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The Andaman Sea (historically also known as the Burma Sea) [4] is a marginal sea of the northeastern Indian Ocean bounded by the coastlines of Myanmar and Thailand along the Gulf of Martaban and the west side of the Malay Peninsula, and separated from the Bay of Bengal to its west by the Andaman Islands and the Nicobar Islands.
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Most of these storms form in the Bay of Bengal: either in the southeastern Bay of Bengal, in the Andaman Sea, or as a remnant of a typhoon from the South China Sea, and a few in the Arabian Sea. [8] High sea surface temperatures and humidity makes the bays more favourable to tropical cyclone development. [16]
The Malay Peninsula [a] is located in Mainland Southeast Asia. The landmass runs approximately north–south, and at its terminus, it is the southernmost point of the Asian continental mainland. The area contains Peninsular Malaysia , Southern Thailand , and the southernmost tip of Myanmar ( Kawthaung ).
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[153] [154] Two days later, at 12:00 UTC (17:30 IST) on November 30, the system crossed into the Andaman Sea, and the IMD started to monitor the system as a low-pressure area. [155] On December 2, at 00:00 UTC (05:30 IST), the system further intensified into a well-marked low-pressure area, as the department found that the storm's thunderstorms ...
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The system then crossed over Southern Thailand and the Malay Peninsula, moving westward into the Andaman Sea. Under conditions favourable for strengthening, the weak system intensified into a depression over the Bay of Bengal on 10 November and further intensified into a cyclonic storm early on 11 November, being named Gaja.