521:, one of the largest in the country, were closed as a precautionary measure. On May 25, over 10,000 people were evacuated from coastal areas in the threatened region. Throughout India, a total of 118,800 people were evacuated and 100,000 more were evacuated in Pakistan. The Indian military was placed on standby to undertake search-and-rescue missions immediately after the storms' passage. Fourteen districts of Gujarat were placed on red alert, the highest level of preparedness. Seven emergency control centers were set up across the country and officials alerted hospitals and fire crews about the approaching storm.
605:
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409:
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Operationally, the JTWC issued their final advisory on the cyclone on May 28 as it weakened to a tropical depression over open waters. The once powerful cyclone, now devoid of all convection, tracked towards the northwestern coast of India. During the afternoon of May 29, the cyclone rapidly regenerated as it made
936:
533:. In the Valsad district, two coastal communities lost a combined 200 homes due to large swells produced by the storm. Offshore, between 1,500 and 2,000 fishing vessels had lost contact with the mainland. Later reports indicated that between 120 and 900 fishermen had gone missing as a result of the cyclone.
528:
of that year that killed over 20,000 people. Additional disaster relief teams were deployed to the region to further prepare residents for the cyclone. Food, water and other necessities were stored and ready to be provided to victims of the storm. Large swells produced by the storm affected a large
491:
equivalent storm by the morning of May 24. Later that morning, 01A attained its peak intensity with winds of 205 km/h (125 mph), according to the JTWC. However, the IMD considered the storm to be slightly stronger, estimating that it attained winds of 215 km/h (135 mph) by
263:
on May 18. Over the following few days, the system gradually organized into a tropical depression. Tracking eastward, towards the coastline of southwestern India, the storm slowly intensified. Shortly before reaching shore, the system turned north and later west, away from land. After taking
482:
developed within the center of circulation during this intensification phase. Throughout most of May 22, the strengthening slowed considerably as it paralleled the southwestern coast of India. Initially, it was feared that the storm would move inland as a powerful cyclone; however, a
500:
tore convection away from the cyclone and caused it to become disorganized. Within 48 hours, the system had degraded to a tropical storm and was situated roughly 555 km (345 mi) west-southwest of Mumbai. The weakening trend lessened shortly thereafter but still continued.
940:
455:. Several hours later, they began monitoring the system as a tropical depression with the identifier 01A; however, operational advisories were not issued until the cyclone was estimated to have attained tropical storm intensity. By the morning of May 22, the
287:
After stalling several hundred kilometres offshore, the storm weakened over cooler waters that it had upwelled. By May 27, the system weakened to a cyclonic storm and by this time was approaching the northwestern coastline of India, near
569:), the lowest in the region at the time. The cyclone was ranked as the strongest in the Arabian Sea for six years until it was surpassed by Gonu in 2007, which attained a minimum pressure of 920 mbar (hPa). In 2010,
495:
At the time of peak intensity, the cyclone displayed a well-defined eye and excellent outflow. Although a powerful storm, it quickly weakened as conditions became hostile for tropical cyclone development. Strong
509:. The JTWC estimated that it crossed the coastline with winds of 100 km/h (60 mph). Not long after moving overland, the system rapidly weakened and dissipated over India within several hours.
311:
produced by the storm. However, the losses were more extensive offshore. Between 120 and 900 fishermen were listed as missing after contact was lost with their vessels during the storm.
573:
surpassed the 2001 cyclone as the second-strongest storm in the region, attaining winds of 230 km/h (145 mph), according to the JTWC. Again it was surpassed to sixth place as
886:
487:
over the northern
Arabian Sea caused the storm to turn westward, back over open water. Once further away from land, the cyclone resumed intensification, becoming a rare,
1046:
704:
549:. However, in post-storm analysis, it was discovered that 1-minute winds did not exceed 205 km/h (125 mph). The next storm to reach this intensity was
545:
storm by the JTWC, with peak winds of 215 km/h (135 mph). This would have made the system the first recorded storm of that intensity on record in the
1013:
264:
this turn, the storm intensified into a very severe cyclonic storm, attaining its peak intensity on May 24 with winds of 215 km/h (130 mph
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470:. By the afternoon of May 22, the JTWC estimated that 01A attained winds of 120 km/h (75 mph), equivalent to a
589:
surpassed its windspeed intensity as they become category 4 tropical cyclones in later years. Now this cyclone is tied with
557:, which became the first known super cyclonic storm in the region. Upon attaining its peak intensity, the storm attained a
1050:
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on May 18. The following day, the system was determined to be relatively stationary near the island of
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Situated in a region favoring tropical cyclone development about 650 km (400 mi) southwest of
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439:. By May 20, the disturbance slowly moved towards the southeast in response to an upper-level
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three-minute sustained winds along with a barometric pressure of 932 mbar (hPa; 27.52 inHg).
