Abstract
The possibility of reconstruction of the bulk aerodynamic formulas used for computation of heat fluxes over the ocean in the form of combinations of parameters of heat and moisture exchange in the SOA interface at the synoptic scales is discussed. Here, only such parameters of the SOA are taken into account, that are directly related to characteristics of natural MCW radiation measured from satellites. Possibility of assimilation of the atmospheric water vapor in bulk-formulas, which is closely related to the near-surface air temperature in the synoptic range of time scales and humidity, is discussed. The role of the near-surface wind speed on the heat flux determination accuracy is studied. Possibilities of using the brightness and infrared temperatures as the direct characteristics of seasonal and annual heat flux variability are considered also.
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Grankov, A.G., Milshin, A.A. (2016). Search for the Direct Relationship Between Heat Fluxes and the Parameters Associated with the SOA Brightness Temperature. In: Microwave Radiation of the Ocean-Atmosphere. Springer, Cham. https://doi.org/10.1007/978-3-319-21647-8_3
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