Numerical simulation of katabatic wind at Mizuho Station, East Antarctica

P(論文) Twenty-six pairs of vertical profiles of wind vectors and air temperatures for typical katabatic winds are chosen from about 70 aerological data of low altitude radiosondes and automatic tracking systems at Mizuho Station, East Antarctica during 1980 (as observed by S. KAWAGUCHI et al. : Mem....

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Main Authors: Adachi, Takashi, Kawaguchi, Sadao
Language:English
Published: 1984
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/record/1669/files/KJ00000012301.pdf
https://nipr.repo.nii.ac.jp/records/1669
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author Adachi, Takashi
Kawaguchi, Sadao
author_facet Adachi, Takashi
Kawaguchi, Sadao
author_sort Adachi, Takashi
collection National Institute of Polar Research Repository, Japan
description P(論文) Twenty-six pairs of vertical profiles of wind vectors and air temperatures for typical katabatic winds are chosen from about 70 aerological data of low altitude radiosondes and automatic tracking systems at Mizuho Station, East Antarctica during 1980 (as observed by S. KAWAGUCHI et al. : Mem. Natl Inst. Polar Res., Spec. Issue, 24,77,1982), and averaged after normalization using katabatic wind layer thickness, surface wind vector, and difference of potential temperature between the top of the katabatic wind layer and the surface. The wind spiral, vertical profiles of the two horizontal wind components, eddy diffusivity, friction velocity, heat flux and local Monin-Obukhov length are calculated with the numerical model of stationary katabatic winds developed by T. ADACHI (Antarct. Rec., 67,64,1979) where not only the two wind components but also eddy diffusivity are unknown. Therefore, this model is superior to the simple K-theory with a known eddy diffusivity. Numerical solutions for katabatic wind profiles agree well with the above-mentioned averaged profiles observed at Mizuho Station. departmental bulletin paper
genre Antarc*
Antarctica
East Antarctica
Memoirs of National Institute of Polar Research
Polar Research
genre_facet Antarc*
Antarctica
East Antarctica
Memoirs of National Institute of Polar Research
Polar Research
geographic East Antarctica
Mizuho
Mizuho Station
geographic_facet East Antarctica
Mizuho
Mizuho Station
id ftnipr:oai:nipr.repo.nii.ac.jp:00001669
institution Open Polar
language English
long_lat ENVELOPE(44.317,44.317,-70.683,-70.683)
ENVELOPE(44.317,44.317,-70.683,-70.683)
op_collection_id ftnipr
op_relation Memoirs of National Institute of Polar Research. Special issue
34
37
53
AA00733561
https://nipr.repo.nii.ac.jp/record/1669/files/KJ00000012301.pdf
https://nipr.repo.nii.ac.jp/records/1669
publishDate 1984
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00001669 2025-04-13T14:08:24+00:00 Numerical simulation of katabatic wind at Mizuho Station, East Antarctica Adachi, Takashi Kawaguchi, Sadao 1984-12 application/pdf https://nipr.repo.nii.ac.jp/record/1669/files/KJ00000012301.pdf https://nipr.repo.nii.ac.jp/records/1669 eng eng Memoirs of National Institute of Polar Research. Special issue 34 37 53 AA00733561 https://nipr.repo.nii.ac.jp/record/1669/files/KJ00000012301.pdf https://nipr.repo.nii.ac.jp/records/1669 1984 ftnipr 2025-03-19T10:19:57Z P(論文) Twenty-six pairs of vertical profiles of wind vectors and air temperatures for typical katabatic winds are chosen from about 70 aerological data of low altitude radiosondes and automatic tracking systems at Mizuho Station, East Antarctica during 1980 (as observed by S. KAWAGUCHI et al. : Mem. Natl Inst. Polar Res., Spec. Issue, 24,77,1982), and averaged after normalization using katabatic wind layer thickness, surface wind vector, and difference of potential temperature between the top of the katabatic wind layer and the surface. The wind spiral, vertical profiles of the two horizontal wind components, eddy diffusivity, friction velocity, heat flux and local Monin-Obukhov length are calculated with the numerical model of stationary katabatic winds developed by T. ADACHI (Antarct. Rec., 67,64,1979) where not only the two wind components but also eddy diffusivity are unknown. Therefore, this model is superior to the simple K-theory with a known eddy diffusivity. Numerical solutions for katabatic wind profiles agree well with the above-mentioned averaged profiles observed at Mizuho Station. departmental bulletin paper Other/Unknown Material Antarc* Antarctica East Antarctica Memoirs of National Institute of Polar Research Polar Research National Institute of Polar Research Repository, Japan East Antarctica Mizuho ENVELOPE(44.317,44.317,-70.683,-70.683) Mizuho Station ENVELOPE(44.317,44.317,-70.683,-70.683)
spellingShingle Adachi, Takashi
Kawaguchi, Sadao
Numerical simulation of katabatic wind at Mizuho Station, East Antarctica
title Numerical simulation of katabatic wind at Mizuho Station, East Antarctica
title_full Numerical simulation of katabatic wind at Mizuho Station, East Antarctica
title_fullStr Numerical simulation of katabatic wind at Mizuho Station, East Antarctica
title_full_unstemmed Numerical simulation of katabatic wind at Mizuho Station, East Antarctica
title_short Numerical simulation of katabatic wind at Mizuho Station, East Antarctica
title_sort numerical simulation of katabatic wind at mizuho station, east antarctica
url https://nipr.repo.nii.ac.jp/record/1669/files/KJ00000012301.pdf
https://nipr.repo.nii.ac.jp/records/1669