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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spelling ftarcticportal:oai:generic.eprints.org:2042 2023-05-15T13:47:18+02:00 Simulation of Katabatic Winds at Mizuho Station, Antarctica Yimin, Ma 1992-06 application/pdf http://library.arcticportal.org/2042/ http://library.arcticportal.org/2042/1/A199201003.pdf en eng Polar Research Institute of China - PRIC http://library.arcticportal.org/2042/1/A199201003.pdf Yimin, Ma (1992) Simulation of Katabatic Winds at Mizuho Station, Antarctica. Advances is Polar Science, 3 (1). pp. 25-30. Article PeerReviewed 1992 ftarcticportal 2023-04-05T22:52:04Z 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. Article in Journal/Newspaper Antarc* Antarctica Polar Science Polar Science Arctic Portal Library Mizuho ENVELOPE(44.317,44.317,-70.683,-70.683) Mizuho Station ENVELOPE(44.317,44.317,-70.683,-70.683)
institution Open Polar
collection Arctic Portal Library
op_collection_id ftarcticportal
language English
description 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.
format Article in Journal/Newspaper
author Yimin, Ma
spellingShingle Yimin, Ma
Simulation of Katabatic Winds at Mizuho Station, Antarctica
author_facet Yimin, Ma
author_sort Yimin, Ma
title Simulation of Katabatic Winds at Mizuho Station, Antarctica
title_short Simulation of Katabatic Winds at Mizuho Station, Antarctica
title_full Simulation of Katabatic Winds at Mizuho Station, Antarctica
title_fullStr Simulation of Katabatic Winds at Mizuho Station, Antarctica
title_full_unstemmed Simulation of Katabatic Winds at Mizuho Station, Antarctica
title_sort simulation of katabatic winds at mizuho station, antarctica
publisher Polar Research Institute of China - PRIC
publishDate 1992
url http://library.arcticportal.org/2042/
http://library.arcticportal.org/2042/1/A199201003.pdf
long_lat ENVELOPE(44.317,44.317,-70.683,-70.683)
ENVELOPE(44.317,44.317,-70.683,-70.683)
geographic Mizuho
Mizuho Station
geographic_facet Mizuho
Mizuho Station
genre Antarc*
Antarctica
Polar Science
Polar Science
genre_facet Antarc*
Antarctica
Polar Science
Polar Science
op_relation http://library.arcticportal.org/2042/1/A199201003.pdf
Yimin, Ma (1992) Simulation of Katabatic Winds at Mizuho Station, Antarctica. Advances is Polar Science, 3 (1). pp. 25-30.
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