Formation mechanism of Japan Sea Proper Water in the flux center off Vladivostok
It is known that wintertime air‐sea interaction in the Japan Sea, enhanced by outbreaks of dry and cold air masses from the Eurasian continent, generates a characteristic water mass called Japan Sea Proper Water (JSPW) through deep convection. Using NASA scatterometer (NSCAT) wind vectors with high...
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Veröffentlicht in: | Journal of Geophysical Research, Washington, DC Washington, DC, 1998-09, Vol.103 (C10), p.21611-21622 |
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