Cyclone Ockhi

Very Severe Cyclonic Storm Ockhi
Very severe cyclonic storm (IMD scale)
Category 3 (Saffir–Simpson scale)
Ockhi 2017-12-02 Suomi NPP.jpg
Cyclone Ockhi at its peak intensity in the Arabian Sea, west of India on December 2
Formed 29 November 2017
Dissipated 6 December 2017
Highest winds 3-minute sustained: 155 km/h (95 mph)
1-minute sustained: 185 km/h (115 mph)
Lowest pressure 976 hPa ( mbar); 28.82 inHg
Fatalities 74 direct, 97 missing
Damage > $442 million (2017 USD)
Areas affected Sri Lanka, South India and Maldives
Part of the 2017 North Indian Ocean cyclone season

Cyclone Ockhi [nb 1] was the most intense tropical cyclone in the Arabian Sea since Cyclone Megh in 2015. The third and the strongest storm of the 2017 North Indian Ocean cyclone season, Ockhi originated as a low pressure area in the Gulf of Thailand on 21 November. [2] While traversing the southern part of the Bay of Bengal, favorable conditions enabled it to consolidate into a deep depression. As a deep depression, it caused damage to property and life in Sri Lanka on 29 November. [2] Due to moisture and warmer temperatures between Sri Lanka and Kanyakumari ( Cape Comorin) in mainland India, it intensified into a Cyclonic Storm on 30 November. [2]

While near Kanyakumari in mainland India, Cyclone Ockhi changed its path and headed towards Lakshadweep in the Arabian Sea, while intensifying. [3] Although it headed away from the coast of mainland India, it caused severe damages to structures and property and also claiming the lives of at least 47 people [4]in the Southern parts of Tamilnadu and Kerala in India. [5] [2] Ockhi caused landfalls in Lakshadweep on 2 December. The cyclone uprooted coconut trees and caused extensive damages to houses, power lines and other infrastructure in the islands. [6] Ockhi dissipated near the south coast of Gujarat in India on December 6, due to prevailing conditions, even before entering the coast. [7]

Cyclone Ockhi is noted for its very unusual course, originating in the Gulf of Thailand and ending near the coast of Gujarat in western India, traveling nearly 4000 nautical miles. [2] In its entire course, Cyclone Ockhi left a trail of massive destruction in Sri Lanka, Lakshadweep, South India and Maldives as it strengthened from a depression to a mature cyclone. Though it rapidly weakened in its final stages over the Arabian sea, it caused heavy rains along the western coast of India, particularly in Maharashtra and Gujarat. More than 39 fatalities were caused by Ockhi in India, and it left hundreds of people, mainly fishermen, missing.

Meteorological history

Map plotting the track and intensity of the storm, according to the Saffir–Simpson scale

On 20 November 2017, the remnant energy of Tropical Storm Kirogi led to the formation of a new low-pressure area over the Gulf of Thailand. [8] Over the next several days, the system moved into the Bay of Bengal and slowly drifted westwards, but the storm was unable to organize significantly due to unfavorable conditions. [8] On 29 November, the storm organized into depression just off the southeastern coast of Sri Lanka, and the India Meteorological Department gave the storm the identifier BOB 07. [9] Due to the storm's rapidly consolidating low level circulation center, the Joint Typhoon Warning Center issued a Tropical Cyclone Formation Alert on the system, shortly before classifying it as Tropical Cyclone 03B on 29 November. [10] The IMD followed suit, upgrading the storm to a Deep Depression, and soon afterwards to Cyclonic Storm Ockhi. The storm tracked along Sri Lanka's southwestern and western coastline, towards the west-northwest, around the southern verge of a subtropical ridge located over India. [11] Owing to highly favorable conditions, the storm displayed a thick convective ring, surrounding a well-defined eye feature on the same day. [12] The storm tracked westwards and intensified further into a Severe Cyclone Storm, early on 1 December. [13] Soon afterwards, Ockhi intensified further into a Very Severe Cyclonic Storm. [14]

Cyclone Ockhi rapidly undergoing extratropical transition off the southwest coast of Gujarat.

As Ockhi moved further into the Arabian Sea, it travel through an area of sea surface temperatures of 31° C (89° F) and decreasing wind shear; a 23 mi (37 km) eye became visible on satellite imagery, prompting the JTWC to upgrade it to a Category 3-equivalent cyclone early on 2 December. [15] On 4 December, analysis showed that Ockhi was maintaining a source aloft, but there was restricted outflow on the western edge, due to a deepening trough advancing rapidly from the west. [16] Increasing vertical wind shear along with a deep layered subtropical ridge to the east steered it to north-northeast, and dry air intrusion from the west gradually weakened the system. [17] On the following day, the storm quickly became disorganized as it encountered increasingly unfavorable conditions, including high wind shear. As Ockhi became embedded within a deep mid-latitude trough, the storm rapidly underwent an extratropical transition. [18] Dry and cold air from the subcontinent rapidly weakened the storm, and it was last noted as a well-marked low-pressure area over the Gulf of Cambay on 6 December. [19]

Other Languages
čeština: Cyklón Ockhi
Bahasa Melayu: Siklon Ockhi
தமிழ்: ஒகி புயல்
українська: Циклон Оцхі (2017)