Cyclone Kyarr

Last updated
Map key
Saffir–Simpson scale
  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

A low-pressure area formed on October 17 in the Arabian Sea west of India near the Lakshadweep islands. Around that time, the India Meteorological Department (IMD) anticipated that the low would eventually develop into a tropical cyclone. The low remained in the same general region for a few days, becoming well-marked by October 22. The IMD classified the system as a Depression early on October 24, upgrading it to a Deep Depression later that day. [3] On the same day, the Joint Typhoon Warning Center (JTWC) began issuing warnings on the system, classifying it as Tropical Cyclone 04A.

The Deep Depression initially moved to the northeast, towards the west coast of India. Early on October 25, the IMD upgraded the system to a Cyclonic Storm, naming it Kyarr. Later that day, the storm turned northward and intensified further into a Severe Cyclonic Storm. [3] Warm water temperatures of around 28 °C (82 °F), as well as low wind shear, fueled rapid intensification. [4] Kyarr turned to the northwest, away from India, on October 26. On the same day, the IMD upgraded the storm to a Very Severe Cyclonic Storm, and later, to an Extremely Severe Cyclonic Storm. Early on October 27, the IMD upgraded Kyarr further to a Super Cyclonic Storm, the first one in the Arabian Sea since Gonu in 2007; it was also the only recorded Super Cyclonic Storm in the Arabian Sea to occur after the monsoon season. [3] The IMD estimated the peak maximum sustained winds of 240 km/h (150 mph), with a minimum central pressure of 922 mbar (27.2 inHg) estimated by the IMD. [3] [5] The JTWC estimated slightly higher winds of 250 km/h (155 mph). [4]

At its peak, Kyarr had a well-defined eye, surrounded by well-defined rainbands and outflow. [6] For about 12 hours, Kyarr maintained peak intensity, although it remained a super cyclonic storm for about 51 hours while moving toward the Arabian Peninsula. On October 30, the storm began weakening as the track shifted to the west, falling to the intensity of a Severe Cyclonic Storm. On the same day, Kyarr co-existed with Extremely Severe Cyclonic Storm Maha, marking the first time on record that there were two simultaneous Cyclonic Storms in the Arabian Sea. Kyarr turned to the southwest, paralleling the coastline of the Arabian Peninsula offshore. On October 31, Kyarr weakened to a Deep Depression, and Kyarr deteriorated further into a Depression on the next day. The storm's circulation passed just north of Socotra on November 2. Shortly afterward, the system weakened into a remnant low off the northern coast of Somalia, before dissipating on the next day. [3]

Preparations and impact

Due to the large circulation of the cyclone, the IMD recommended all fishermen avoid sailing in the Arabian Sea for five days. The Indian Coast Guard rescued at least 19 fishermen caught by the storm. [7] The Indian Navy rescued 17 fishermen from a boat that sank amid high seas west of Mumbai. [8] On October 24, Kyarr washed ashore the chemical tanker Nu-Shi Nalini near Dona Paula in Goa state, which was carrying naphtha, an explosive. The material was salvaged about a month after the storm, and was eventually shipped in early January 2020. [9] Also offshore, the cyclone forced two AIDA cruise ships to reroute their paths. [10]

In advance of the tropical cyclone, the IMD issued rain and surf alerts for the Indian states of Maharashtra, Karnataka, and Goa. [11] As Kyarr approached western India, the cyclone dropped heavy rainfall onshore, peaking at 400 mm (16 in) in Malvan, Maharashtra. [3] In Goa, the rains caused flash flooding, while strong winds felled trees and power lines. [11] In Mumbai, the storm's heavy rains contributed to a dengue outbreak, with a 70% increase in cases of the mosquito-borne disease in December 2019 compared to the same month in 2018. [12] In Gujarat, more than 157,000 farmers filed insurance claims due to damage related to Kyarr, with most of the losses related to groundnut and cotton. The state government reimbursed farmers for their losses. [13] [14] 5 people killed from rain-related incidents in Karnataka, India. [2]

In southern Pakistan, officials closed beaches and opened four shelters due to high tides from the cyclone. Floods affected parts of Karachi, closing a section of Defence Raya Golf and Country Club, killing 200, and damaging 2000 houses. [15]

High tides from Kyarr flooded towns on the coast of Oman. [16] In neighboring United Arab Emirates, high tides flooded streets, houses, and schools in eastern coastal areas of Sharjah and Fujairah. [17] Heavy rainfall from the outskirts of Kyarr also caused flooding in Dubai. [10]

Kyarr started to slow down as it moved through the Arabian Sea, and it dissipated before reaching Socotra Island. [18] [19]

See also

Notes

  1. ↑ The word "Kyarr" means "tiger" in Burmese.

Related Research Articles

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

In the Indian Ocean north of the equator, tropical cyclones can form throughout the year on either side of the Indian subcontinent, although most frequently between April and June, and between October and December.

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

The 2007 North Indian Ocean cyclone season was one of the most active North Indian Ocean cyclone seasons on record. 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">Cyclone Gonu</span> North Indian Ocean super cyclonic storm in 2007

Super Cyclonic Storm Gonu was an extremely powerful tropical cyclone that became the strongest cyclone on record in the Arabian Sea. The second named tropical cyclone of the 2007 North Indian Ocean cyclone season, Gonu developed from a persistent area of convection in the eastern Arabian Sea on June 1, 2007. With a favorable upper-level environment and warm sea surface temperatures, it rapidly intensified to attain peak winds of 240 km/h (150 mph) on June 4, according to the India Meteorological Department. Gonu weakened after encountering dry air and cooler waters, and early on June 6, it made landfall on the easternmost tip of Oman, becoming the strongest tropical cyclone to hit the Arabian Peninsula. It then turned northward into the Gulf of Oman, and dissipated on June 7, after making landfall in southern Iran, the first landfall in the country since 1898.

<span class="mw-page-title-main">2004 North Indian Ocean cyclone season</span>

The 2004 North Indian Ocean cyclone season was the first in which tropical cyclones were officially named in the basin. Cyclone Onil, which struck India and Pakistan, was named in late September. The final storm, Cyclone Agni, was also named, and crossed into the southern hemisphere shortly before dissipation. This storm became notable during its origins and became one of the storms closest to the equator. The season was fairly active, with ten depressions forming from May to November. The India Meteorological Department designated four of these as cyclonic storms, which have maximum sustained winds of at least 65 km/h (40 mph) averaged over three minutes. The Joint Typhoon Warning Center also issued warnings for five of the storms on an unofficial basis.

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

The 2001 North Indian Ocean cyclone season was fairly quiet, although activity was evenly spread between the Arabian Sea and the Bay of Bengal. There were six depressions tracked by the India Meteorological Department (IMD), which is the official Regional Specialized Meteorological Center for the northern Indian Ocean. The agency also tracked four cyclonic storms, which have maximum winds of at least 65 km/h (40 mph) sustained over 3 minutes. The American-based Joint Typhoon Warning Center (JTWC) tracked an additional storm – Tropical Storm Vamei – which crossed over from the South China Sea at a record-low latitude.

<span class="mw-page-title-main">Cyclone Phyan</span>

Cyclonic Storm Phyan developed as a tropical disturbance to the southwest of Colombo in Sri Lanka on November 4, 2009. Over the next couple of days, the disturbance gradually developed before weakening as it made landfall on Southern India on November 7. After the disturbance emerged into the Arabian Sea, it rapidly became more of a concern to the India Meteorological Department (IMD) reporting early on November 9 that the disturbance had intensified into a Depression, and designated it as Depression ARB 03 whilst the Joint Typhoon Warning Center (JTWC) issued a Tropical Cyclone Formation Alert. Later that day, the JTWC designated the system as Cyclone 04A. During the next day, the Depression turned towards the northeast the IMD reported that it had intensified into a Cyclonic Storm and named it as Phyan.

<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">Tropical cyclones in India</span>

India is a country in the north of Indian Ocean that is the most vulnerable to getting hit by tropical cyclones in the basin, from the east or from the west. On average, 2–3 tropical cyclones make landfall in India each year, with about one being a severe tropical cyclone or greater.

