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- W2070710456 abstract "Abstract 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 layer model. The bulk parameterization method requires the inputs of sea surface temperature, cloud amount, wind speed, air temperature, and specific humidity. With the inverse mixed layer model, the authors estimate the surface net heat flux using surface wind stresses and sea surface temperature (SST) as input, assuming a linear variation of surface heat fluxes between two time intervals of known SST in a secant root-finding algorithm. The meteorological data time series from the Woods Hole Oceanography Institution buoy at 1°45′S, 156°E during the Tropical Ocean Global Atmosphere Coupled Ocean–Atmosphere Response Experiment intensive observation period is used as the test dataset. The inverse method generates large variations in daily mean heat flux estimation while the derived longer time-averaged..." @default.
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- W2070710456 date "1997-11-01" @default.
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- W2070710456 title "Surface Heat Fluxes in the Western Equatorial Pacific Ocean Estimated by Bulk Parameterization and by an Inverse Mixed Layer Model" @default.
- W2070710456 doi "https://doi.org/10.1175/1520-0485(1997)027<2477:shfitw>2.0.co;2" @default.
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