1998 Gujarat cyclone

Last updated
Map key
  Tropical depression (≤38 mph, ≤62 km/h)
  Tropical storm (39–73 mph, 63–118 km/h)
  Category 1 (74–95 mph, 119–153 km/h)
  Category 2 (96–110 mph, 154–177 km/h)
  Category 3 (111–129 mph, 178–208 km/h)
  Category 4 (130–156 mph, 209–251 km/h)
  Category 5 (≥157 mph, ≥252 km/h)
  Unknown
Storm type
Disc Plain black.svg Tropical cyclone
Solid black.svg Subtropical cyclone
ArrowUp.svg Extratropical cyclone, remnant low, tropical disturbance, or monsoon depression

On June 1, an area of low pressure developed over the Laccadive Islands. Two days later, the JTWC issued a TCFA for the system as it became better organized. Early on June 4, the JTWC issued its first advisory on Tropical Cyclone 03A. [1] Around the same time, the IMD began monitoring the system as Depression ARB 02. Shortly after, the depression was upgraded to a deep depression and further strengthened into a cyclonic storm the following day. [2] The small storm moved slowly towards the west and weakened as wind shear began to increase. The storm weakened below tropical storm intensity later that day and the initial final advisory was issued. However, the system redeveloped and advisories resumed the next day. The storm gradually intensified as it moved towards the northwest. [3]

Dvorak satellite intensity estimates on June 6 reached T4.0, corresponding to an intensity of 120 km/h (75 mph). [3] The IMD also marked the increase in intensity, upgrading ARB 02 to a severe cyclonic storm. [2] Around this time, the storm began to turn towards the north and accelerate due to an approaching mid-level trough. As the storm neared the Indian coastline, an eye developed and the storm strengthened into the equivalent of a major hurricane with winds reaching 185 km/h (115 mph). [1] The IMD assessed the storm to be a very severe cyclonic storm at this time, with winds up to 165 km/h (105 mph) and a barometric pressure of 958 mbar (hPa). [2] After slightly weakening early on June 9, [3] 03A re-strengthened, attaining its peak intensity with winds of 195 km/h (120 mph). [1] Then it made landfall near Porbandar in the Indian state of Gujarat [3] between 01:00 and 02:00 UTC. [2] The storm weakened following landfall and the JTWC issued their final advisory later that day. [1] The IMD continued to monitor ARB 02 until June 10, by which time it had weakened to a depression before dissipating. [2]

Impact and aftermath

Microwave image of the cyclonic storm Lowpowerstormbeforelandfall.jpg
Microwave image of the cyclonic storm

Tropical Cyclone 03A brought a large storm surge of 4.9 m (16 ft) which devastated coastal communities and salt mines. [3] An estimated 4,000 to 10,000 people were killed by the storm, [4] [5] many of whom were salt mine workers who did not own a radio and received little or no warning of the cyclone. The large loss of life was partially attributed to contractors who wanted to continue making profits and did not inform their workers of the approaching storm. [3] According to the official figures, 1173 people died and 1774 people went missing. [5] Also, the region had witnessed only 17 cyclones since 1890, all of which were weaker than 03A. As a result, its vulnerability was miscalculated by the local population and the disaster management administration. [6] Power supply to numerous residences was lost due to the storms high winds. [7] A microwave tower in Porbandar collapsed, causing widespread disruption in telecommunication. [8] Hundreds of other power transmission towers also fell, causing an estimated loss of Rs 10 billion for the Gujarat Electricity Board. [9] At least 893 people were injured by the storm and over 11,000 animals were killed. Over 162,000 structures were damaged or destroyed throughout the affected area and damages amounted to Rs.  120 billion (US$3 billion). [10] In Kandla, the damages were estimated around 1,855.33 crore (equivalent to 84 billionorUS$1.0 billion in 2023). [5]

Over the next one month, insurance companies had lost approximately Rs. 13 billion (US$266.5 million). [9] The remnants of the storm produced heavy rains over Pakistan which electrocuted 12 people. [3] In the wake of the storm, the United States Government provided US$25,000 for rehabilitation of the affected population. [10] The Government of Denmark also contributed $72,992 in funds for relief efforts. [11] The Gujarat government deployed approximately 330 medical teams to the affected areas. Local aid, amounting to Rs 1 billion (US$20.5 million) was provided to assist victims. [12]

See also

Related Research Articles

<span class="mw-page-title-main">1992 North Indian Ocean cyclone season</span>

The 1992 North Indian Ocean cyclone season was unofficially the most active year on record for the basin, with 10 tropical storms developing, according to the Joint Typhoon Warning Center (JTWC). There are two main seas in the North Indian Ocean – the Bay of Bengal to the east of the Indian subcontinent – and the Arabian Sea to the west of India. The official Regional Specialized Meteorological Centre in this basin is the India Meteorological Department (IMD), while the JTWC releases unofficial advisories. An average of four to six storms form in the North Indian Ocean every season with peaks in May and November. Cyclones occurring between the meridians 45°E and 100°E are included in the season by the IMD.

