Changes in the thermodynamical profiles of the subsurface ocean and atmosphere induce cyclones to congregate over the Eastern Arabian Sea.

The area-averaged θ e between 500 and 1000 hPa shows an increasing trend during both MAMJ and OND seasons, as shown in Fig. 3 a.

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The recent epoch over the EAS during both seasons indicate a positive trend in the vertically averaged mid-tropospheric humidity, which is averaged between 800 and 300 hPa.

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