A GREAT WARMING IN THE WESTERN NORTH PACIFIC BY A …
The latent heat flux Qlat is dependent on the wind speed w, the specific humidity difference (q (saturated specific humidity at the sea surface qs minus specific humidity of air qa), and the transfer coefficient for latent heat CE, while the sensible heat flux Qsen is dependent on the wind speed, the temperature difference (T (SST minus air ... ................
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