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SPECTRAL ALBEDO OBSERVATION ON THE SNOW FIELD AT BARROW, ALASKA
https://doi.org/10.15094/00002861
https://doi.org/10.15094/00002861af5edc8b-550f-4c30-bfed-43245adff11a
名前 / ファイル | ライセンス | アクション |
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KJ00002364371 (1.1 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1998-11-01 | |||||
タイトル | ||||||
タイトル | SPECTRAL ALBEDO OBSERVATION ON THE SNOW FIELD AT BARROW, ALASKA | |||||
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 | 10.15094/00002861 | |||||
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 | SPECTRAL ALBEDO OBSERVATION ON THE SNOW FIELD AT BARROW, ALASKA | |||||
著者名よみ |
アオキ, テルオ
× アオキ, テルオ× アオキ, タダオ× フカボリ, マサシ× タチバナ, ヨシヒロ× ザイゼン, ユウジ× ニシオ, フミヒコ× オイシ, トモヒコ |
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著者名(英) |
AOKI, Teruo
× AOKI, Teruo× AOKI, Tadao× FUKABORI, Masashi× TACHIBANA, Yoshihiro× ZAIZEN, Yuji× NISHIO, Fumihiko× OISHI, Tomohiko |
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著者所属(英) | ||||||
en | ||||||
Meteorological Research Institute | ||||||
著者所属(英) | ||||||
en | ||||||
Meteorological Research Institute | ||||||
著者所属(英) | ||||||
en | ||||||
Meteorological Research Institute | ||||||
著者所属(英) | ||||||
en | ||||||
Research Institute of Civilization, Tokai University | ||||||
著者所属(英) | ||||||
en | ||||||
Meteorological Research Institute | ||||||
著者所属(英) | ||||||
en | ||||||
Hokkaido University of Education | ||||||
著者所属(英) | ||||||
en | ||||||
Tokai University | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Spectral albedo observation at the visible and near infrared wavelengths was carried out on the snow field at Barrow. Alaska in April, 1997. The data are compared with the theoretical calculations made by a multiple scattering radiative transfer model for the atmosphere-snow system using the snow physical parameters observed by snow pit work. It is found that the optically effective snow grain size is on the order of branch size for new snow consisting of dendrites, but is not of the crystal size. The observed spectral albedo was lower than theoretically calculated for "pure snow" in the visible and a part of the near infrared; such reduction is explained by the internal mixture of soot and external mixture of dust for snow particles. The theoretical spectral albedo calculated for a two-layer snow model that contains impurities agrees very well with the observations at all wavelengths. | |||||
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 12, p. 1-9, 発行日 1998-11 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |