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[24] [25] Research has found that in recent decades the sea surface temperatures has risen up by 1.2–1.4 °C (2.2–2.5 °F) in the Arabian Sea. [25] During Cyclone Amphan ’s rapid intensification, sea surface temperatures were as high as 33 °C (91 °F) in the Bay of Bengal, and parts of the Arabian Sea reached 32 °C (90 °F) before the ...
This is a list of countries and sovereign states by temperature. Average yearly temperature is calculated by averaging the minimum and maximum daily temperatures in the country, averaged for the years 1991 – 2020, from World Bank Group , derived from raw gridded climatologies from the Climatic Research Unit .
The state has three distinct periods of rainfall: advanced rainfall; rainfall from the tropical cyclones emerging in the neighbourhood of the Andaman Islands during the Retreat of Monsoons(October–November): and the North-East monsoon during the months of October–December, with dominant northeast monsoon winds from the western disturbances emerging over the Bay of Bengal.
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The system crossed West Bengal's North 24 Parganas and South 24 Parganas and moved over the adjoining Bangladeshi coast on the noon of October 23 with the maximum wind speed of 45 km/h (30 mph). The system weakened into a well marked low-pressure area, 50 km north-northwest of Dhaka on the morning of October 24. [30] [31]
Sea currents are south-easterly and easterly in winter and south-westerly and westerly in summer. The average surface water temperature is 26–28 °C (79–82 °F) in February and 29 °C (84 °F) in May. The water temperature is constant at 4.8 °C (40.6 °F) at the depths of 1,600 metres (5,200 ft) and below.
Warm sea surface temperatures of 28–29 °C (82–84 °F), little dry air, and moderate wind shear allowed the system to further organize to a depression by 03:00 UTC on November 7. Throughout the next day, the depression gradually curve southwestward as it was steered by easterly and northeasterly winds in the mid and upper troposphere.
Owing to low wind shear and favorable sea surface temperatures, the storm gradually intensified into a Deep Depression on the following day. [4] Skirting off the Andaman and Nicobar Islands as a Deep Depression, BOB 06 was upgraded to a Cyclonic Storm by the IMD and JTWC, in the early hours of 8 December, and was assigned the name Vardah. [5]