Determination of the geostrophic drag coefficient
نویسندگان
چکیده
منابع مشابه
The Effect of Thermal Stratification and Evaporation on Geostrophic Drag Coefficient in the Atmospheric Boundary layer
The turbulent energy equation, together with a modified mixing length, is adopted to close the governing equations in the turbulent planetary boundary layer under stratification conditions. The system of governing equations is decoupled by introducing a stratification parameter, Q. Numerical integration of the system, in general, is outlined and should be easily implemented. Results for the mom...
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ژورنال
عنوان ژورنال: Tellus
سال: 1975
ISSN: 0040-2826,2153-3490
DOI: 10.3402/tellusa.v27i1.9889