303:
Although a powerful cyclone over water, the storm had relatively little impact over land. In the
202:
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300:). The depression quickly weakened after moving inland and dissipated early on May 29.
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The origins of the 2001 Gujarat cyclone can be traced to a tropical disturbance over the
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developed. A mid-level circulation finally developed late on May 21, prompting the
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were stronger. The storm originated from a tropical disturbance that formed east of
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323:
Map plotting the storm's track and intensity, according to the Saffir–Simpson scale
244:
831:
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593:
for sixth strongest cyclone in
Arabian Sea based on windspeed of one minute mean.
17:
912:
International
Federation of Red Cross And Red Crescent Societies (May 25, 2001).
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Several relief agencies were already positioned in the region in response to a
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280:). At the time, this ranked the cyclone as the strongest known storm in the
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887:"India's quake-hit Gujarat braces as giant cyclone gathers strength"
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portion of the western Indian coastline, especially in the city of
318:
307:, two coastal communities lost a combined 200 homes due to large
1106:
435:
was associated with the disturbance, there was no evidence of a
443:
over India. The overall structure gradually improved as good
296:
as a deep depression with winds of 55 km/h (35 mph
1076:. Naval Meteorology and Oceanography Command. Archived from
1049:. Naval Meteorology and Oceanography Command. Archived from
1019:. Naval Meteorology and Oceanography Command. Archived from
989:. Naval Meteorology and Oceanography Command. Archived from
707:. Naval Meteorology and Oceanography Command. Archived from
889:. ReliefWeb. Associated Press. May 27, 2001. Archived from
347:
Tropical storm (39–73 mph, 63–118 km/h)
342:
Tropical depression (≤38 mph, ≤62 km/h)
415:, remnant low, tropical disturbance, or monsoon depression
367:
Category 4 (130–156 mph, 209–251 km/h)
362:
Category 3 (111–129 mph, 178–208 km/h)
357:
Category 2 (96–110 mph, 154–177 km/h)
352:
Category 1 (74–95 mph, 119–153 km/h)
738:. India Meteorological Department. 2009. Archived from
517:
Ahead of the storm, all ports in
Gujarat, including
372:
Category 5 (≥157 mph, ≥252 km/h)
292:. The following day, the storm made landfall in the
191:
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The cyclone shortly before peak intensity on May 23
809:"100,000 Pakistanis who fled storm to return home"
541:Operationally, the cyclone was considered to be a
1047:"JTWC Best Track for Tropical Cyclone 02A (Gonu)"
987:"JTWC North Indian Ocean Best Tracks 1945–2008"
811:. ReliefWeb. Agence France-Presse. May 29, 2001
673:"Monthly Tropical Weather Summary for May 2001"
478:. Additionally, a 22 km (14 mi)-wide
964:"Monthly Tropical Cyclone Tracks for May 2001"
762:"India cyclone weakening but still 'a threat'"
1072:Joint Typhoon Warning Center (June 2, 2010).
8:
30:
914:"India: Cyclone Information Bulletin No. 1"
1074:"Cyclone Phet (03A) Advisory Number Eight"
939:. The Record. p. D.21. Archived from
634:List of the most intense tropical cyclones
205:
36:
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832:"Gujarat govt geared up to face cyclone"
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694:
692:
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730:
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619:2001 North Indian Ocean cyclone season
555:2007 North Indian Ocean cyclone season
459:(IMD) also took notice of the system.
219:2001 North Indian Ocean cyclone season
120:Category 3-equivalent tropical cyclone
1045:Joint Typhoon Warning Center (2008).
1014:"2001 Annual Tropical Cyclone Report"
1012:Joint Typhoon Warning Center (2002).
985:Joint Typhoon Warning Center (2009).
703:Joint Typhoon Warning Center (2002).
7:
858:"M 7.7 - 17 km NW of Bhach?u, India"
736:"IMD Best Tracks Data ( 1990–2008 )"
666:
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787:"Cyclone threatens India, Pakistan"
526:magnitude 7.7 earthquake in January
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1131:Extremely severe cyclonic storms
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453:Tropical Cyclone Formation Alert
407:
397:
387:
1102:India Meteorological Department
457:India Meteorological Department
72:Extremely severe cyclonic storm
962:Gary Padgett (June 11, 2001).
671:Gary Padgett (July 10, 2001).
476:Saffir–Simpson hurricane scale
1:
1146:Tropical cyclones in Pakistan
935:Staff Writer (May 26, 2001).
830:Vikram Vakil (May 24, 2001).
1107:Joint Typhoon Warning Center
789:. CNN. Reuters. May 25, 2001
764:. CNN. Reuters. May 26, 2001
449:Joint Typhoon Warning Center
145:205 km/h (125 mph)
93:215 km/h (130 mph)
27:North Indian cyclone in 2001
1167:
1141:Tropical cyclones in India
937:"Cyclone Rips Into Bombay"
1151:Tropical cyclones in 2001
472:Category 1 hurricane
243:on record; only Cyclones
214:
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125:
77:
35:
705:"Cyclone 01A Best Track"
611:Tropical cyclones portal
231:was the third strongest
1136:2001 disasters in India
513:Preparations and impact
179:120–900 dead or missing
866:U.S. Geological Survey
420:
315:Meteorological history
49:Meteorological history
543:Category 4 equivalent
437:low-level circulation
413:Extratropical cyclone
322:
742:on November 16, 2009
334:Saffir–Simpson scale
229:2001 Gujarat cyclone
150:Lowest pressure
98:Lowest pressure
31:2001 Gujarat cyclone
943:on October 24, 2012
862:earthquake.usgs.gov
856:(26 January 2001).
559:barometric pressure
403:Subtropical cyclone
270:barometric pressure
237:barometric pressure
32:
1112:2010-03-01 at the
1053:on October 9, 2012
451:(JTWC) to issue a
421:
142:Highest winds
127:1-minute sustained
90:Highest winds
79:3-minute sustained
18:2001 India cyclone
1080:on August 7, 2010
893:on August 5, 2012
468:rapidly developed
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294:Saurashtra region
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239:, to form in the
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16:(Redirected from
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1082:. Retrieved
1078:the original
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1057:December 13,
1055:. Retrieved
1051:the original
1040:
1030:December 13,
1028:. Retrieved
1021:the original
1007:
997:December 13,
995:. Retrieved
991:the original
980:
970:December 13,
968:. Retrieved
957:
947:December 13,
945:. Retrieved
941:the original
930:
920:December 13,
918:. Retrieved
907:
897:December 13,
895:. Retrieved
891:the original
881:
869:. Retrieved
861:
848:
838:December 13,
836:. Retrieved
825:
815:December 13,
813:. Retrieved
803:
793:December 13,
791:. Retrieved
768:December 13,
766:. Retrieved
756:
746:December 13,
744:. Retrieved
740:the original
713:. Retrieved
709:the original
679:December 13,
677:. Retrieved
624:Cyclone Gonu
591:Cyclone Megh
571:Cyclone Phet
561:of 932
551:Cyclone Gonu
540:
523:
516:
494:
466:, the storm
461:
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382:
332:
302:
286:
272:of 932
228:
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217:
216:Part of the
126:
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66:May 29, 2001
58:May 21, 2001
916:. ReliefWeb
547:Arabian Sea
425:Arabian Sea
282:Arabian Sea
241:Arabian Sea
1125:Categories
640:References
498:wind shear
433:convection
383:Storm type
176:Casualties
63:Dissipated
871:29 August
1110:Archived
834:. Rediff
597:See also
503:landfall
377:Unknown
268:) and a
1084:June 3,
715:June 3,
537:Records
507:Gujarat
474:on the
445:outflow
429:Socotra
327:Map key
290:Gujarat
261:Somalia
203:IBTrACS
187:Minimal
531:Bombay
519:Kandla
441:trough
375:
370:
365:
360:
355:
350:
345:
340:
309:swells
184:Damage
55:Formed
1024:(PDF)
1017:(PDF)
485:ridge
253:Kyarr
131:SSHWS
1086:2010
1059:2009
1032:2009
999:2009
972:2009
949:2009
922:2009
899:2009
873:2021
854:ANSS
840:2009
817:2009
795:2009
770:2009
748:2009
717:2010
681:2009
585:and
563:mbar
274:mbar
257:2019
251:and
249:2007
245:Gonu
227:The
164:inHg
160:mbar
154:927
135:JTWC
112:inHg
108:mbar
102:932
567:hPa
553:in
505:in
480:eye
278:hPa
255:in
247:in
156:hPa
104:hPa
83:IMD
1127::
864:.
860:.
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129:(
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Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
