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Estimation of the vertical eddy diffusion-coefficient of heat in the gulf of trieste (northern adriatic) ArchiMer
Malacic, V.
The vertical eddy diffusion coefficient of heat has been computed from a least squares trigonometric fit of temperatures measured in the Gulf of Trieste (approximately 21 m depth), at four levels of the water column, from January 1986 to September 1989. This coefficient is supposed to be in the form of a constant plus a time and depth function. In climatological time scales, the constant coefficient is sufficient for the description of annual temperature changes in the lower part (approximately 10-21 m depth) of the water column. For the upper part of the column, the possible range of values of the coefficient for the shallow Gulf of Trieste is discussed.
Tipo: Text Palavras-chave: HEAT; EDDY DIFFUSION; LEAST SQUARE FITS; NORTHERN ADRIATIC.
Ano: 1991 URL: http://archimer.ifremer.fr/doc/00101/21253/18866.pdf
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