Meteorological observations at Syowa Station in 2000 by the 41st Japanese Antarctic Research Expedition

This report is a collection of results on meteorological observations performed by the 41st Japanese Antarctic Research Expedition from February 1, 2000 through January 31, 2001 at Syowa Station. The measuring instruments and means of compiling statistics were almost the same as those used on the 40...

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Main Authors: Kanji Yamaguchi, Takashi Aoyama, Juhei Sugaya, Junya Yamashita, Yoshiaki Hirano
Format: Article in Journal/Newspaper
Language:English
Japanese
Published: National Institute of Polar Research 2005
Subjects:
Online Access:https://doi.org/10.15094/00009313
https://doaj.org/article/e80a2cde7b6447abaf0e290c176c79e5
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spelling ftdoajarticles:oai:doaj.org/article:e80a2cde7b6447abaf0e290c176c79e5 2023-05-15T13:51:00+02:00 Meteorological observations at Syowa Station in 2000 by the 41st Japanese Antarctic Research Expedition Kanji Yamaguchi Takashi Aoyama Juhei Sugaya Junya Yamashita Yoshiaki Hirano 2005-03-01T00:00:00Z https://doi.org/10.15094/00009313 https://doaj.org/article/e80a2cde7b6447abaf0e290c176c79e5 EN JA eng jpn National Institute of Polar Research http://doi.org/10.15094/00009313 https://doaj.org/toc/0085-7289 https://doaj.org/toc/2432-079X doi:10.15094/00009313 0085-7289 2432-079X https://doaj.org/article/e80a2cde7b6447abaf0e290c176c79e5 Antarctic Record, Vol 49, Iss 1, Pp 67-127 (2005) Geography (General) G1-922 article 2005 ftdoajarticles https://doi.org/10.15094/00009313 2022-12-31T13:59:04Z This report is a collection of results on meteorological observations performed by the 41st Japanese Antarctic Research Expedition from February 1, 2000 through January 31, 2001 at Syowa Station. The measuring instruments and means of compiling statistics were almost the same as those used on the 40th Expedition. Remarkable weather phenomena during the wintering period are as follows.1) In surface weather observations, fine weather continued in March, the minimum monthly mean temperature, monthly lowest temperature, and maximum duration of monthly sunshine were recorded. On the other hand, cloudy weather continued in October, the maximum monthly mean cloud amount and the minimum duration of monthly sunshine were recorded.2) In upper air observations, heavy westerly wind blew above 50hPa compared to a normal year, in September and October.3) The large-scale ozone hole was observed, as in the previous year. The ozone hole disappeared on December 1; the recovery of the total amount of ozone was secondary earliest in the last 9 years.4) In observations using aerosol sondes, we observed variations of polar stratospheric clouds (PSCs), which are thought to be the most important cause of ozone holes formed in the springtime Antarctic lower stratosphere. Article in Journal/Newspaper Antarc* Antarctic Directory of Open Access Journals: DOAJ Articles Antarctic Syowa Station
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
Japanese
topic Geography (General)
G1-922
spellingShingle Geography (General)
G1-922
Kanji Yamaguchi
Takashi Aoyama
Juhei Sugaya
Junya Yamashita
Yoshiaki Hirano
Meteorological observations at Syowa Station in 2000 by the 41st Japanese Antarctic Research Expedition
topic_facet Geography (General)
G1-922
description This report is a collection of results on meteorological observations performed by the 41st Japanese Antarctic Research Expedition from February 1, 2000 through January 31, 2001 at Syowa Station. The measuring instruments and means of compiling statistics were almost the same as those used on the 40th Expedition. Remarkable weather phenomena during the wintering period are as follows.1) In surface weather observations, fine weather continued in March, the minimum monthly mean temperature, monthly lowest temperature, and maximum duration of monthly sunshine were recorded. On the other hand, cloudy weather continued in October, the maximum monthly mean cloud amount and the minimum duration of monthly sunshine were recorded.2) In upper air observations, heavy westerly wind blew above 50hPa compared to a normal year, in September and October.3) The large-scale ozone hole was observed, as in the previous year. The ozone hole disappeared on December 1; the recovery of the total amount of ozone was secondary earliest in the last 9 years.4) In observations using aerosol sondes, we observed variations of polar stratospheric clouds (PSCs), which are thought to be the most important cause of ozone holes formed in the springtime Antarctic lower stratosphere.
format Article in Journal/Newspaper
author Kanji Yamaguchi
Takashi Aoyama
Juhei Sugaya
Junya Yamashita
Yoshiaki Hirano
author_facet Kanji Yamaguchi
Takashi Aoyama
Juhei Sugaya
Junya Yamashita
Yoshiaki Hirano
author_sort Kanji Yamaguchi
title Meteorological observations at Syowa Station in 2000 by the 41st Japanese Antarctic Research Expedition
title_short Meteorological observations at Syowa Station in 2000 by the 41st Japanese Antarctic Research Expedition
title_full Meteorological observations at Syowa Station in 2000 by the 41st Japanese Antarctic Research Expedition
title_fullStr Meteorological observations at Syowa Station in 2000 by the 41st Japanese Antarctic Research Expedition
title_full_unstemmed Meteorological observations at Syowa Station in 2000 by the 41st Japanese Antarctic Research Expedition
title_sort meteorological observations at syowa station in 2000 by the 41st japanese antarctic research expedition
publisher National Institute of Polar Research
publishDate 2005
url https://doi.org/10.15094/00009313
https://doaj.org/article/e80a2cde7b6447abaf0e290c176c79e5
geographic Antarctic
Syowa Station
geographic_facet Antarctic
Syowa Station
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
op_source Antarctic Record, Vol 49, Iss 1, Pp 67-127 (2005)
op_relation http://doi.org/10.15094/00009313
https://doaj.org/toc/0085-7289
https://doaj.org/toc/2432-079X
doi:10.15094/00009313
0085-7289
2432-079X
https://doaj.org/article/e80a2cde7b6447abaf0e290c176c79e5
op_doi https://doi.org/10.15094/00009313
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