Titlebook: Air-Sea Exchange of Heat and Moisture During Storms; R. S. Bortkovskii,Edward C. Monahan Book 1987 Springer Science+Business Media B.V. 19

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The Transfer of Energy and Mass in the Spray-Filled Lower Marine Atmospheric Boundary Layer, the intensity of spray generation. As the vertical spray flow .. increases, it begins to play a substantial role in the transfer of momentum, heat, and moisture in the lower marine atmospheric boundary layer.

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Conclusion,acter of the energy and mass transfer during a storm. Of the various transfer mechanisms operating at the air-sea interface during a storm, we have considered in detail only one: the transfer of heat and mass by the spray, which under these conditions fills the air layer immediately above the water.

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The Role Played by Storms in Macroscale and Mesoscale Processes,ms from the mean, ‘nonstorm’ values of the sea-air temperature (Δ.) and humidity (Δ.) differences. The probability distribution of the modulus of the wind speed over the ocean has been studied repeatedly on the basis of various sets of observational data (Davidan .., 1978; Dubov, 1974; Rzheplinskii, 1972; Sorkina and Gnevko, 1968).

高度表

Book 1987sfer and moisture transfer at the sea surface, all increase with an intensification of the wind, reaching high values during a storm. This belief is based on the results of gradient and eddy correlation measurements in the air layer over the water, as weIl as on data concerning the effect of storms

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