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Currents and turbulent diffusion in the bottom boundary layer of the Barents Sea

✍ Scribed by V. M. Kushnir; E. Hansen; L. A. Petrenko; V. K. Pavlov; A. N. Morozov; S. V. Stanichnyi; S. V. Fedorov


Publisher
Springer
Year
2007
Tongue
English
Weight
855 KB
Volume
17
Category
Article
ISSN
0928-5105

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Diurnal variations of the vertical profiles of wind and temperature have been surveyed, and the diffusivity and the dimensionless gradient function in the atmospheric boundary layer have been estimated. Even in the middle of the atmospheric boundary layer (e.g., below a height of 442 m), the vertica