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Lei Shi, Ge Peng, and John J. Bates

-latitude sea surface air temperature (Ta) and surface specific humidity (Qa) derived from HIRS measurements. The surface temperature and humidity are key components in computing surface turbulent heat fluxes. Past studies ( Curry et al. 2004 ; Jackson et al. 2006 ) showed that a significant portion of errors for current air–sea heat flux datasets is due to uncertainties in retrieving Ta and Qa. Liu and Curry (2006) also showed that the discrepancies of the interannual variability and decadal trend of

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