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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National Institute of Polar Research
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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 |
_version_ |
1766254557486120960 |