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Physical properties of maritime low clouds as retrieved by combined use of Tropical Rainfall Measuring Mission (TRMM) Microwave Imager and Visible/Infrared Scanner : 2. Climatology of warm clouds and rain
http://hdl.handle.net/2261/51883
http://hdl.handle.net/2261/518838f52806b-fde5-483b-b43c-1b4dd2759eeb
名前 / ファイル | ライセンス | アクション |
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Nakajima2002JGRA_H24P75.pdf (6.0 MB)
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Item type | 学術雑誌論文 / Journal Article(1) | |||||
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公開日 | 2017-01-10 | |||||
タイトル | ||||||
タイトル | Physical properties of maritime low clouds as retrieved by combined use of Tropical Rainfall Measuring Mission (TRMM) Microwave Imager and Visible/Infrared Scanner : 2. Climatology of warm clouds and rain | |||||
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 |
Masunaga, Hirohiko
× Masunaga, Hirohiko× Nakajima, Takashi Y.× Nakajima, Teruyuki× Kachi, Misako× Suzuki, Kentaroh |
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著者所属 | ||||||
著者所属 | Earth Observation Research Center, National Space Development Agency | |||||
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 | In this paper, we investigate characteristics of low clouds and warm-rain production in terms of droplet growth based on the effective droplet radii retrieved by a combined use of visible, infrared, and microwave satellite remote sensing. We propose to categorize low clouds into the following groups: (1) nondrizzling, nonraining clouds; (2) nonraining clouds with drizzling near the cloud top; (3) raining clouds; and (4) clouds with no clear interpretation in terms of the effective radii derived using two different schemes. This categorization is supported by examination of the correlation between static stability and the retrieved results in the three "precipitating regions" (the Middle Pacific, South Pacific Convergence Zone [SPCZ], and Intertropical Convergence Zone [ITCZ] cumulus regions) and in the four "nonprecipitating regions" (the Californian, Peruvian, Namibian, and eastern Asian stratus regions). The rain rate derived by Precipitation Radar (PR) provides global characteristics consistent with our results. Californian and Peruvian stratus clouds are found to frequently have the drizzle mode near the cloud top, whereas Namibian strati have fewer chances to drizzle. The drizzle mode almost completely disappears in the eastern Asian region in the winter. The cloud-aerosol interaction is a promising candidate for suppressing the drizzle mode formation in nonprecipitating clouds. | |||||
書誌情報 |
Journal of geophysical research. D 巻 107, 号 D19, p. 4367, 発行日 2002-10-02 |
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ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 01480227 | |||||
書誌レコードID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA10819765 | |||||
DOI | ||||||
識別子タイプ | DOI | |||||
関連識別子 | info:doi/10.1029/2001JD001269 | |||||
権利 | ||||||
権利情報 | Copyright 2002 by the American Geophysical Union. | |||||
日本十進分類法 | ||||||
主題 | 451 | |||||
主題Scheme | NDC | |||||
出版者 | ||||||
出版者 | American Geophysical Union | |||||
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/10.1029/2001JD001269 |