A modeling study of the effects of baroclinicity on the structure of the interacting atmospheric and oceanic boundary layers-Reference-Cited by-同舟云学术

A modeling study of the effects of baroclinicity on the structure of the interacting atmospheric and oceanic boundary layers

Published:1988 Issue:C7 Volume:93 Page:8203
ISSN:0148-0227
Container-title:Journal of Geophysical Research
language:en
Short-container-title:J. Geophys. Res.

Author:

Ly Le Ngoc,Takle Eugene S.

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Link

http://www.agu.org/journals/jc/v093/iC07/JC093iC07p08203/JC093iC07p08203.pdf

Reference43 articles.

1. Effect of baroclinicity on wind profiles and the geostrophic drag law for the convective planetary boundary layer;Arya;J. Atmos. Sci.,1975

2. On the use of exchange coefficients in modelling turbulent flow;Brown;Boundary Layer Meteorol.,1981

3. On satellite scatterometer capabilities in air-sea interaction;Brown;J. Geophys. Res.,1986

4. An operational larger-scale marine planetary boundary layer model;Brown;J. Atmos. Sci.,1982

5. The marine boundary layer, from air-sea interface to inversion;Businger,1985

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1. A numerical coupled model for studying air–sea–wave interaction;Physics of Fluids;1995-10

2. A numerical study of the influence of an air temperature-inversion layer and a seawater density-jump layer on the structure of interacting boundary layers;Boundary-Layer Meteorology;1994-02

3. An application of the E-? turbulence model for studying coupled air-sea boundary-layer structure;Boundary-Layer Meteorology;1991-03

4. Thermal advection and stratification effects on surface winds and the low level meridional mass transport;Journal of Geophysical Research;1990

5. Numerical studies of the surface-wave effects on the upper turbulent layer in the ocean;Tellus A: Dynamic Meteorology and Oceanography;1990-01