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EFFECTIVE EMISSIVITY OF CLOUDS FROM RADIOMETERSONDE MEASUREMENTS AT SYOWA STATION, ANTARCTICA
https://doi.org/10.15094/00003885
https://doi.org/10.15094/00003885a67e284f-2c29-47ce-af87-9255f0d61394
名前 / ファイル | ライセンス | アクション |
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KJ00001015002 (1.3 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1995-09-01 | |||||
タイトル | ||||||
タイトル | EFFECTIVE EMISSIVITY OF CLOUDS FROM RADIOMETERSONDE MEASUREMENTS AT SYOWA STATION, ANTARCTICA | |||||
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 | 10.15094/00003885 | |||||
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 | EFFECTIVE EMISSIVITY OF CLOUDS FROM RADIOMETERSONDE MEASUREMENTS AT SYOWA STATION, ANTARCTICA | |||||
著者名よみ |
ヤマモト, アキラ
× ヤマモト, アキラ× ヤマノウチ, タカシ× ワダ, マコト |
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著者名(英) |
YAMAMOTO, Akira
× YAMAMOTO, Akira× YAMANOUCHI, Takashi× WADA, Makoto |
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著者所属(英) | ||||||
en | ||||||
Meteorological Research Institute | ||||||
著者所属(英) | ||||||
en | ||||||
National Institute of Polar Research | ||||||
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 effective emissivity of Antarctic clouds is calculated from radiation measurements using the radiometersonde in 1987 at Syowa Station, Antarctica. The accuracy of the radiometersonde near the surface is evaluated by comparison with a pyrgeometer on the ground surface. The effective emissivity is referred to vertical integrated liquid water content (LWC) from microwave radiation measurements. Though disagreement of measured volume might occur between the microwave radiometer and the sonde, the effective emissivity for downward flux correlates well to the LWC, but that for upward flux does not. A large discrepancy is found between the effective emissivity for upward flux and that for downward flux, and especially, for upward flux, the effective emissivity is very small in some cases. It is assumed that the scattering of longwave radiation by water and ice particles produces this discrepancy. The value of the LWC suggests that water particles may exist much closer to the cloud top than the cloud base. Difference among features of the effective emissivity due to type of cloud systems resolved from NOAA/AVHRR imagery is not found in this study. | |||||
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 9, p. 133-145, 発行日 1995-09 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |