Long-term seasonal inhomogeneity and recent patterns in air-sea conditions and tropical cyclone activities over the Bay of Bengal.

Further, the SHF shows a decreasing trend in both pre- and post-ISM reducing the heat flux 0.6–1 W/m 2 (Table S3).

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In the earlier period, the LHF has an increasing trend resulting 11 W/m 2 and 7 W/m 2 increase during pre- and post-ISM, respectively.

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