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  1. 139 大気海洋研究所
  2. 10 気候システム研究系
  3. 1391010 学術雑誌
  1. 0 資料タイプ別
  2. 10 学術雑誌論文
  3. 014 自然科学

Glory of clouds in the near infrared

http://hdl.handle.net/2261/51844
http://hdl.handle.net/2261/51844
30f843a7-d311-4d7a-9d4a-10b069bdd102
名前 / ファイル ライセンス アクション
Nakajima1994OSA_H24P30.pdf Nakajima1994OSA_H24P30.pdf (1.9 MB)
Item type 学術雑誌論文 / Journal Article(1)
公開日 2017-01-06
タイトル
タイトル Glory of clouds in the near infrared
言語
言語 eng
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ journal article
著者 Spinhirne, James D.

× Spinhirne, James D.

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Spinhirne, James D.

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Nakajima, Teruyuki

× Nakajima, Teruyuki

WEKO 3244

Nakajima, Teruyuki

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著者所属
著者所属 Laboratory for Atmospheres, Code 917, NASA Goddard Space Flight Center
著者所属
著者所属 Center for Climate System Research, University of Tokyo
抄録
内容記述タイプ Abstract
内容記述 Spectrally resolved visible and infrared images of marine stratus clouds were acquired from the NASA ER-2 high-altitude aircraft during the 1987 First International Cloud Climatology Program Regional Experiment. The images were obtained by cross-track scanning radiometers. Data images at near-infrared wavelengths show frequent and readily apparent brightness features that are due to glory single scattering. The observations and subsequent analysis by radiative transfer calculations show that the glory is a significant feature of near-infrared solar reflectance from water clouds. Glory observations and calculations based on in-cloud microphysics measurements agree well. The most dramatic difference from the visible glory is that the scattering angles are significantly larger in the near infrared. The glory is also apparently more distinct in the near infrared than in the visible, as scattering size parameters are in a range that effectively produces a glory feature, and also there is less obscuration by multiple-scattering reflectance because of absorption of radiation by droplets in the near infrared. For both the visible and the near infrared, the principal factors that wash out the glory are dispersion and, to a lesser degree, the effective radius of the cloud droplet-size distribution. The obscuration by multiple scattering in optically thick clouds is secondary. Rather than being a novelty, glory observations would be an accurate and unambiguous technique to sense the droplet size of water clouds remotely.
書誌情報 Applied optics

巻 33, 号 21, p. 4652-4662, 発行日 1994-07-20
ISSN
収録物識別子タイプ ISSN
収録物識別子 00036935
書誌レコードID
収録物識別子タイプ NCID
収録物識別子 AA00543409
DOI
識別子タイプ DOI
関連識別子 info:doi/10.1364/AO.33.004652
権利
権利情報 © 1994 Optical Society of America
日本十進分類法
主題Scheme NDC
主題 451
出版者
出版者 Optical Society of America
異版である
関連タイプ isVersionOf
識別子タイプ URI
関連識別子 http://www.opticsinfobase.org/ao/abstract.cfm?uri=ao-33-21-4652
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