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

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">Cyclone Nilofar</span> North Indian cyclone in 2014

Extremely Severe Cyclonic Storm Nilofar was, at the time, the third-strongest cyclone in the Arabian Sea. In late October 2014, it reached peak maximum sustained winds estimated between 205 km/h (125 mph) and 215 km/h (130 mph). The India Meteorological Department (IMD) named it Nilofar; the name refers to the water lily, and was suggested by Pakistan. The western fringes of the storm caused flash flooding in northeastern Oman, killing four people.

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

The 2015 North Indian Ocean cyclone season was an event in the annual cycle of tropical cyclone formation. It was an average season with 4 cyclonic storms. The North Indian Ocean cyclone season has no official bounds, but cyclones tend to form between months of 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.

<span class="mw-page-title-main">Cyclone Chapala</span> North Indian cyclone in 2015

Extremely Severe Cyclonic Storm Chapala was a powerful tropical cyclone that caused moderate damage in Somalia and Yemen during November 2015. Chapala was the third named storm of the 2015 North Indian Ocean cyclone season. It developed as a depression on 28 October off western India, and strengthened a day later into a cyclonic storm. Chapala then rapidly intensified amid favorable conditions. On 30 October, the India Meteorological Department (IMD) estimated that Chapala attained peak three-minute sustained winds of 215 km/h (135 mph). The American-based Joint Typhoon Warning Center (JTWC) estimated sustained winds of 240 km/h (150 mph), making Chapala among the strongest cyclones on record in the Arabian Sea. After peak intensity, Chapala skirted the Yemeni island of Socotra on 1 November, becoming the first hurricane-force storm there since 1922. High winds and heavy rainfall resulted in an island-wide power outage, and severe damage was compounded by Cyclone Megh, which struck Yemen a week later.

<span class="mw-page-title-main">October 1996 India cyclone</span> North Indian Ocean cyclone in 1996

The October 1996 India cyclone had an unusual and protracted path that spanned much of the northern Indian Ocean. It originated in a weather disturbance that formed on October 14 in the southern Bay of Bengal, off India's east coast. Moving westward, it struck Andhra Pradesh on October 17 as a well-defined low-pressure area. It crossed southern India and reorganized in the Arabian Sea off the western coast of India. The system developed into a depression on October 22 and quickly intensified while moving northward. By October 24, the cyclone approached hurricane intensity as it developed an eye, reaching peak winds of at least 110 km/h (70 mph). On October 25, the storm abruptly stalled and weakened off Gujarat, and progressed southwestward as a minimal storm. It was no longer classifiable as a tropical cyclone by October 28, although its remnants persisted until November 2 when they dissipated east of Somalia.

<span class="mw-page-title-main">2016 North Indian Ocean cyclone season</span>

The 2016 North Indian Ocean cyclone season was an event in the annual cycle of tropical cyclone formation. It was the deadliest season since 2010, killing more than 400 people. The season was an average one, seeing four named storms, with one further intensifying into a very severe cyclonic storm. The first named storm, Roanu, developed on 19 May while the season's last named storm, Vardah, dissipated on 18 December. 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">2018 North Indian Ocean cyclone season</span>

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>

The 2019 North Indian Ocean cyclone season was the second most active North Indian Ocean cyclone season on record in terms of cyclonic storms, 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 also became 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>

The 2020 North Indian Ocean cyclone season was the costliest North Indian Ocean cyclone season on record, mostly due to the devastating Cyclone Amphan. it was an above average season featuring 5 cyclonic storms. 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 Mekunu</span> Category 3 North Indian Cyclone in 2018

Extremely Severe Cyclonic Storm Mekunu was the strongest storm to strike Oman's Dhofar Governorate since 1959. The second named storm of the 2018 North Indian Ocean cyclone season, Mekunu developed out of a low-pressure area on May 21. It gradually intensified, passing east of Socotra on May 23 as a very intense tropical cyclone. On May 25, Mekunu reached its peak intensity. The India Meteorological Department estimated 10 minute sustained winds of 175 km/h (110 mph), making Mekunu an extremely severe cyclonic storm. The American-based Joint Typhoon Warning Center estimated slightly higher 1 minute winds of 185 km/h (115 mph). While at peak intensity, Mekunu made landfall near Raysut, Oman, on May 25. The storm rapidly weakened over land, dissipating on May 27.

References

  1. ↑ Cappucci, Matthew (28 October 2019). "Category 5 Kyarr is the strongest cyclone over the Arabian Sea in 12 years". The Washington Post. Archived from the original on 28 October 2019. Retrieved 28 October 2019.
  2. 1 2 Bureau, Karnataka (2019-10-26). "Cyclone Kyarr: Five killed in rain-related incidents in Karnataka". The Hindu. ISSN   0971-751X . Retrieved 2021-01-20.{{cite news}}: |last= has generic name (help)
  3. 1 2 3 4 5 6 Super Cyclonic Storm 'Kyarr' over the Arabian Sea (24th October – 02nd November 2019): Summary (PDF) (Report). India Meteorological Department. Retrieved June 6, 2020.
  4. 1 2 Bob Henson. "Kyarr Nears Cat 5 Strength in Arabian Sea; Pablo a Hurricane; California Faces Hellish Sunday of Fire" . Retrieved June 6, 2020.
  5. ↑ "04A Kyarr Track File" (TXT). Joint Typhoon Warning Center. Retrieved June 6, 2020.
  6. ↑ Matthew Cappucci (October 28, 2019). "Category 4 Kyarr is the strongest cyclone over the Arabian Sea in 12 years". The Washington Post. Retrieved June 6, 2020.
  7. ↑ "Cyclone Kyarr intensifies to super cyclonic storm, Coast Guard on alert". The Hindustan Times. October 27, 2019. Retrieved June 6, 2020.
  8. ↑ "Cyclone Kyarr: Navy Rescues 17 Fishermen From Sinking Boat Near Mumbai". All India. October 27, 2019. Archived from the original on October 29, 2019. Retrieved October 29, 2019.
  9. ↑ "2,400 tonnes of naphtha taken out of Goa, shipped to Gulf". Times of India. January 1, 2020.
  10. 1 2 "Unstable weather causes itinerary changes for UK cruise ship in Dubai". Middle East Logistics. November 17, 2019. Retrieved June 11, 2020.
  11. 1 2 "Cyclone Kyarr, Weather forecast today LIVE Updates: Super cyclone moves towards Oman coast". The Indian Express. 2019-10-28. Archived from the original on 2019-10-28. Retrieved 2019-10-28.
  12. ↑ "Seasonal sting in the tail; Protracted rains led to rise in dengue, dengue-like illnesses Health experts". The Free Press Journal. January 8, 2020. Yahoo! News. Retrieved June 11, 2020.
  13. ↑ "Gujarat: Over 1.57 lakh farmers claim insurance after October's unseasonal rain damaged crops". The Indian Express. November 7, 2019. Retrieved June 12, 2020.
  14. ↑ "Vijay Rupani: Will compensate farmers for crop loss". 8 November 2019.
  15. ↑ "Coastal areas flooded as cyclone Kyarr intensifies". October 29, 2019. Archived from the original on October 29, 2019. Retrieved October 29, 2019.
  16. ↑ "Cyclone Kyarr: Oman feet-deep in flood water with more on the way". Archived from the original on 2019-10-29. Retrieved 2019-10-29.
  17. ↑ "UAE roads closed: 'Unusually high tide, flooding' as Cyclone Kyarr kicks up waves". Archived from the original on 2019-10-29. Retrieved 2019-10-29.
  18. ↑ "Kyarr 2019 – Hurricane And Typhoon Updates". blogs.nasa.gov. Archived from the original on 2020-02-20. Retrieved 2020-02-20.
  19. ↑ "TROPICAL CYCLONE KYARR Tracker | Cyclocane". www.cyclocane.com. Archived from the original on 2019-11-22. Retrieved 2020-02-20.
Super Cyclonic Storm Kyarr
Kyarr 2019-10-27 0900Z.jpg
Kyarr near peak intensity on October 27
Tropical cyclones of the 2019 North Indian Ocean cyclone season
2019 North Indian Ocean cyclone season summary.png
CS
Pabuk
ESCS
Fani
VSCS
Vayu
DD
BOB 03
VSCS
Hikaa
D
LAND 01
SUCS
Kyarr
ESCS
Maha
VSCS
Bulbul
CS
Pawan
DD
ARB 06
DD
ARB 08
This page is based on this Wikipedia article
Text is available under the CC BY-SA 4.0 license; additional terms may apply.
Images, videos and audio are available under their respective licenses.