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CLOUD-RADIATIVE FORCING OVER THE SNOW-COVERED SURFACE AROUND ASUKA STATION, ANTARCTICA
https://doi.org/10.15094/00003700
https://doi.org/10.15094/000037009e650514-8db9-4409-aaa0-f7d47e69737d
名前 / ファイル | ライセンス | アクション |
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KJ00002409929 (2.1 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 | CLOUD-RADIATIVE FORCING OVER THE SNOW-COVERED SURFACE AROUND ASUKA 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 | 10.15094/00003700 | |||||
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 | CLOUD-RADIATIVE FORCING OVER THE SNOW-COVERED SURFACE AROUND ASUKA STATION, ANTARCTICA | |||||
著者名よみ |
アオキ, テルオ
× アオキ, テルオ× ヤマノウチ, タカシ |
|||||
著者名(英) |
AOKI, Teruo
× AOKI, Teruo× YAMANOUCHI, Takashi |
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著者所属(英) | ||||||
en | ||||||
Meteorological Research Institute | ||||||
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 | Cloud-radiative forcing at the snow-covered surface in Antarctica was estimated from data of the radiation budget observation at Asuka Station (71°31'S, 24°08'E, 930m) in 1988. Cloud-radiative forcing at the top of the atmosphere was also estimated from satellite data in December 1988. It was found that shortwave forcing was negative (cooling) at the surface and positive (heating) at the top of the atmosphere. The longwave forcing was positive both at the surface and at the top of the atmosphere. The (shortwave+longwave) forcing was positive both at the surface and at the top of the atmosphere. This is different from those in middle and the low latitudes. The cloud-radiative forcing distributions at the top of the atmosphere in the extended region from the sea to inland were estimated from the satellite data in December 1988. The results indicated that the shortwave forcing was positive over the snow-covered region except the high inland, and negative over the sea. The longwave forcing was positive over all regions. The (shortwave+longwave) forcing was positive over the snow-covered regions except the high inland plateau, and negative over the sea. | |||||
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. 76-89, 発行日 1992-02 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |