OH1_SW-LHF_ESRG.
3yr_Ave_WaterVap-N-Windsp.SSMI
Using satellite data for the three year period 1988 to 1990 we have estimated the two main components of the ocean surface heat fluxes (latent heat flux and solar radiation flux) . Employing SSM/I microwave data, monthly average air temperature, air moisture and wind speed are mapped onto a regular square grid with 1 degree resolution. Monthly SST values are provided by AVHRR. From these parameters Latent Heat Flux, LHF, is calculated.
The remaining two components ( sensible heat flux, SE, and longwave radiation, L) are obtained from long term shipboard-based climatologies in a first stage.
These four terms are used to determine the net oceanic heat gain, NOHG, for each grid cell by :
Net Oceanic Heat Gain = SW - LHF - SE - LW
Net Oceanic Heat Gain over the globe as well as over individual basins will be presented. Integrating NOHG zonally from north to south for the Pacific, Atlantic and Indian oceans gives the heat transport for these oceans. Preliminary meridonal heat transports will be also presented and their implications will be discussed.