Observations of an atmospheric gravity wave by shear instability in katabatic wind at Mizuho Station, East Antarctica

P(論文) Measurements were made of vertical wind speed components, using two sonic anemothermometers on the snow surface at Mizuho Station in 1980 by the present authors who were members of the 21st Japanese Antarctic Research Expedition (JARE-21). The two anemothermometers were mounted at the fixed he...

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Main Authors: Kobayashi, Shun'ichi, Ishikawa, Nobuyoshi, Ohata, Tetsuo, Kawaguchi, Sadao
Language:English
Published: 1982
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/record/1329/files/KJ00000011963.pdf
https://nipr.repo.nii.ac.jp/records/1329
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author Kobayashi, Shun'ichi
Ishikawa, Nobuyoshi
Ohata, Tetsuo
Kawaguchi, Sadao
author_facet Kobayashi, Shun'ichi
Ishikawa, Nobuyoshi
Ohata, Tetsuo
Kawaguchi, Sadao
author_sort Kobayashi, Shun'ichi
collection National Institute of Polar Research Repository, Japan
description P(論文) Measurements were made of vertical wind speed components, using two sonic anemothermometers on the snow surface at Mizuho Station in 1980 by the present authors who were members of the 21st Japanese Antarctic Research Expedition (JARE-21). The two anemothermometers were mounted at the fixed heights of 3m and 30m on a 30-m-high micrometeorological tower. The existence of shear instability (Kelvin-Helmholtz) waves with period of about 20s was revealed as a result. The maximum aplitude of the K-H waves was found when the surface layer had a local gradient Richardson number smaller than 0.25; the instability regime was in agreement with DRAZIN's criterion (J. Fluid. Mech., 4,214,1958). Such gravity waves were observed when a strong surface inversion was progressing above the snow surface after the katabatic wind had been disturbed by a synoptic scale disturbance. departmental bulletin paper
genre Antarc*
Antarctic
Antarctica
East Antarctica
Memoirs of National Institute of Polar Research
Polar Research
genre_facet Antarc*
Antarctic
Antarctica
East Antarctica
Memoirs of National Institute of Polar Research
Polar Research
geographic Antarctic
East Antarctica
Mizuho
Mizuho Station
Tower The
geographic_facet Antarctic
East Antarctica
Mizuho
Mizuho Station
Tower The
id ftnipr:oai:nipr.repo.nii.ac.jp:00001329
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)
ENVELOPE(-58.479,-58.479,-62.215,-62.215)
op_collection_id ftnipr
op_relation Memoirs of National Institute of Polar Research. Special issue
24
46
56
AA00733561
https://nipr.repo.nii.ac.jp/record/1329/files/KJ00000011963.pdf
https://nipr.repo.nii.ac.jp/records/1329
publishDate 1982
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00001329 2025-04-13T14:10:33+00:00 Observations of an atmospheric gravity wave by shear instability in katabatic wind at Mizuho Station, East Antarctica Kobayashi, Shun'ichi Ishikawa, Nobuyoshi Ohata, Tetsuo Kawaguchi, Sadao 1982-12 application/pdf https://nipr.repo.nii.ac.jp/record/1329/files/KJ00000011963.pdf https://nipr.repo.nii.ac.jp/records/1329 eng eng Memoirs of National Institute of Polar Research. Special issue 24 46 56 AA00733561 https://nipr.repo.nii.ac.jp/record/1329/files/KJ00000011963.pdf https://nipr.repo.nii.ac.jp/records/1329 1982 ftnipr 2025-03-19T10:19:57Z P(論文) Measurements were made of vertical wind speed components, using two sonic anemothermometers on the snow surface at Mizuho Station in 1980 by the present authors who were members of the 21st Japanese Antarctic Research Expedition (JARE-21). The two anemothermometers were mounted at the fixed heights of 3m and 30m on a 30-m-high micrometeorological tower. The existence of shear instability (Kelvin-Helmholtz) waves with period of about 20s was revealed as a result. The maximum aplitude of the K-H waves was found when the surface layer had a local gradient Richardson number smaller than 0.25; the instability regime was in agreement with DRAZIN's criterion (J. Fluid. Mech., 4,214,1958). Such gravity waves were observed when a strong surface inversion was progressing above the snow surface after the katabatic wind had been disturbed by a synoptic scale disturbance. departmental bulletin paper Other/Unknown Material Antarc* Antarctic Antarctica East Antarctica Memoirs of National Institute of Polar Research Polar Research National Institute of Polar Research Repository, Japan Antarctic East Antarctica Mizuho ENVELOPE(44.317,44.317,-70.683,-70.683) Mizuho Station ENVELOPE(44.317,44.317,-70.683,-70.683) Tower The ENVELOPE(-58.479,-58.479,-62.215,-62.215)
spellingShingle Kobayashi, Shun'ichi
Ishikawa, Nobuyoshi
Ohata, Tetsuo
Kawaguchi, Sadao
Observations of an atmospheric gravity wave by shear instability in katabatic wind at Mizuho Station, East Antarctica
title Observations of an atmospheric gravity wave by shear instability in katabatic wind at Mizuho Station, East Antarctica
title_full Observations of an atmospheric gravity wave by shear instability in katabatic wind at Mizuho Station, East Antarctica
title_fullStr Observations of an atmospheric gravity wave by shear instability in katabatic wind at Mizuho Station, East Antarctica
title_full_unstemmed Observations of an atmospheric gravity wave by shear instability in katabatic wind at Mizuho Station, East Antarctica
title_short Observations of an atmospheric gravity wave by shear instability in katabatic wind at Mizuho Station, East Antarctica
title_sort observations of an atmospheric gravity wave by shear instability in katabatic wind at mizuho station, east antarctica
url https://nipr.repo.nii.ac.jp/record/1329/files/KJ00000011963.pdf
https://nipr.repo.nii.ac.jp/records/1329