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During the experimental and theoretical studies of the sea surface in the infrared range, it was proved that the microbubble air layer of the sea surface discovered earlier can be used as an indicator of the magnitude of the heat flux on the border of the sea-atmosphere. The result was obtained by developing a method for the simultaneous determination of the reflection coefficients, temperature and wave state of the sea surface measuring the radiation of the sea surface and atmosphere in the infrared range in a wi...