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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

Cloud and Water Vapor Feedbacks in a Vertical Energy-Balance Model with Maximum Entropy Production

http://hdl.handle.net/2261/51877
http://hdl.handle.net/2261/51877
2fae0dfe-ef6a-4a75-bcbe-8f6060b932e8
名前 / ファイル ライセンス アクション
Nakajima2008JC_H24P133.pdf Nakajima2008JC_H24P133.pdf (327.7 kB)
Item type 学術雑誌論文 / Journal Article(1)
公開日 2017-01-10
タイトル
タイトル Cloud and Water Vapor Feedbacks in a Vertical Energy-Balance Model with Maximum Entropy Production
言語
言語 eng
キーワード
主題Scheme Other
主題 Feedback
キーワード
主題Scheme Other
主題 Clouds
キーワード
主題Scheme Other
主題 Water vapor
キーワード
主題Scheme Other
主題 Energy budget
キーワード
主題Scheme Other
主題 Entropy
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ journal article
著者 Wang, Biao

× Wang, Biao

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Wang, Biao

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Nakajima, Teruyuki

× Nakajima, Teruyuki

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Nakajima, Teruyuki

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Shi, Guangyu

× Shi, Guangyu

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Shi, Guangyu

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著者所属
著者所属 State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Science
著者所属
著者所属 Center for Climate System Research, Tokyo University
抄録
内容記述タイプ Abstract
内容記述 A vertically one-dimensional model is developed with cloud fraction constrained by the maximum entropy production (MEP) principle. The model reasonably reproduces the global mean climate with its surface temperature, radiation and heat fluxes, cloud fraction, and lapse rate. The maximum convection hypothesis in Paltridge's models is related to the MEP principle, and the MEP state of climate is approximately equivalent to that with the maximum lapse rate. The sensitivity investigation about the model assumptions and the prescribed parameters show that the model is considerably robust in simulating the global mean climate. With the MEP constraint, the feedbacks of cloud and water vapor to external forcings, such as changes of CO2 concentration, solar incidence, and surface albedo, are evaluated. While water vapor always behaves as a strong positive feedback, cloud feedbacks to the different forcings are different, in both magnitude and sign. The modeled feedback of cloud fraction to the forcing resulting from surface albedo variation seems in good agreement with the observed seasonal variation of the global cloud fraction.
書誌情報 Journal of climate

巻 21, 号 24, p. 6689-6697, 発行日 2008-12-15
ISSN
収録物識別子タイプ ISSN
収録物識別子 08948755
書誌レコードID
収録物識別子タイプ NCID
収録物識別子 AA10683936
DOI
識別子タイプ DOI
関連識別子 info:doi/10.1175/2008JCLI2349.1
権利
権利情報 © Copyright 2008 American Meteorological Society (AMS). Permission to use figures, tables, and brief excerpts from this work in scientific and educational works is hereby granted provided that the source is acknowledged. Any use of material in this work that is determined to be “fair use” under Section 107 of the U.S. Copyright Act or that satisfies the conditions specified in Section 108 of the U.S. Copyright Act (17 USC §108, as revised by P.L. 94-553) does not require the AMS’s permission. Republication, systematic reproduction, posting in electronic form, such as on a web site or in a searchable database, or other uses of this material, except as exempted by the above statement, requires written permission or a license from the AMS. Additional details are provided in the AMS Copyright Policy, available on the AMS Web site located at (http://www.ametsoc.org/) or from the AMS at 617-227-2425 or copyright@ametsoc.org.
日本十進分類法
主題Scheme NDC
主題 451
出版者
出版者 American Meteorological Society
異版である
関連タイプ isVersionOf
識別子タイプ URI
関連識別子 http://doi.org/10.1175/2008JCLI2349.1
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