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Features of observed radar sea returns are interpreted to provide evidence of widespread small-scale wave breaking over the sea surface. These breakings can extensively disrupt aqueous thermal and diffusion sublayers, greatly modifying present formulations on air–sea exchanges of heat and mass.
Features of observed radar sea returns are interpreted to provide evidence of widespread small-scale wave breaking over the sea surface. These breakings can extensively disrupt aqueous thermal and diffusion sublayers, greatly modifying present formulations on air–sea exchanges of heat and mass.
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