A simplified model for the transformation of the atmospheric planetary boundary layer overlying a thermal front in the sea

Author:

Kudryavtsev V. N.

Publisher

Springer Science and Business Media LLC

Subject

Fluid Flow and Transfer Processes,Ocean Engineering,Water Science and Technology,Oceanography,General Earth and Planetary Sciences,Fluid Flow and Transfer Processes,General Environmental Science,Ocean Engineering,Water Science and Technology,Oceanography

Reference21 articles.

1. Mitnik, L.M., Bulatov, N.V. and Lobanov, V.B. Synoptic eddies in the ocean as observed by satellite-mounted radars.Dokl. Akad. Nauk SSSR (1989)307, 454–456.

2. Beal, R., Kudryavtsev, V., Tompson, D., Grodsky, S., Tilley, D.G. and Dulov, V. Interpretation of ERS-1 SAR imagery of the Gulf Stream using near-surface measurements from the R/VAkademik Vernadsky. J. Geophys. Res. (in press).

3. Weismann, D.E., Tompson, T.W. and Legeckis, R. Modulation of sea surface radar cross-section by surface stress: wind speed and temperature effects across the Gulf Stream.J. Geophys. Res. (1980)85, 5032–5042.

4. Donelan, M.A. and Pierson, W.J. Radar scattering and equilibrium ranges in wind-generated waves with applications to scatterometry.J. Geophys. Res. (1987)92, 4971–5029.

5. Garrat, G.R. The internal boundary layer. Review.Boundary-Layer Meteorol. (1990)50, 171–203.

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