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  1. 防災科研関係論文

Diurnal land-sea rainfall peak migration over Sumatera Island, Indonesian Maritime Continent, observed by TRMM satellite and intensive rawinsonde soundings

https://nied-repo.bosai.go.jp/records/4957
https://nied-repo.bosai.go.jp/records/4957
eff1dce1-7651-4632-8b7f-faeab9ca1bad
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Diurnal land-sea rainfall peak migration over Sumatera Island, Indonesian Maritime Continent, observed by TRMM satellite and intensive rawinsonde soundings
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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Yudi Iman Tauhid

× Yudi Iman Tauhid

en Yudi Iman Tauhid

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Manabu D. Yamanaka

× Manabu D. Yamanaka

en Manabu D. Yamanaka

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Noriko Okamoto

× Noriko Okamoto

en Noriko Okamoto

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Fumie Murata

× Fumie Murata

en Fumie Murata

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Namiko Sakurai

× Namiko Sakurai

en Namiko Sakurai

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Hiroyuki Hashiguchi

× Hiroyuki Hashiguchi

en Hiroyuki Hashiguchi

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Tien Sribimawati

× Tien Sribimawati

en Tien Sribimawati

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抄録
内容記述タイプ Other
内容記述 The diurnal cycle of rainfall and its regional variation over Sumatera Island, Indonesian Maritime Continent, are examined using Tropical Rainfall Measuring Mission (TRMM) satellite precipitation radar (PR) and intensive rawinsonde sounding data. The TRMM PR sensor can detect raindrops directly, regardless of ground and cloud conditions, and can distinguish between convective and stratiform types of rainfall. Rainfall variation over this area was found to have the following characteristics: 1) convective rainfall with a broad peak between 1500 and 2000 LT predominates over the land region of Sumatera Island, whereas rainfall in the early morning, composed almost equally of stratiform and convective types, is predominant over the surrounding sea region. 2) A rainfall peak in the daytime and one in the nighttime migrate with time starting from the southwestern coastline of the island into the inland and offshore regions, respectively. The distance of each rainfall peak migration from the coastline is up to 400 km, and the average speed of migration is approximately 10 m s . 3) Using intensive rawinsonde sounding data, it was also found that remarkable diurnal variations of wind, humidity, and stability appear in the lower troposphere corresponding to the migrating rainfall peaks over both the inland and the coastal sea regions. The mechanism of the diurnal land-sea rainfall peak migration is discussed comprehensively using TRMM PR, intensive rawinsonde soundings, Geostationary Meteorological Satellite (GMS) data, objective reanalysis, and ground-based observation data. Finally, a crucial difference in rainfall peak migrating mechanisms is suggested between those toward the inland region in the daytime and the offshore region in the nighttime. c 2004 American Meteorological Society. -1
言語 en
書誌情報 en : Monthly Weather Review

巻 132, 号 8, p. 2021-2039, 発行日 2004-08
ISSN
収録物識別子タイプ ISSN
収録物識別子 0027-0644
DOI
関連識別子 10.1175/1520-0493(2004)132<2021:DLRPMO>2.0.CO;2
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