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Digitale Medien

The sea surface temperature deviation and the heat flow at the sea-air interface (1971)

Hasse, Lutz

Springer

Boundary layer meteorology 1 (1971), S. 368-379

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Details

ISSN: 1573-1472

Quelle: Springer Online Journal Archives 1860-2000

Thema: Geologie und Paläontologie , Physik

Notizen: Abstract The deviation of the sea surface temperature from the water temperature below is calculated as a function of the heat flow through the air-sea interface, using wind tunnel determinations of the effective thermal diffusivity in a boundary layer. The influence ofQ, shortwave radiation, andH, latent and sensible heat transfer plus effective back radiation, and U, wind speed, can be described by:T 0 −T w =C 1 ·H/U +C 2 ·Q/U. The calculated coefficients vary slightly with reference depth, Tables II and III. They are in good agreement with independent observations.

Materialart: Digitale Medien

URL: http://dx.doi.org/10.1007/BF02186037

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