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  1. 070 環境科学部 = Faculty of Environmental Science
  2. 070 学術雑誌論文 = Articles in academic journal

Distributional correspondence of 94-GHz radar reflectivity with the variation in water cloud properties over the northwestern Pacific and China

http://hdl.handle.net/10069/35118
http://hdl.handle.net/10069/35118
72b9d3ac-fc4a-490e-a648-16609acbb4bf
名前 / ファイル ライセンス アクション
JQSRT153_38.pdf JQSRT153_38.pdf (1.1 MB)
アイテムタイプ 学術雑誌論文 / Journal Article(1)
公開日 2015-03-06
タイトル
タイトル Distributional correspondence of 94-GHz radar reflectivity with the variation in water cloud properties over the northwestern Pacific and China
言語
言語 eng
キーワード
主題Scheme Other
主題 Cloud microphysics
キーワード
主題Scheme Other
主題 CloudSat
キーワード
主題Scheme Other
主題 Drizzle
キーワード
主題Scheme Other
主題 Precipitation
キーワード
主題Scheme Other
主題 Vertical profile
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 journal article
著者 Kawamoto, Kazuaki

× Kawamoto, Kazuaki

Kawamoto, Kazuaki

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Suzuki, Kentaroh

× Suzuki, Kentaroh

Suzuki, Kentaroh

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抄録
内容記述タイプ Abstract
内容記述 This paper studied the behavior of 94-GHz radar reflectivity (Ze) with variation in the properties of low-level water clouds, such as the effective droplet radius (re), geometrical thickness (Dcld), and liquid water path (LWP), over the northwest Pacific and China. The changes in the distribution of maxZe (the largest Ze within a cloud layer) were examined in terms of variation in the cloud parameters such as small, mid and large categories, while maxZe had monomodal distributions regarding variation in re and Dcld, that appeared bimodal in the small category of LWP. It was confirmed that the small category of LWP contained both non-precipitating clouds in the incipient stage and raining clouds in the dissipating stage. Next, optically measured particle size was combined with LWP derived from the microwave measurement to classify the precipitation type. Applying maxZe and Dcld to the analysis of classified precipitation types corroborated the importance of Dcld for examining the occurrence of precipitation. Finally, the position of maxZe relative to the cloud top was investigated using a measure of the probability of precipitation (POP) according to variation in re. The results showed that the Pacific and China had ‘bow’ and ‘funnel’ shapes, respectively. The emergence of these shapes according to the variation in re was interpreted as the enhancement of Ze due to droplet collisional growth and the attenuation of Ze by the presence of large particles. Furthermore, a detailed analysis of smaller particles (<10 μm in radius) reinforced the idea of rapid, efficient particle growth in the lower part of the cloud.
書誌情報 Journal of Quantitative Spectroscopy and Radiative Transfer

巻 153, p. 38-48, 発行日 2015-03
出版者
出版者 Elsevier Ltd
ISSN
収録物識別子タイプ ISSN
収録物識別子 00224073
DOI
関連タイプ isVersionOf
識別子タイプ DOI
関連識別子 10.1016/j.jqsrt.2014.10.012
権利
権利情報 c 2014 Elsevier Ltd.
権利
権利情報 NOTICE: this is the author’s version of a work that was accepted for publication in Journal of Quantitative Spectroscopy and Radiative Transfer. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be reflected in this document. Changes may have been made to this work since it was submitted for publication. A definitive version was subsequently published in Journal of Quantitative Spectroscopy and Radiative Transfer, 153, (2015)
著者版フラグ
出版タイプ AM
出版タイプResource http://purl.org/coar/version/c_ab4af688f83e57aa
引用
内容記述タイプ Other
内容記述 Journal of Quantitative Spectroscopy and Radiative Transfer, 153, pp.38-48; 2015
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