclone even re-intensified into a proper cyclone as it continued into Kalilonde, perpetuated by the massive amount of rainfall that had occured in western Azkali and Kalilonde days before; a textbook example of the [[W:Brown ocean effect|Brown ocean effect]].
-However, starting on the 19th, as it entered into dry land, the cyclone quickly weakened, and by 9:00 AM on the 20th, it transitioned into an extratropical system. The remnants continued to move northwest it was absorbed another extratropical system
+However, starting on the 19th, as it entered into dry land, the cyclone quickly weakened, and by 9:00 AM on the 20th, it transitioned into an extratropical system. The remnants continued to move northwest it was absorbed another extratropical system.
 == Preparations ==
@@ Line 59: / Line 25: @@
 ==== Southern Azkali ====
-Southern Azkali was the most affected portion of Azkali. The impacts of the cyclone can still be clearly seen in modern times - almost all communities save large cities were completely obliterated by the cyclone's rain and wind. The meteorological station at Hengatzeisu recorded a maximum wind speed at the time of landfall of 218 miles an hour, with gusts estimated to have been up to 275-300 miles an hour, before its anemometer was blown off. The [[MS Ari]], docked at Hengatzeisu and holding approximately four hundred refugees, was blown out into the sea and was [[Sinking of the MS Ari|capsized in the gulf]]. As the storm made landfall, it caused an average of a 12.2 meter storm surge which overtopped almost every building in affected communities. A fourty two meter rogue wave, the tallest ever recorded in global history, completely destroyed the town of [[Herisour]].
+Southern Azkali was the most affected portion of Azkali. The impacts of the cyclone can still be clearly seen in modern times - almost all communities save large cities were destroyed by the cyclone's rain and wind. The meteorological station at Hengatzeisu recorded a maximum wind speed at the time of landfall of 218 miles an hour, with gusts estimated to have been up to 275-300 miles an hour, before its anemometer was blown off. The [[MS Ari]], docked at Hengatzeisu and holding approximately four hundred refugees, was blown out into the sea and was [[Sinking of the MS Ari|capsized in the gulf]]. As the storm made landfall, it caused an average of a 12.2 meter storm surge which overtopped almost every building in affected communities. A fourty two meter rogue wave, the tallest ever recorded in global history, completely destroyed the town of [[Herisour]].
 Radio Atzogui reported that almost three fourths of all who lived between Meithakoli and Atzogui were killed by the storm. Flights over the area after the event showed almost apocalyptic destruction between this area, which was quickly dubbed as the ''[[Cyclone corridor (Azkali)|cyclone corridor]]'', a nickname which still persists today.[[File:FEMA - 20460 - Photograph by Marvin Nauman taken on 11-19-2005 in Louisiana.jpg|thumb|369x369px|Township of [[Rekazki]], an [[Azkalophone]] community in [[Kalilonde]], [[Sunteria]], completely destroyed. Photograph taken on 28th of August, 1990]]
@@ Line 74: / Line 42: @@
 == Aftermath ==
 == Records ==

Photosynthesis bisectors at 16:17, 7 February 2025

2025-02-07T16:17:31Z

← Older revision		Revision as of 16:17, 7 February 2025
Line 1:		Line 1:
			{{Short description\|2005 category 5 Atlantic hurricane}}
			{{Distinguish\|Hurricane Catarina\|Hurricane Karina}}
			{{Other hurricanes\|List of storms named Katrina}}
			{{Pp-semi-indef}}
			{{Pp-move}}
			{{Use American English\|date=September 2024}}
			{{Use mdy dates\|date=September 2024}}
			{{Infobox weather event
			\| image = Katrina 2005-08-28 1700Z.jpg
			\| caption = Katrina at peak intensity in the [[Gulf of Mexico]] on August 28
			\| formed = August 23, 2005
			\| extratropical = August 30, 2005
			\| dissipated = August 31, 2005
			}}{{Infobox weather event/NWS
			\| winds = 150
			\| pressure = 902
			}}{{Infobox weather event/Effects
			\| year = 2005
			\| fatalities = 1,392 total
			\| missing = 652
			\| damage = 125000000000
			\| damage-suffix = <br/>([[List of the costliest tropical cyclones\|Tied as the costliest tropical cyclone on record,]] costliest when adjusted for inflation)
			\| areas = {{flatlist\|
			* [[Bahamas]]
			* [[Southeastern United States]] (especially [[Florida]], [[Louisiana]], and [[Mississippi]])
			* [[Cuba]]
			* [[Northeastern United States]]
			* [[Eastern Canada]]
			}}
			\| refs =
			}}{{Infobox weather event/Footer
			\| season = [[2005 Atlantic hurricane season]]
			}}
			{{Katrina}}

	[[File:Tropical Cyclone Edzani 2010-01-09.jpg\|thumb\|302x302px\|The cyclone at it's peak intensity, approaching the Azkali coast at noon on the 11th of Agotzo.]]		[[File:Tropical Cyclone Edzani 2010-01-09.jpg\|thumb\|302x302px\|The cyclone at it's peak intensity, approaching the Azkali coast at noon on the 11th of Agotzo.]]
	The '''1990 Azkali cyclone''' (usually referred to as the '''Naharretazakon''' in [[Azkali]]) was a devestating off-season [[Volic gulf cyclone\|Volic Gulf cyclone]] that struck [[Azkali]] and [[Sunteria]] on 12 Agotzo 1990 (27 Snoiguia 3116). It remains the cyclone with the fastest recorded wind speed and lowest barometic pressure on record. It was the deadliest tropical cyclone in recorded history, and greatly exacerbated the at the time ongoing [[Azkali societal collapse]], resulting in one of the most devestating humanitarian disasters in the history of the world. It caused approximately 400,000 deaths, and possibly as much as 750,000. These casualties were almost solely in Azkali, and caused damages there estimated at $440 billion dollars. The 1990 Azkali cyclone was the first cyclonic storm of the [[1990 Volic cyclone season]].		The '''1990 Azkali cyclone''' (usually referred to as the '''Naharretazakon''' in [[Azkali]]) was a devestating off-season [[Volic gulf cyclone\|Volic Gulf cyclone]] that struck [[Azkali]] and [[Sunteria]] on 12 Agotzo 1990 (27 Snoiguia 3116). It remains the cyclone with the fastest recorded wind speed and lowest barometic pressure on record. It was the deadliest tropical cyclone in recorded history, and greatly exacerbated the at the time ongoing [[Azkali societal collapse]], resulting in one of the most devestating humanitarian disasters in the history of the world. It caused approximately 400,000 deaths, and possibly as much as 750,000. These casualties were almost solely in Azkali, and caused damages there estimated at $440 billion dollars. The 1990 Azkali cyclone was the first cyclonic storm of the [[1990 Volic cyclone season]].