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We will show in this monograph some possibilities of using the
potential of satellite passive microwave radiometric methods for
the analysis of variations of heat and dynamic processes in the
ocean-atmosphere interface in a wide range of time scales - from
mesometeorogical (hours, daily) to seasonal (month) and multiyear
(climatic) ones. The most essential mechanisms of
intercommunication of natural microwave radiation of the system
ocean-atmosphere (SOA) with the vertical turbulence fluxes of
sensible, latent heat, as well as the momentum at the boundary of
the SOA are studied. We will consider the turbulence heat fluxes as
the factors generated by the c- otic movements in the atmosphere,
when every small individual part of air is moved irregularly. Here,
one can observe a transfer of the energy from large-scale to sma-
scales; the average distance between the air particles is increased
with a time. Also, the potential of remote sensing the
characteristics of heat and water adv- tion and their accumulation
in the atmosphere boundary layer are demonstrated. In these
studies, we mean mainly the middle and high latitudes of the North
Atlantic, which are forming the weather conditions and climatic
trends over Europe and European territories of the Russia.
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