<span class="mw-page-title-main">Timeline of the 2007 North Indian Ocean cyclone season</span>

Below is a timeline of the 2007 North Indian Ocean cyclone season, documenting major events with regards to tropical cyclone formation, strengthening, weakening, landfall, extratropical transition, as well as dissipation. The 2007 North Indian Ocean cyclone season was an ongoing event in the annual cycle of tropical cyclone formation.

<span class="mw-page-title-main">1998 North Indian Ocean cyclone season</span> Cyclone season in the North Indian ocean

The 1998 North Indian Ocean cyclone season was an active season in annual cycle of tropical cyclone formation. The season has no official bounds but cyclones tend to form between April and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. There are two main seas in the North Indian Ocean—the Bay of Bengal to the east of the Indian subcontinent and the Arabian Sea to the west of India. The official Regional Specialized Meteorological Centre in this basin is the India Meteorological Department (IMD), while the Joint Typhoon Warning Center releases unofficial advisories. An average of four to six storms form in the North Indian Ocean every season with peaks in May and November. Cyclones occurring between the meridians 45°E and 100°E are included in the season by the IMD.

<span class="mw-page-title-main">1999 North Indian Ocean cyclone season</span> Cyclone season in the North Indian ocean

The 1999 North Indian Ocean cyclone season was an event in the annual cycle of tropical cyclone formation. The North Indian Ocean cyclone season has no official bounds, but cyclones tend to form between April and December, with peaks in May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean.

<span class="mw-page-title-main">Timeline of the 2008 North Indian Ocean cyclone season</span>

The 2008 North Indian Ocean cyclone season officially ran throughout the year during 2008, with the first depression forming on April 27. The timeline includes information that was not operationally released, meaning that information from post-storm reviews by the Joint Typhoon Warning Center (JTWC), and the India Meteorological Department (IMD), such as information on a storm that was not operationally warned on. This timeline documents all the storm formations, strengthening, weakening, landfalls, extratropical transitions, as well as dissipation's during the 2008 North Indian Ocean cyclone season.

<span class="mw-page-title-main">1993 North Indian Ocean cyclone season</span> Cyclone season in the North Indian Ocean in 1993

The 1993 North Indian Ocean cyclone season was the least active on record in the basin, with only four tropical disturbances. There are two main seas in the North Indian Ocean – the Bay of Bengal to the east of the Indian subcontinent and the Arabian Sea to the west. The India Meteorological Department (IMD) issued advisories for the systems in its official capacity as the local Regional Specialized Meteorological Center, while the Joint Typhoon Warning Center also issued advisories for two of the storms on an unofficial basis. Of the five disturbances tracked by the IMD, two intensified into cyclonic storms.

<span class="mw-page-title-main">1994 North Indian Ocean cyclone season</span>

The 1994 North Indian Ocean cyclone season was a below-average year in which eight tropical cyclones affected seven countries bordering the North Indian Ocean. The India Meteorological Department tracks all tropical cyclones in the basin, north of the equator. The first system developed on March 21 in the Bay of Bengal, the first March storm in the basin since 1938. The second storm was the most powerful cyclone of the season, attaining maximum sustained winds of 215 km/h (135 mph) in the northern Bay of Bengal. Making landfall near the border of Bangladesh and Myanmar, the cyclone killed 350 people and left US$125 million in damage.

<span class="mw-page-title-main">2009 North Indian Ocean cyclone season</span> North Indian Ocean tropical cyclone season

The 2009 North Indian Ocean cyclone season was an event in the annual cycle of tropical cyclone formation. The North Indian Ocean cyclone season has no official bounds, but cyclones tend to form between April and December, with peaks in May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean.

<span class="mw-page-title-main">2011 North Indian Ocean cyclone season</span> North Indian Ocean tropical cyclone season

The 2011 North Indian Ocean cyclone season was the least active tropical cyclone season in the North Indian Ocean since 1993. Only two cyclonic storms formed, below the average of four to six. The North Indian Ocean cyclone season has no official bounds, but cyclones tend to form between April and December, with peaks in May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. The scope of this article is limited to the Indian Ocean in the Northern Hemisphere, east of the Horn of Africa and west of the Malay Peninsula. There are two main seas in the North Indian Ocean — the Arabian Sea to the west of the Indian subcontinent, abbreviated ARB by the India Meteorological Department (IMD); and the Bay of Bengal to the east, abbreviated BOB by the IMD.

