Temperature Fluctuations in the Lower Boundary Layer at Mizuho Station, East Antarctica

P(論文) Micrometeorological observations at Mizuho Station were carried out from February 1979 to January 1980 by the members of the 20th Japanese Antarctic Research Expedition (JARE-20), and will be continued until January 1982 by the other JARE members. Characteristic profiles of the temperature and...

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Main Authors: Wada, Makoto, Yamanouchi, Takashi, Mae, Shinji, Tsukamura, Koji
Language:English
Published: 1981
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/record/1165/files/KJ00000011691.pdf
https://nipr.repo.nii.ac.jp/records/1165
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author Wada, Makoto
Yamanouchi, Takashi
Mae, Shinji
Tsukamura, Koji
author_facet Wada, Makoto
Yamanouchi, Takashi
Mae, Shinji
Tsukamura, Koji
author_sort Wada, Makoto
collection National Institute of Polar Research Repository, Japan
description P(論文) Micrometeorological observations at Mizuho Station were carried out from February 1979 to January 1980 by the members of the 20th Japanese Antarctic Research Expedition (JARE-20), and will be continued until January 1982 by the other JARE members. Characteristic profiles of the temperature and the wind speed measured simultaniously from a 30m tower were analyzed. The temperature fluctuations at the level of 30m or 16m at Mizuho Station were observed. At that time, the wind speed at the 30m level was often not stronger than that at a lower level. Fluctuations of the temperature are classified into three types by the level where the phenomena appeared. When these phenomena were observed at Mizuho Station, the strong inversion layer between the surface and the height of 1000m which seemed to be caused by a large scale disturbance was observed at Syowa Station. When the katabatic wind was disturbed on a large scale these peculiar phenomena were observed at Mizuho Station. It seems that the difference of the three types depends on the relation between the large scale disturbance and the katabatic wind. 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
Syowa Station
Mizuho
Mizuho Station
geographic_facet Antarctic
East Antarctica
Syowa Station
Mizuho
Mizuho Station
id ftnipr:oai:nipr.repo.nii.ac.jp:00001165
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
19
17
26
AA00733561
https://nipr.repo.nii.ac.jp/record/1165/files/KJ00000011691.pdf
https://nipr.repo.nii.ac.jp/records/1165
publishDate 1981
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00001165 2025-04-13T14:10:17+00:00 Temperature Fluctuations in the Lower Boundary Layer at Mizuho Station, East Antarctica Wada, Makoto Yamanouchi, Takashi Mae, Shinji Tsukamura, Koji 1981-10 application/pdf https://nipr.repo.nii.ac.jp/record/1165/files/KJ00000011691.pdf https://nipr.repo.nii.ac.jp/records/1165 eng eng Memoirs of National Institute of Polar Research. Special issue 19 17 26 AA00733561 https://nipr.repo.nii.ac.jp/record/1165/files/KJ00000011691.pdf https://nipr.repo.nii.ac.jp/records/1165 1981 ftnipr 2025-03-19T10:19:56Z P(論文) Micrometeorological observations at Mizuho Station were carried out from February 1979 to January 1980 by the members of the 20th Japanese Antarctic Research Expedition (JARE-20), and will be continued until January 1982 by the other JARE members. Characteristic profiles of the temperature and the wind speed measured simultaniously from a 30m tower were analyzed. The temperature fluctuations at the level of 30m or 16m at Mizuho Station were observed. At that time, the wind speed at the 30m level was often not stronger than that at a lower level. Fluctuations of the temperature are classified into three types by the level where the phenomena appeared. When these phenomena were observed at Mizuho Station, the strong inversion layer between the surface and the height of 1000m which seemed to be caused by a large scale disturbance was observed at Syowa Station. When the katabatic wind was disturbed on a large scale these peculiar phenomena were observed at Mizuho Station. It seems that the difference of the three types depends on the relation between the large scale disturbance and the katabatic wind. 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 Syowa Station Mizuho ENVELOPE(44.317,44.317,-70.683,-70.683) Mizuho Station ENVELOPE(44.317,44.317,-70.683,-70.683)
spellingShingle Wada, Makoto
Yamanouchi, Takashi
Mae, Shinji
Tsukamura, Koji
Temperature Fluctuations in the Lower Boundary Layer at Mizuho Station, East Antarctica
title Temperature Fluctuations in the Lower Boundary Layer at Mizuho Station, East Antarctica
title_full Temperature Fluctuations in the Lower Boundary Layer at Mizuho Station, East Antarctica
title_fullStr Temperature Fluctuations in the Lower Boundary Layer at Mizuho Station, East Antarctica
title_full_unstemmed Temperature Fluctuations in the Lower Boundary Layer at Mizuho Station, East Antarctica
title_short Temperature Fluctuations in the Lower Boundary Layer at Mizuho Station, East Antarctica
title_sort temperature fluctuations in the lower boundary layer at mizuho station, east antarctica
url https://nipr.repo.nii.ac.jp/record/1165/files/KJ00000011691.pdf
https://nipr.repo.nii.ac.jp/records/1165