Monsoonal intraseasonal oscillations in the ocean heat content over the surface layers of the Bay of Bengal
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文摘
Meridionally propagating ISO time scale signal in the heat content anomaly of the upper ocean of the Bay of Bengal. ISO time scale signal in a number of other parameters such as precipitation, winds, SST, net heat flux and river runoff. Time lag among the ISO time scale variability in the heat content anomaly of the upper ocean and other parameters. Importance of ocean heat content compared to SST on modulating the monsoon rainfall.

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