<span class="mw-page-title-main">2001 Gujarat cyclone</span> North Indian cyclone in 2001

The 2001 Gujarat cyclone was the third strongest tropical cyclone, in terms of barometric pressure, to form in the Arabian Sea on record; only Cyclones Gonu in 2007 and Kyarr in 2019 were stronger. The storm originated from a tropical disturbance that formed east of Somalia 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 this turn, the storm intensified into a very severe cyclonic storm, attaining its peak intensity on May 24 with winds of 215 km/h and a barometric pressure of 932 mbar (hPa). At the time, this ranked the cyclone as the strongest known storm in the Arabian Sea.

<span class="mw-page-title-main">Cyclone Phet</span> North Indian cyclone in 2010

Very Severe Cyclonic Storm Phet was a powerful tropical cyclone that made landfall on Oman, Western India, and Pakistan. The third named cyclone of the 2010 cyclone season, Phet developed in the Arabian Sea on May 31 to the west of India. With conducive environmental conditions, the storm intensified to reach peak sustained winds of 155 km/h (95 mph) on June 2, based on analysis by the India Meteorological Department (IMD). On the next day, Phet dropped heavy rainfall while moving across eastern Oman, with a peak of 603 mm (23.7 in) in Qurayyat. The rains flooded arid areas and collected into wadis – normally dry river beds. Thousands of homes were wrecked across Oman. There were 24 fatalities in the country, and damage was estimated at US$780 million.

<span class="mw-page-title-main">Cyclone Keila</span> North Indian cyclone in 2011

Cyclonic Storm Keila was the first named storm of the 2011 North Indian Ocean cyclone season. A weak system for much of its duration, Keila developed in the western Arabian Sea in late October 2011, amid an area of marginally favorable conditions. On November 2, it briefly organized enough to be classified as a cyclonic storm, which has maximum sustained winds of at least 65 km/h (40 mph). Given the name Keila by the India Meteorological Department (IMD), the storm quickly moved ashore southern Oman near Salalah, and weakened while meandering over the country. The remnants soon after moved offshore, dissipating on November 4.

<span class="mw-page-title-main">2014 North Indian Ocean cyclone season</span> North Indian Ocean tropical cyclone season

The 2014 North Indian Ocean cyclone season was an event in the annual cycle of tropical cyclone formation. The season included two very severe cyclonic storms, both in October, and one other named cyclonic storm, classified according to the tropical cyclone intensity scale of the India Meteorological Department. Cyclone Hudhud is estimated to have caused US$3.58 billion in damage across eastern India, and more than 120 deaths.

<span class="mw-page-title-main">Deep Depression ARB 01 (2013)</span>

Deep Depression ARB 01 was the second deadliest tropical cyclone worldwide in 2013 as well as the deadliest to affect Somalia in recorded history. The sixth tropical cyclone and third deep depression of the 2013 North Indian Ocean cyclone season, ARB 01 formed in the Arabian Sea on November 8. The cyclone subsequently strengthened into a deep depression before making landfall in the Puntland region of Somalia at peak intensity on November 11. After making landfall, the cyclone rapidly weakened over land and degenerated into a well-marked low-pressure area later on the same day.

<span class="mw-page-title-main">2018 North Indian Ocean cyclone season</span> North Indian Ocean tropical cyclone season

The 2018 North Indian Ocean cyclone season was one of the most active North Indian Ocean cyclone seasons since 1992, with the formation of fourteen depressions and seven cyclones. The North Indian Ocean cyclone season has no official bounds, but cyclones tend to form between April and December, with the two peaks in May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean.

<span class="mw-page-title-main">2019 North Indian Ocean cyclone season</span> North Indian Ocean tropical cyclone season

The 2019 North Indian Ocean cyclone season was the most active North Indian Ocean cyclone season on record, in terms of cyclonic storms, however the 1992 season was more active according to the Joint Typhoon Warning Center. The season featured 12 depressions, 11 deep depressions, 8 cyclonic storms, 6 severe cyclonic storms, 6 very severe cyclonic storms, 3 extremely severe cyclonic storms, and 1 super cyclonic storm, Kyarr, the first since Cyclone Gonu in 2007. Additionally, it was also the third-costliest season recorded in the North Indian Ocean, only behind the 2020 and 2008 seasons.

<span class="mw-page-title-main">2020 North Indian Ocean cyclone season</span> North Indian Ocean tropical cyclone season

The 2020 North Indian Ocean cyclone season was the costliest North Indian Ocean cyclone season on record, mostly due to the devastating Cyclone Amphan. The North Indian Ocean cyclone season has no official bounds, but cyclones tend to form between April and November, with peaks in late April to May and October to November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. The season began on May 16 with the designation of Depression BOB 01 in the Bay of Bengal, which later became Amphan. Cyclone Amphan was the strongest storm in the Bay of Bengal in 21 years and would break Nargis of 2008's record as the costliest storm in the North Indian Ocean. The season concluded with the dissipation of Cyclone Burevi on December 5. Overall, the season was slightly above average, seeing the development of five cyclonic storms.

