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A COMPARISON OF OBSERVATION WITH MODELING FOR ALBEDO AND TRANSMITTANCE OF SNOW
https://doi.org/10.15094/00003845
https://doi.org/10.15094/000038457b3842bd-9fcd-4093-872e-662959679558
名前 / ファイル | ライセンス | アクション |
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KJ00000767953 (53.4 kB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1994-11-01 | |||||
タイトル | ||||||
タイトル | A COMPARISON OF OBSERVATION WITH MODELING FOR ALBEDO AND TRANSMITTANCE OF SNOW | |||||
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 | 10.15094/00003845 | |||||
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 | ||||||
ABSTRACT | ||||||
論文名よみ | ||||||
その他のタイトル | A COMPARISON OF OBSERVATION WITH MODELING FOR ALBEDO AND TRANSMITTANCE OF SNOW | |||||
著者名よみ |
アオキ, テルオ
× アオキ, テルオ× セコ, カツモト× アオキ, タダオ× フカボリ, マサシ |
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著者名(英) |
AOKI, Teruo
× AOKI, Teruo× SEKO, Katsumoto× AOKI, Tadao× FUKABORI, Masashi |
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著者所属(英) | ||||||
en | ||||||
Meteorological Research Institute | ||||||
著者所属(英) | ||||||
en | ||||||
Atmospheric and Water Research Institute, Nagoya University | ||||||
著者所属(英) | ||||||
en | ||||||
Meteorological Research Institute | ||||||
著者所属(英) | ||||||
en | ||||||
Meteorological Research Institute | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Snow surface albedo and transmittance inside the snow have been investigated by observation and modeling. Observations were taken by a grating type spectrometer at Tokamachi in March 1993. The observed snow was old and very wet. Microscope photo-graphs of snow grains taken at this time indicate that snow grain is spherical particles with size of about 1.0μm. Surface albedo and transmittance of snow by a multiple scattering model for the atmosphere-snow system with pure snow grain size of 1.0μm have similar wavelength dependence to our observation. Though both the maximum albedo and transmit-tance have been observed at the wavelength 0.55μm, model calculation shows that this wavelength is 0.45μm. Moreover, the observed albedo is lower than the model with a maximum of 10% in visible region. It is considered that these differences are mainly due to impurities and/or liquid water in natural snow. | |||||
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 8, p. 188, 発行日 1994-11 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |