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A PROPOSAL FOR OBSERVATION OF ATMOSPHERIC CIRCULATION AND TRANSPORT PROCESSES IN THE TROPOSPHERE AND LOWER STRATOSPHERE OVER ANTARCTICA WITH A NETWORK OF WIND PROFILERS
https://doi.org/10.15094/00003696
https://doi.org/10.15094/000036967c438647-ac40-4546-be9a-089cce5a0bd0
名前 / ファイル | ライセンス | アクション |
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KJ00002409925 (1.4 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1992-02-01 | |||||
タイトル | ||||||
タイトル | A PROPOSAL FOR OBSERVATION OF ATMOSPHERIC CIRCULATION AND TRANSPORT PROCESSES IN THE TROPOSPHERE AND LOWER STRATOSPHERE OVER ANTARCTICA WITH A NETWORK OF WIND PROFILERS | |||||
言語 | ||||||
言語 | eng | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
資源タイプ | departmental bulletin paper | |||||
ID登録 | ||||||
ID登録 | 10.15094/00003696 | |||||
ID登録タイプ | JaLC | |||||
ページ属性 | ||||||
内容記述タイプ | Other | |||||
内容記述 | P(論文) | |||||
論文名よみ | ||||||
その他のタイトル | A PROPOSAL FOR OBSERVATION OF ATMOSPHERIC CIRCULATION AND TRANSPORT PROCESSES IN THE TROPOSPHERE AND LOWER STRATOSPHERE OVER ANTARCTICA WITH A NETWORK OF WIND PROFILERS | |||||
著者名よみ |
カンザワ, ヒロシ
× カンザワ, ヒロシ |
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著者名(英) |
KANZAWA, Hiroshi
× KANZAWA, Hiroshi |
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著者所属(英) | ||||||
en | ||||||
National Institute of Polar Research | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | The wind profiler is a powerful tool to study atmospheric circulation and transport processes because it can measure not only horizontal components but also the vertical component of wind. A wind profiler developed originally by the U.S. NOAA/Environmental Research Laboratories/Wave Propagation Laboratory can measure winds from 0.5-17km above the surface with an altitude resolution of 250m and time resolution under 1 hour. The profiler uses a 400MHz UHF band, and the area of the antenna is about 170m^2. Observations with a network of the wind profilers at several sites over Antarctica will give useful information on meridional circulation in the Antarctic troposphere and lower stratosphere, on vertical motion around the tropopause whose altitude over Antarctica is around 10km, and on disturbances such as convection, gravity waves, baroclinic waves, and so on. Observations are also useful for understanding how, when, and how much ozone, water vapor, and other materials are transported from the stratosphere to the troposphere, and then to the Antarctic surface or the middle latitude troposphere. Problems to be overcome for realizing the project are also briefly discussed. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA10756213 | |||||
書誌情報 |
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology 巻 5, p. 29-38, 発行日 1992-02 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |