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The simulated precipitation system was enhanced over the northwestern part of the island due to wind passing around Jeju Island, low-level convergence (1.6 x 10(-3) s(-1)) due to orographic blocking, and high RH (similar to 95%). In order to clarify the influence of topography and the low-level moist environment on enhancement of the precipitation system, numerical sensitivity experiments were conducted. The NOTR (no terrain) experiment produced straightforward wind without low-level convergence over the topography. Associated with these features, the CNTL rainfall amount on the northwestern lateral side of the island was 30.6% more than that produced in NOTR. A comparison of RH-controlled experiments and CNTL revealed that increasing moisture in the low-level environment resulted in greater intensity of the precipitation system. A reduction in low-level RH by as little as 2% could result in a 20.8% reduction in rainfall amount. 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  1. 防災科研関係論文

Enhancement mechanism of the 30 June 2006 precipitation system observed over the northwestern slope of Mt. Halla, Jeju Island, Korea

https://nied-repo.bosai.go.jp/records/4227
https://nied-repo.bosai.go.jp/records/4227
1bee61f3-f893-44ea-bede-ad0085f39f48
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Enhancement mechanism of the 30 June 2006 precipitation system observed over the northwestern slope of Mt. Halla, Jeju Island, Korea
言語
言語 eng
著者 Keun-Ok Lee

× Keun-Ok Lee

en Keun-Ok Lee

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Shingo Shimizu

× Shingo Shimizu

en Shingo Shimizu

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Masayuki Maki

× Masayuki Maki

en Masayuki Maki

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Cheol-Hwan You

× Cheol-Hwan You

en Cheol-Hwan You

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Hiroshi Uyeda

× Hiroshi Uyeda

en Hiroshi Uyeda

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Dong-In Lee

× Dong-In Lee

en Dong-In Lee

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抄録
内容記述タイプ Other
内容記述 Doppler radar analysis and a cloud-resolving storm simulator (CReSS) are used to investigate the enhancement mechanism of a localized intense precipitation system that occurred over Jeju Island, Korea, on 30 June 2006. Rain gauge data revealed intensive rainfall (> 80 mm in 100 min) over northwest of Jeju Island, and relatively low rainfall (<= 20 mm) over the northeast of the island. The environment of the precipitation system consisted of near-saturated air (relative humidity (RH): similar to 95%) from the surface to 700 hPa and a low lifting condensation level of 951 hPa. Doppler radar analysis revealed enhancement of the precipitation system on the northwestern lateral side (in this study, the term 'lateral side' refers to the sides of the mountain other than the lee-side and windward side) of Mt. Halla, the central mountain on the island (1950 m). In the region of enhancement low-level convergence (7 x 10(-4) s(-1)) induced by orographic blocking with a relatively low Froude number (0.55) was observed. These observations were well simulated by a control run (CNTL) using CReSS. The simulated precipitation system was enhanced over the northwestern part of the island due to wind passing around Jeju Island, low-level convergence (1.6 x 10(-3) s(-1)) due to orographic blocking, and high RH (similar to 95%). In order to clarify the influence of topography and the low-level moist environment on enhancement of the precipitation system, numerical sensitivity experiments were conducted. The NOTR (no terrain) experiment produced straightforward wind without low-level convergence over the topography. Associated with these features, the CNTL rainfall amount on the northwestern lateral side of the island was 30.6% more than that produced in NOTR. A comparison of RH-controlled experiments and CNTL revealed that increasing moisture in the low-level environment resulted in greater intensity of the precipitation system. A reduction in low-level RH by as little as 2% could result in a 20.8% reduction in rainfall amount. Therefore, land areas with small, narrow, but steep topographic features, such as Jeju Island, could determine the intensity and location of the precipitation system under a moist environment during the rainy season. (c) 2010 Elsevier B.V. All rights reserved.
言語 en
書誌情報 en : ATMOSPHERIC RESEARCH

巻 97, 号 3, p. 343-358
出版者
言語 en
出版者 ELSEVIER SCIENCE INC
ISSN
収録物識別子タイプ ISSN
収録物識別子 0169-8095
DOI
関連識別子 10.1016/j.atmosres.2010.04.008
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