Item type |
紀要論文(ELS) / Departmental Bulletin Paper(1) |
公開日 |
1999-12-01 |
タイトル |
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タイトル |
AIRBORNE OBSERVATION OF WATER VAPOR AND AEROSOLS ALONG MIZUHO ROUTE, ANTARCTICA |
言語 |
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言語 |
eng |
資源タイプ |
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資源タイプ識別子 |
http://purl.org/coar/resource_type/c_6501 |
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資源タイプ |
departmental bulletin paper |
ID登録 |
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ID登録 |
10.15094/00002886 |
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ID登録タイプ |
JaLC |
ページ属性 |
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内容記述タイプ |
Other |
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内容記述 |
P(論文) |
記事種別(英) |
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en |
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Scientific Paper |
論文名よみ |
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その他のタイトル |
AIRBORNE OBSERVATION OF WATER VAPOR AND AEROSOLS ALONG MIZUHO ROUTE, ANTARCTICA |
著者名よみ |
ヤマノウチ, タカシ
ワダ, マコト
フカツ, トル
ハヤシ, マサヒコ
オサダ, カズオ
ナガタニ, マサヒロ
ナカダ, アキラ
イワサカ, ヤスノブ
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著者名(英) |
YAMANOUCHI, Takashi
WADA, Makoto
FUKATSU, Toru
HAYASHI, Masahiko
OSADA, Kazuo
NAGATANI, Masahiro
NAKADA, Akira
IWASAKA, Yasunobu
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著者所属(英) |
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en |
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National Institute of Polar Research |
著者所属(英) |
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en |
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National Institute of Polar Research |
著者所属(英) |
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en |
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Tokai Radio Communication Administration Office |
著者所属(英) |
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en |
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Solar-Terrestrial Environment Laboratory, Nagoya University:(Present address)Faculty of Science, Fukuoka University |
著者所属(英) |
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en |
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Solar-Terrestrial Environment Laboratory, Nagoya University |
著者所属(英) |
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en |
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Solar-Terrestrial Environment Laboratory, Nagoya University |
著者所属(英) |
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en |
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Solar-Terrestrial Environment Laboratory, Nagoya University |
著者所属(英) |
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en |
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Solar-Terrestrial Environment Laboratory, Nagoya University |
抄録(英) |
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内容記述タイプ |
Other |
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内容記述 |
Airborne observations of water vapor and aerosols using a dew point meter and optical particle counters were made along the route from Syowa Station (69°00′S, 39°35′E) to Mizuho Station (70°42′S, 44°20′E). Vertical flights were made around Syowa and Mizuho Stations, horizontal flights along the route were made at a height of 3800m a.s.l., which is the altitude of Dome Fuji Station, and return flights from Mizuho Station to Syowa Station were made along the slope at about 300-500m height from the ground snow surface. A typical result, on December 25,showed gradual increase of water vapor amount and some decreases of aerosol concentration from the coast to the inland area along the 3800m flight. On August 30,strong enhancement of aerosol loading was found in the 700 to 900hPa layer, related to the passage of a strong low pressure system. Particle size distribution was steeper in summer and flatter in winter, indicating an increase of large particles and decrease of smaller particles in winter. |
雑誌書誌ID |
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収録物識別子タイプ |
NCID |
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収録物識別子 |
AA1129795X |
書誌情報 |
Polar meteorology and glaciology
巻 13,
p. 22-37,
発行日 1999-12
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出版者 |
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出版者 |
National Institute of Polar Research |