<span class="mw-page-title-main">Timeline of the 2015 North Indian Ocean cyclone season</span>

The 2015 North Indian Ocean cyclone season was a below-average tropical cyclone season which featured the highest number of deaths since the 2010 season. Despite inactivity in the Bay of Bengal caused by the ongoing El Niño, the season produced an above-average number of tropical cyclones in the Arabian Sea. The first storm of the season, Ashobaa, formed on 7 June, while the final storm of the season, Megh, ultimately dissipated on 10 November.

<span class="mw-page-title-main">Cyclone Luban</span> Category 2 Indian ocean cyclone in 2018

Very Severe Cyclonic Storm Luban was the third tropical cyclone to affect the Arabian Peninsula during the 2018 North Indian Ocean cyclone season, after cyclones Sagar and Mekunu in May. Luban developed on October 6 in the central Arabian Sea, and for much of its duration, maintained a general west-northwestward trajectory. On October 10, the India Meteorological Department (IMD) upgraded Luban to a very severe cyclonic storm – equivalent to a Category 1 hurricane – and estimated maximum sustained winds of 140 km/h (85 mph). The storm made landfall on October 14 in eastern Yemen, as a cyclonic storm. The storm quickly weakened over the dry, mountainous terrain of the Arabian Peninsula, before dissipating on October 15.

<span class="mw-page-title-main">2023 North Indian Ocean cyclone season</span> North Indian Ocean tropical cyclone season

The 2023 North Indian Ocean cyclone season is an ongoing event in the annual cycle of tropical cyclone formation. The North Indian Ocean cyclone season has no official bounds, but cyclones tend to form between April and December, with the peak from May to November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean.

References

  1. 1 2 3 4 Joint Typhoon Warning Center (1999). "Tropical Cyclone 03A Preliminary Report" (PDF). World Meteorological Organization. Archived from the original (PDF) on June 7, 2011. Retrieved February 9, 2009.
  2. 1 2 3 4 5 "IMD Best Tracks Data ( 1990 - 2008 )". India Meteorological Department. 2009. Archived from the original on September 27, 2013. Retrieved July 16, 2009.
  3. 1 2 3 4 5 6 7 Gary Padgett (July 14, 1998). "Monthly Tropical Cyclone Summary for June 1998". Typhoon 2000. Archived from the original on November 9, 2021. Retrieved February 9, 2009.
  4. Staff Writer (December 29, 1998). "1998 Natural Catastrophes: Top 10". Munich Re. Archived from the original on February 10, 2008. Retrieved December 8, 2015.
  5. 1 2 3 Rawat, Mukesh (2019-06-13). "Cyclone Vayu spares Gujarat: 21 yrs ago, a cyclone rained death, killed thousands in state". India Today. Archived from the original on 2021-11-09. Retrieved 2019-06-14.
  6. Zschau, Jochen; Andreas N. Küppers (2003). Early warning systems for natural disaster reduction. Springer. p. 200. ISBN   978-3-540-67962-2.
  7. Office for the Coordination of Humanitarian Affairs (June 10, 1998). "India: Cyclone Situation Report No. 1". United Nations. Archived from the original on March 16, 2005. Retrieved February 9, 2009.
  8. Office for the Coordination of Humanitarian Affairs (June 11, 1998). "India: Cyclone Situation Report No. 2". United Nations. Archived from the original on March 16, 2005. Retrieved February 9, 2009.
  9. 1 2 "Insurance companies lose Rs 1,300 crore in Gujarat cyclone". Indian Express. July 3, 1998. Archived from the original on May 28, 2009. Retrieved May 22, 2009.
  10. 1 2 Office for the Coordination of Humanitarian Affairs (June 19, 1998). "India: Cyclone Situation Report No. 4". United Nations. Archived from the original on March 16, 2005. Retrieved February 9, 2009.
  11. Office for the Coordination of Humanitarian Affairs (March 3, 1999). "India —Cyclone —June 1998 Contributions Report". ReliefWeb. Archived from the original on July 16, 2006. Retrieved May 8, 2009.
  12. Office for the Coordination of Humanitarian Affairs (June 19, 1998). "India: Cyclone Situation Report No. 4". United Nations. Archived from the original on March 16, 2005. Retrieved February 9, 2009.
Extremely Severe Cyclonic Storm ARB 02
TC Gujarat 1998.gif
The cyclone at peak intensity before landfall on the Sind-Gujarat border on June 8.