<?xml version="1.0" encoding="utf-8" standalone="no"?>
<!DOCTYPE article SYSTEM "http://www.adv-geosci.net/inc/adgeo/copernicus.dtd">
<article language="en">
	<journal>
		<journal_title>Advances in Geosciences</journal_title>
		<journal_url>www.adv-geosci.net</journal_url>
		<issn>1680-7340</issn>
		<eissn>1680-7359</eissn>
		<volume_number>25</volume_number>
		<volume_title>Precipitation: Measurement, Climatology, Remote Sensing, and Modeling (EGU Session 2009)</volume_title>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/adgeo-25-23-2010</doi>
	<article_url>http://www.adv-geosci.net/25/23/2010/</article_url>
	<abstract_html>http://www.adv-geosci.net/25/23/2010/adgeo-25-23-2010.html</abstract_html>
	<fulltext_pdf>http://www.adv-geosci.net/25/23/2010/adgeo-25-23-2010.pdf</fulltext_pdf>
	<start_page>23</start_page>
	<end_page>28</end_page>
	<publication_date>2010-03-08</publication_date>
	<article_title content_type="html">Seasonal changes in diurnal rainfall cycle over and around the Indochina Peninsula observed by TRMM-PR</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>H. G. Takahashi</name>
			<email>hiroshi3@tmu.ac.jp</email>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Kanagawa, Japan</affiliation>
		<affiliation numeration="2" content_type="html">Graduate School of Urban Environmental Sciences, Tokyo Metropolitan University (TMU), Tokyo, Japan</affiliation>
	</affiliations>
	<abstract content_type="html">This study used TRMM-PR data to examine seasonal changes in rainfall
characteristics over the Indochina Peninsula, with a focus on the diurnal
rainfall cycle. No distinct seasonal changes in the phases of diurnal
variations of rainfall were found, even though low-level wind fields changed
largely with the seasonal march. Regions with an afternoon maximum received
large amounts of rainfall during the pre-monsoon season, whereas regions with
a nocturnal or morning rainfall maximum received little rainfall during the
pre-monsoon season. This result suggests that the difference in diurnal
rainfall variations may be associated with the regional differences in
seasonal march of monsoon rainfall over and around the Indochina Peninsula,
through the different mechanism between evening and morning rainfalls.</abstract>
	<references>
		<reference numeration="1" content_type="text"> Fujita, M., Sasaki, T., and Kimura, F.: A dramatic daytime decrease in water vapor over coastal Thailand, SOLA, 2, 49–52, 2006. </reference>
		<reference numeration="2" content_type="text"> Hirose, M. and Nakamura, K.: Spatial and diurnal variation of precipitation systems over Asia observed by the TRMM Precipitation Radar, J. Geophys. Res., 110, D05106, doi:10.1029/2004JD004815, 2005. </reference>
		<reference numeration="3" content_type="text"> Iguchi, T., Kozu, T., Meneghini, R., Awaka, J., and Okamoto, K.: Rain-profiling algorithm for the TRMM Precipitation Radar, J. Appl. Meteorol., 39, 2038–2052, 2000. </reference>
		<reference numeration="4" content_type="text"> Kodama, Y., Ohta, A., Katsumata, M., Mori, S., Satoh, S., and Ueda, H.: Seasonal transition of predominant precipitation type and lightning activity over tropical monsoon areas derived from TRMM observations, Geophys. Res. Lett, 32, doi:10.1029/2005GL022986, 2005. </reference>
		<reference numeration="5" content_type="text"> Matsumoto, J.: Seasonal transition of summer rainy season over indochina and adjacent monsoon region, Adv. Atmos. Sci., 14, 231–245, 1997. </reference>
		<reference numeration="6" content_type="text"> Murakami, M.: Analysis of the deep convective activity over the western Pacific and Southeast Asia. Part I: Diurnal variation, Journal of the Meteorological Society of Japan, 61, 60–76, 1983. </reference>
		<reference numeration="7" content_type="text"> Nitta, T. and Sekine, S.: Diurnal variation of convective activity over the tropical western Pacific, Journal of the Meteorological Society of Japan, 72, 627–641, 1994.  </reference>
		<reference numeration="8" content_type="text"> Onogi, K. et~al.: The JRA-25 Reanalysis, Journal of the Meteorological Society of Japan, 85, 369–432, 2007. </reference>
		<reference numeration="9" content_type="text"> Satomura, T.: Diurnal variation of precipitation over the Indo-China Peninsula: Two-dimensional numerical simulation, Journal of the Meteorological Society of Japan, 78, 461–475, 2000. </reference>
		<reference numeration="10" content_type="text"> Takahashi, H. and Yasunari, T.: A climatological monsoon break in rainfall over Indochina -A singularity in the seasonal march of the Asian summer monsoon-, J. Climate, 19, 1545–1556, 2006.  </reference>
		<reference numeration="11" content_type="text"> Takahashi, H. and Yasunari, T.: Decreasing trend in rainfall over Indochina during the late summer monsoon: Impact of tropical cyclones, Journal of the Meteorological Society of Japan, 86, 429–438, 2008.  </reference>
		<reference numeration="12" content_type="text"> Takahashi, H., Yoshikane, T., Hara, M., and Yasunari, T.: High-resolution regional climate simulations of the long-term decrease in September rainfall over Indochina, Atmos. Sci. Lett., 10(1), 14–18, doi:10.1002/asl.203, 2009. </reference>
		<reference numeration="13" content_type="text"> Takahashi, H., Fujinami, H., Yasunari, T., and Matsumoto, J.: Diurnal rainfall pattern observed by TRMM-PR around the Indochina Peninsula, J. Geophys. Res., 115, \doi10.1029/2009JD012155, 2010a. </reference>
		<reference numeration="14" content_type="text"> Takahashi, H., Yoshikane, T., Hara, M., Takata, K., and Yasunari, T.: High-resolution modelling of the potential impact of land-surface conditions on regional climate over Indochina associated with the diurnal precipitation cycle, Int. J. Climatol., doi:10.1002/joc.2119, 2010b. </reference>
	</references>
</article>

