Supported by the National Basic Research Program of China(973 Program)(No.2013CB430304);the National Natural Science Foundation of China(Nos.41030854,41106005,41176003,41206178,41376015,41376013,41306006);the National High-Tech R&D Program of China(No.2013AA09A505);the Public Science and Technology Research Funds Projects of Ocean(No.20130531-8)
At the interface between the lower atmosphere and sea surface,sea spray might significantly influence air-sea heat fluxes and subsequently,modulate upper ocean temperature during a typhoon passage. The effects of sea ...
Supported by the National Basic Research Program of China(973 Program)(No.2013CB430304);the National Natural Science Foundation of China(Nos.41030854,41106005,41176003,41206178,41376015,41376013,41306006);the National High-Tech R&D Program of China(No.2013AA09A505)
Upper ocean heat content is a factor critical to the intensity change of tropical cyclones(TCs). Because of the inhomogeneity of in situ observations in the North Indian Ocean,gridded temperature/salinity(T/S) profile...
Supported by the National Basic Research Program(973Program)(Nos.2007CB816001,2005CB422302,2005CB422307and2007CB411806);the National Natural Science Foundation of China(Nos.41030854,40776016,40906015,and40906016);the Major Project of National Natural Science Foundation of China(Nos.40490263,40976005);the Research Project of National Marine Data and Information Service(No.29106006C)
We investigated the Stokes drift-driven ocean currents and Stokes drift-induced wind energy input into the upper ocean using a two-way coupled wave-current modeling system that consists of the Princeton Ocean Model ge...