The plume layer (0-15 m, marked out by 2-3°C isotherm, 22-24 psu isohaline) was isolated from the bottom water with a well-pronounced thermocline and halocline. At a distance of 180-300 km from the ...

In particular, we show that the winter ventilation of the halocline in the eastern Eurasian Basin resulted in more than twofold rate in sea-ice loss caused by oceanic heat fluxes as compared to ...

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These downwelling Rossby waves deepened the thermocline by more than 60 m and caused anomalous surface warming, thereby contributing to the occurrences of MHWs. With the development and peak of the ...

Ceol Tacsi. Vertical Records. 9.