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  1. 防災科研関係論文

Balloon-borne and Raman lidar observations of Asian dust and cirrus cloud properties over Tsukuba, Japan

https://nied-repo.bosai.go.jp/records/2711
https://nied-repo.bosai.go.jp/records/2711
e8b51e9e-aeb2-4f7a-a2e5-249fa341fe4e
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Balloon-borne and Raman lidar observations of Asian dust and cirrus cloud properties over Tsukuba, Japan
言語
言語 eng
著者 Tetsu Sakai

× Tetsu Sakai

en Tetsu Sakai

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Narihiro Orikasa

× Narihiro Orikasa

en Narihiro Orikasa

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Tomohiro Nagai

× Tomohiro Nagai

en Tomohiro Nagai

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Masataka Murakami

× Masataka Murakami

en Masataka Murakami

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Takuya Tajiri

× Takuya Tajiri

en Takuya Tajiri

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Atsushi Saito

× Atsushi Saito

en Atsushi Saito

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Katsuya Yamashita

× Katsuya Yamashita

en Katsuya Yamashita

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Akihiro Hashimoto

× Akihiro Hashimoto

en Akihiro Hashimoto

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抄録
内容記述タイプ Other
内容記述 The vertical distributions of the microphysical and optical properties of tropospheric aerosols and cirrus cloud were measured using an instrumented balloon and a ground-based Raman lidar over Tsukuba, Japan (36 degrees N, 140 degrees E), during the Asian dust events on 9 and 21 May 2007 to investigate the influence of Asian mineral dust on ice cloud formation in the upper troposphere. The instrumented balloon measured the particle size distribution, ice crystal images, dew/frost point, relative humidity, and temperature. The Raman lidar measured the particle backscattering and extinction coefficients and the depolarization ratio at a wavelength of 532 nm. The results of the balloon measurements showed that supermicrometer (0.7 to 2.8 mu m in optical-equivalent radius) dust particles and ice crystals (10 to 400 mu m in maximum dimension) were present in the upper troposphere (8 to 12 km in altitude), with number concentrations varying from 5 x 10(-3) to 0.6 cm(-3) for dust and from 5 x 10(-3) to 0.15 cm(-3) for ice crystals. The Raman lidar measurement indicated that the particle depolarization ratios were 15 to 35% in the altitude range of 6 to 12 km, indicating the predominance of nonspherical particles in the region. The temperature ranged from -33 to -63 degrees C, and the relative humidity with respect to ice (RHi), estimated from the total (vapor plus condensate) water content obtained with the Snow White hygrometer in the cloud, was 130% at maximum on 9 May, which was close to the activation point of Asian mineral dust as ice nuclei to form ice crystals.
言語 en
書誌情報 en : JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES

巻 119, 号 6, p. 3295-3308, 発行日 2014-03
出版者
言語 en
出版者 AMER GEOPHYSICAL UNION
ISSN
収録物識別子タイプ EISSN
収録物識別子 2169-8996
DOI
関連識別子 10.1002/2013JD020987
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