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Preliminary validation of the GLI cryosphere algorithms with MODIS daytime data
https://doi.org/10.15094/00002926
https://doi.org/10.15094/00002926719f8412-a4b0-422f-9883-7fb8b6d33978
名前 / ファイル | ライセンス | アクション |
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KJ00002364413 (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 | 2001-11-01 | |||||
タイトル | ||||||
タイトル | Preliminary validation of the GLI cryosphere algorithms with MODIS daytime data | |||||
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 | 10.15094/00002926 | |||||
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) | |||||
記事種別(英) | ||||||
en | ||||||
Scientific Paper | ||||||
論文名よみ | ||||||
その他のタイトル | Preliminary validation of the GLI cryosphere algorithms with MODIS daytime data | |||||
著者名よみ |
ホリ, マサヒロ
× ホリ, マサヒロ× アオキ, テルオ× / / |
|||||
著者名(英) |
Hori, Masahiro
× Hori, Masahiro× Aoki, Teruo× Stamnes, Knut× Chen, Bingquan× Li, Wei |
|||||
著者所属(英) | ||||||
en | ||||||
National Space Development Agency of Japan | ||||||
著者所属(英) | ||||||
en | ||||||
Meteorological Research Institute | ||||||
著者所属(英) | ||||||
en | ||||||
Stevens Institute of Technology | ||||||
著者所属(英) | ||||||
en | ||||||
Stevens Institute of Technology | ||||||
著者所属(英) | ||||||
en | ||||||
Stevens Institute of Technology | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Preliminary validation of the two GLI cryosphere algorithms is conducted by applying them to MODIS daytime data on June 18,2000. One of the algorithms has been developed for the discrimination of cloud/clear and snow/sea-ice, and the other for the retrievals of snow grain size and mass fraction of impurities mixed in snow. Analysis results show that cloudy areas around the northern polar region are successfully discriminated from areas under clear condition with various surface types such as snow, open ocean and bare land. Reasonable spatial distributions of snow grain size and mass fraction of impurities around the North Pole are also successfully retrieved in the range from nearly 0.0 to over 5000μm for snow grain size and 0.0-0.2 ppmw for snow impurities. Finally, possible sources of error in the retrieved parameters and remaining development points on the present version of the GLI algorithms to be improved for future advances are discussed. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA1129795X | |||||
書誌情報 |
Polar meteorology and glaciology 巻 15, p. 1-20, 発行日 2001-11 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |