1991 North Indian Ocean cyclone season

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1991 North Indian Ocean cyclone season
1991 North Indian Ocean cyclone season summary.jpg
Season summary map
Seasonal boundaries
First system formedJanuary 17, 1991
Last system dissipatedNovember 16, 1991
Strongest storm
Name BOB 01
  Maximum winds235 km/h (145 mph)
(3-minute sustained)
  Lowest pressure920 hPa (mbar)
Seasonal statistics
Depressions8 official, 1 unofficial
Deep depressions4
Cyclonic storms3
Severe cyclonic storms1
Very severe cyclonic storms1
Extremely severe cyclonic storms1
Super cyclonic storms1
Total fatalities>138,906
Total damage$1.7 billion (1991 USD)
Related articles
North Indian Ocean tropical cyclone seasons
1989, 1990, 1991, 1992, 1993

The 1991 North Indian Ocean Cyclone season was an extremely deadly and destructive season causing the deaths of more than 138,000 people and over $1.5 billion in damages. It was the period in which tropical cyclones formed to the north of the equator in the Indian Ocean. During the season tropical cyclones were monitored by the India Meteorological Department (IMD) and the Joint Typhoon Warning Center. The IMD assigned all depressions that it monitored with BOB followed by a number in numerical order. The JTWC also assigned a number and either the letter A or B depending on where the depression was when the first advisory was issued.

Contents

During the year there were eight depressions that were monitored by the IMD while the JTWC monitored four during the year of which one was not monitored by the IMD. The first cyclone of the year formed on January 17 and had little effect on ships that were moving through the Arabian sea to take part in the Gulf War. The deadliest cyclone during the year was Super Cyclonic Storm BOB 01, which killed over 138,000 people.

Season summary

1991 Bangladesh cyclone1991 North Indian Ocean cyclone season

During 1991 the India Meteorological Department officially monitored eight cyclonic disturbances, which included five depressions and three cyclonic storms. [1] [2] For the sixth and final year in a row, there was no cyclonic storms officially monitored within the Arabian Sea. However, the United States Joint Typhoon Warning Center unofficially monitored a tropical storm within the Arabian Sea, during January that posed a direct threat to Coalition forces in the buildup to the Gulf war. [3] The first official system of the season was the strongest, deadliest, and most damaging system of the season

Systems

Super Cyclonic Storm BOB 01

Super cyclonic storm (IMD)
Category 5 tropical cyclone (SSHWS)
BOB 01 Apr 29 1991 1200Z.png   1991 Bangladesh cyclone track.png
DurationApril 22 – April 30
Peak intensity235 km/h (145 mph) (3-min); 920  hPa  (mbar)

BOB 01, tracked by the Joint Typhoon Warning Center as 02B, hit Bangladesh on April 29 as a strong cyclone. [4] It brought a tremendous storm surge and massive wind damage, resulting in the deaths of over 138,000 people. BOB 01 was the deadliest cyclone on Earth since the 1970 Bhola Cyclone. It also destroyed an estimated 1 million homes, leaving as many as 10 million people (a substantial portion of the country's population) homeless.

Cyclonic Storm BOB 02

Cyclonic storm (IMD)
Tropical storm (SSHWS)
03B Jun 2 1991 0113Z.png   Cyclone 03B 1991 track.png
DurationMay 30 – June 3
Peak intensity85 km/h (50 mph) (3-min); 990  hPa  (mbar)

On May 30, a depression formed in the Bay of Bengal. It moved north-northeastward and strengthened to a 60 mph tropical storm on June 2. BOB 02 affected the same region as the super cyclonic storm nearly a month earlier. Although the storm disrupted relief efforts, as a result of well-executed warnings, it caused no reported fatalities. BOB 02 dissipated inland the next day.

Deep Depression BOB 03

Deep depression (IMD)
BOB 03 Jul 28 1991 1355Z.png   Cyclone BOB 03 1991.png
DurationJuly 27 – July 31
Peak intensity55 km/h (35 mph) (3-min); 984  hPa  (mbar)

During July 27, a depression developed over the northern Bay of Bengal to the east of the Indian state of Odisha. [2] [4] Over the next day the system moved westwards and developed into a Deep Depression, as it made landfall near Badudebpur in Odisha with estimated winds of 55 km/h (35 mph). [4] The system dissipated over East Rajasthan during July 31, as it enhanced monsoon activities over northern and eastern India. [4]

Depression BOB 04

Depression (IMD)
BOB 04 Aug 22 1991 1415Z.png   Cyclone BOB 04 1991.png
DurationAugust 21 – August 26
Peak intensity45 km/h (30 mph) (3-min); 992  hPa  (mbar)

Early on August 22, reported that Depression BOB 04 had formed about 160 km (100 mi), to the southeast of Balasore, India. [4] As the depression moved towards northwest, it failed to intensify any further. [4] The depression made landfall in the Indian state of Odisha later that day and maintained its identity until it weakened into a low-pressure area early on August 26. [4] The depression's windspeeds were estimated to have peaked at 45 km/h (30 mph), whilst the lowest pressure recorded was 992 hPa. [4]

Depression BOB 05

Depression (IMD)
BOB 05 Sep 21 1991 1351Z.png   Cyclone BOB 05 1991.png
DurationSeptember 21 – September 22
Peak intensity45 km/h (30 mph) (3-min); 1000  hPa  (mbar)

Depression BOB 05 developed in the Bay of Bengal on September 21. It struck Andhra Pradesh and dissipated the following day.

Depression BOB 06

Depression (IMD)
BOB 06 Oct 14 1991 0122Z.png   Cyclone BOB 06 1991.png
DurationOctober 12 – October 14
Peak intensity45 km/h (30 mph) (3-min); 998  hPa  (mbar)

Depression BOB 06 developed in the Bay of Bengal on October 12. It struck Bangladesh and dissipated on October 14.

Depression BOB 07

Depression (IMD)
BOB 07 Oct 29 1991 0929Z.png   Cyclone BOB 07 1991.png
DurationOctober 28 – October 30
Peak intensity45 km/h (30 mph) (3-min); 998  hPa  (mbar)

Depression BOB 07 developed in the Bay of Bengal on October 28. It struck Tamil Nadu and dissipated on October 30.

Cyclonic Storm BOB 08

Cyclonic storm (IMD)
Tropical storm (SSHWS)
04B Nov 14 1991 2222Z.png   Cyclone 04B 1991 track.png
DurationNovember 9 – November 16
Peak intensity85 km/h (50 mph) (3-min); 998  hPa  (mbar)

The final storm of the season, which formed in the eastern Bay of Bengal on November 9, hit eastern India as a 45 mph tropical storm on the 15th. It dissipated the next day over the country.

The Cyclonic storm brought torrential rain and flash floods across southern India when it made landfall. Twenty-four-hour rainfall totaled 480 millimetres (19 in) at Karaikal. [5] As a direct result of the flooding at least 40 people died. [6]

Other systems

A possible near-equatorial tropical storm on 17 January 01A Jan 17 1991 0213Z.jpg
A possible near-equatorial tropical storm on 17 January

During January 14, the JTWC started to monitor an area of convection that had developed within the near equatorial trough of low pressure, about 900 km (560 mi) to the southeast of Colombo, Sri Lanka. [3] [7] [8] Over the next couple of days the disturbance moved towards the northwest under the subtropical ridge of pressure, before early on January 17, the JTWC noticed a steady increase in deep convection and issued a Tropical Cyclone Formation Alert. [3] Later that day the JTWC initiated advisories as the disturbance had intensified into a tropical storm and designated it as Cyclone 01A. [3] [7] As the Cyclone was suffering from being in an area of strong vertical wind shear it was not able to intensify past minimal tropical storm strength of 65 km/h, (40 mph). [3] [7] During the next couple of days, strong upper-level winds stripped deep convection away from the center with the JTWC downgrading the cyclone to a tropical depression early on January 19. [3] The remaining low level circulation center slowly dissipated with the JTWC issuing their final advisory early the next day. [3]

The cyclone posed a direct threat to Coalition forces, which were operating in the Arabian Sea, Persian Gulf and the Red Sea, in the buildup to the Gulf war. [3] However it was not a significant factor in the buildup to the Gulf war and due to it low latitude track and weak intensity it had little effect on ships steaming to the Middle East. [3] As a result of the cyclone remaining out to sea, there was no reported impact on land. [3]

Season effects

NameDatesPeak intensityAreas affectedDamage
(USD)
DeathsRefs
Category Wind speedPressure
BOB 01 April 22–30Super Cyclonic Storm240 km/h (150 mph)920 hPa (27.17 inHg)India, Bangladesh, Myanmar, Yunnan$1.5 billion138,866
BOB 02May 30 – June 3Cyclonic Storm85 km/h (55 mph)990 hPa (29.23 inHg)India, BangladeshNone
BOB 03July 27–31Deep Depression55 km/h (35 mph)984 hPa (29.06 inHg)India
BOB 04August 21–26Depression45 km/h (30 mph)992 hPa (29.29 inHg)India
BOB 05September 21–22Depression45 km/h (30 mph)1,000 hPa (29.53 inHg)India
BOB 06October 12–14Depression45 km/h (30 mph)998 hPa (29.47 inHg)Bangladesh, India
BOB 07October 28–30Depression45 km/h (30 mph)998 hPa (29.47 inHg)India
BOB 08November 9–16Cyclonic Storm85 km/h (55 mph)998 hPa (29.47 inHg)IndiaMinimal40
Season aggregates
8 SystemsApril 22 – November 16240 km/h (150 mph)920 hPa (27.17 inHg)>$1.5 billion138906

See also

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References

  1. Bangladesh Cyclone, April 24–30 1991 (PDF) (Report on Cyclonic Disturbances (Depressions and Tropical Cyclones) over North Indian Ocean in 1991). India Meteorological Department. January 1992. p. 4. Archived (PDF) from the original on March 4, 2016. Retrieved January 15, 2014.
  2. 1 2 Report on Cyclonic Disturbances (Depressions and Tropical Cyclones) over North Indian Ocean in 1991 (PDF) (Report). India Meteorological Department. January 1992. pp. 5–6. Archived (PDF) from the original on March 4, 2016. Retrieved March 27, 2016.
  3. 1 2 3 4 5 6 7 8 9 10 Joint Typhoon Warning Center; Naval Western Oceanography Center. 1991 Annual Tropical Cyclone Report (PDF) (Report). United States Navy, United States Airforce. pp. 150–161. Archived (PDF) from the original on September 7, 2012. Retrieved July 11, 2012.
  4. 1 2 3 4 5 6 7 8 "IMD Best track data 1982-2022" (xls). India Meteorological Department. A guide on how to read the database is available here.
  5. The Hindu (2008-11-28). "Rain-related death toll rises to 51". The Hindu . Archived from the original on January 10, 2009. Retrieved 2010-06-08.
  6. https://news.google.com/newspapers?id=EeYdAAAAIBAJ&sjid=RCwEAAAAIBAJ&pg=5208,450731&dq=andhra+pradesh+cyclone&hl=en [ dead link ]
  7. 1 2 3 "Tropical Cyclone 01A Best Track". Joint Typhoon Warning Center. 2002-12-01. Archived from the original on 2011-06-06. Retrieved 2010-04-02.
  8. Darwin Regional Specialised Meteorological Centre (1991). "January 1991" (PDF). Darwin Tropical Diagnostic Statement. Australian Bureau of Meteorology. 10 (1): 4. ISSN   1321-4233. Archived (PDF) from the original on December 22, 2015. Retrieved August 26, 2012.