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The other part migrated offshore at a speed of approximately 4 m s_1 and intensified until around 21 LT while still offshore. Additional convective cells also developed offshore in the early morning hours, independent of those that formed over land. 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  1. 防災科研関係論文

Convective systems developed along the coastline of sumatera island, indonesia, observed with an X-band doppler radar during the HARIMAU2006 campaign

https://nied-repo.bosai.go.jp/records/5507
https://nied-repo.bosai.go.jp/records/5507
0c618b5c-b179-498e-b483-0ef7da1f9738
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Convective systems developed along the coastline of sumatera island, indonesia, observed with an X-band doppler radar during the HARIMAU2006 campaign
言語
言語 eng
著者 Shuichi Mori

× Shuichi Mori

en Shuichi Mori

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Hamada Jun-Ichi

× Hamada Jun-Ichi

en Hamada Jun-Ichi

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Namiko Sakurai

× Namiko Sakurai

en Namiko Sakurai

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Hironori Fudeyasu

× Hironori Fudeyasu

en Hironori Fudeyasu

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Masayuki Kawashima

× Masayuki Kawashima

en Masayuki Kawashima

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Hiroyuki Hashiguchi

× Hiroyuki Hashiguchi

en Hiroyuki Hashiguchi

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Fadli Syamsudin

× Fadli Syamsudin

en Fadli Syamsudin

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Ardhi A. Arbain

× Ardhi A. Arbain

en Ardhi A. Arbain

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Reni Sulistyowati

× Reni Sulistyowati

en Reni Sulistyowati

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Jun Matsumoto

× Jun Matsumoto

en Jun Matsumoto

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Manabu D. Yamanaka

× Manabu D. Yamanaka

en Manabu D. Yamanaka

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抄録
内容記述タイプ Other
内容記述 An overview of convective activity during the HARIMAU2006 campaign conducted from 26 October to 27 November 2006 was presented, focusing on the di{currency sign}erences between coastal land/sea and inactive/active phases of intraseasonal variation (ISV) based on observations using an X-band Doppler radar (XDR) and intensive soundings at Sumatera Island. Diurnal variation (DV) in coastal convections and formation of the coastal heavy rainband (CHeR) along Sumatera Island were also examined in terms of diurnal land-sea migration of coastal convective systems.Convection in the ISV inactive period (PP1) contained convective rain fractions nearly twice as much as stratiform rain fractions, whereas that in the ISV active period (PP2) comprised convective and stratiform elements almost equally. Vertical profiles of radar echo coverage for stratiform rain during PP2 were greater than those during PP1, especially in the lower troposphere over the sea. The radar echo coverage for convective rain over the sea during both periods was nearly double that over land from the near surface up to 6 km high. Convection was generated in the southwestern foothills of the mountain range in the early afternoon (12-15Local Time, LT). Part of the convective system remained over the coastal land and exhibited weak reflectivity until the next morning. The other part migrated offshore at a speed of approximately 4 m s_1 and intensified until around 21 LT while still offshore. Additional convective cells also developed offshore in the early morning hours, independent of those that formed over land. Results suggested that the CHeR along Sumatera Island is dictated by diurnal variations in coastal convective development and consists of the following phases: 1) migration of convection away from the coastal land and its redevelopment in the late evening, and 2) additional generation of convection just offshore during the early morning hours. c 2011, Meteorological Society of Japan.
言語 en
書誌情報 en : Journal of the Meteorological Society of Japan

巻 89, 号 A, p. 61-81, 発行日 2011
ISSN
収録物識別子タイプ ISSN
収録物識別子 0026-1165
DOI
関連識別子 10.2151/jmsj.2011-A04
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