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MERIDIONAL DISTRIBUTION OF SHORT-VERTICAL-SCALE FLUCTUATIONS IN THE LOWER STRATOSPHERE REVEALED BY CROSS-EQUATORIAL OZONESONDE OBSERVATIONS ON "SHIRASE"
https://doi.org/10.15094/00003982
https://doi.org/10.15094/00003982044cc550-70fd-4fa0-8301-8875574f6264
名前 / ファイル | ライセンス | アクション |
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KJ00001014945 (1.8 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1997-11-01 | |||||
タイトル | ||||||
タイトル | MERIDIONAL DISTRIBUTION OF SHORT-VERTICAL-SCALE FLUCTUATIONS IN THE LOWER STRATOSPHERE REVEALED BY CROSS-EQUATORIAL OZONESONDE OBSERVATIONS ON "SHIRASE" | |||||
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 | 10.15094/00003982 | |||||
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 | MERIDIONAL DISTRIBUTION OF SHORT-VERTICAL-SCALE FLUCTUATIONS IN THE LOWER STRATOSPHERE REVEALED BY CROSS-EQUATORIAL OZONESONDE OBSERVATIONS ON "SHIRASE" | |||||
著者名よみ |
オギノ, シンヤ
× オギノ, シンヤ× ヤマナカ, マナブ× カネト, ススム× ヤマノウチ, タカシ× フカオ, ショウイチロウ |
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著者名(英) |
OGINO, Shin-Ya
× OGINO, Shin-Ya× YAMANAKA, Manabu D.× KANETO, Susumu× YAMANOUCHI, Takashi× FUKAO, Shoichiro |
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著者所属(英) | ||||||
en | ||||||
Radio Atmospheric Science Center, Kyoto University | ||||||
著者所属(英) | ||||||
en | ||||||
Radio Atmospheric Science Center, Kyoto University | ||||||
著者所属(英) | ||||||
en | ||||||
Antarctic Observations Office, Japan Meteorological Agency | ||||||
著者所属(英) | ||||||
en | ||||||
National Institute of Polar Research | ||||||
著者所属(英) | ||||||
en | ||||||
Radio Atmospheric Science Center, Kyoto University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Meridional distribution of magnitude for short-vertical-scale fluctuations in the lower stratosphere over the wide latitudinal region between 62°S-43°N roughly along 120°E is investigated on the basis of vertical wavenumber spectra analyzed from temperature and ozone mixing ratio data observed by ozonesondes on "SHIRASE" cruises from 1987 to 1990. The power spectral densities of the 4.0km, 2.7km and 2.0km wavelength components for normalized temperature and normalized ozone mixing ratio in the altitude range of 19-27km are plotted as functions of latitude. It is found that there are symmetrical distributions with maxima near the equator as the first component and asymmetrical ones with larger value in the Northern Hemisphere as the second component for power spectral densities of normalized temperature. However, similar features are not found in distributions of ozone mixing ratio. To investigate this inconsistency, detailed short-vertical-scale structures of potential temperature and ozone mixing ratio have been compared. It is found that they do not show good agreement in the mid-latitude region. | |||||
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 11, p. 199-210, 発行日 1997-11 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |