FN Archimer Export Format
PT J
TI Estimation of the vertical eddy diffusion-coefficient of heat in the gulf of trieste (northern adriatic)
BT 
AF MALACIC, V
AS 1:;
FF 1:;
IF 0.662
TC 30
UR https://archimer.ifremer.fr/doc/00101/21253/18866.pdf
LA English
DT Article
DE ;HEAT;EDDY DIFFUSION;LEAST SQUARE FITS;NORTHERN ADRIATIC
AB 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.
PY 1991
SO Oceanologica Acta
SN 0399-1784
PU Gauthier-Villars
VL 14
IS 1
UT A1991EZ66900002
BP 23
EP 32
ID 21253
ER

EF