Simulation of Katabatic Winds at Mizuho Station, Antarctica

A new simulation method for solving dynamic equations for stationary katabatic wind is suggested by the assumption that the turbulent exchange coefficient is a function of height and the effect of the cold sloping surface is a multinormal function of height. Calculated wind profiles agree with obser...

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Bibliographic Details
Main Author: Yimin, Ma
Format: Article in Journal/Newspaper
Language:English
Published: Polar Research Institute of China - PRIC 1992
Subjects:
Online Access:http://library.arcticportal.org/2042/
http://library.arcticportal.org/2042/1/A199201003.pdf
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Summary:A new simulation method for solving dynamic equations for stationary katabatic wind is suggested by the assumption that the turbulent exchange coefficient is a function of height and the effect of the cold sloping surface is a multinormal function of height. Calculated wind profiles agree with observational data at Mizuho Station, Antarctica.