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Vertical fluxes of momentum and sensible heat have been measured above the sea surface by the direct dissipation method. Measurements were made over the open ocean from the Scripps Floating Instrument...
A direct estimate of oceanic meridional heat flux at 30°8 yields a result between +1.15 × 1015 W and +2.27 × 1015 W. The estimate is based on hydrographic data from individual cruises and climatologic...
The four components of the long-term annual mean net surface heating of the tropical Pacific Ocean between 30°N and 40°S are calculated and portrayed. These flux elements were derived by using the bul...
Monthly climatological estimates of wind stress and sea surface temperature are used to compute meridional Ekman heat fluxes in the world ocean. Qualitatively the annual cycles of the Atlantic and Pac...
There are a number of atlases that display the distribution of ocean-atmosphere sensible and latent heat fluxes over various regions. Many are based on the “classical” method, in which time mean quant...
Sea surface heat fluxes in the western equatorial Pacific Ocean estimated by bulk parameterization are compared with fluxes computed with a one-dimensional, level 2.5 turbulence closure inverse mixed ...

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