The Effect of Diurnal Sea Surface Temperature Warming on Climatological Air–Sea Fluxes
Diurnal sea surface warming affects the fluxes of latent heat, sensible heat, and upwelling longwave radiation. Diurnal warming most typically reaches maximum values of 3°C, although very localized events may reach 7°–8°C. An analysis of multiple years of diurnal warming over the global ice-free oce...
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American Meteorological Society
2013
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| Mynediad Ar-lein: | http://hdl.handle.net/1721.1/81285 https://orcid.org/0000-0002-0467-3785 |