Observational evidence of salt finger in the diurnal thermocline.

However, between 1000 and 1400 IST, when the ML salinity shows an increasing trend, the horizontal advection estimated from uCTD and SMAP SSS shows near-zero value in contrast to a mild positive tendency as apparent in TSG-based estimate (Fig.

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Vertical salinity profiles show a decreasing trend with depth, suggesting that the vertical processes can freshen the ML (~ − 0.03 psu day −1 ) through the entrainment of relatively low saline sub-surface water to the ML during the deepening phase of ML during the night (Figs. 4 b and 9 a).

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