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<ArticleSet>
<Article>
<Journal>
				<PublisherName></PublisherName>
				<JournalTitle>Environmental Management Hazards</JournalTitle>
				<Issn>2423-415X</Issn>
				<Volume>3</Volume>
				<Issue>1</Issue>
				<PubDate PubStatus="epublish">
					<Year>2016</Year>
					<Month>03</Month>
					<Day>20</Day>
				</PubDate>
			</Journal>
<ArticleTitle>Thermodynamic and Synoptic Analyses of Pick Floods Caused by Showery Precipitation in Mountainous Regions (Ghare Sou Basin)</ArticleTitle>
<VernacularTitle>Thermodynamic and Synoptic Analyses of Pick Floods Caused by Showery Precipitation in Mountainous Regions (Ghare Sou Basin)</VernacularTitle>
			<FirstPage>75</FirstPage>
			<LastPage>90</LastPage>
			<ELocationID EIdType="pii">59276</ELocationID>
			
<ELocationID EIdType="doi">10.22059/jhsci.2016.59276</ELocationID>
			
			<Language>FA</Language>
<AuthorList>
<Author>
					<FirstName>Mostafa</FirstName>
					<LastName>Karampoor</LastName>
<Affiliation>Assistant Professor, University of Lorestan, Lorestan, Iran</Affiliation>

</Author>
<Author>
					<FirstName>Zahra</FirstName>
					<LastName>Zarei Cheghabaleki</LastName>
<Affiliation>PhD student of Climatology, University of Lorestan, Lorestan, Iran</Affiliation>

</Author>
<Author>
					<FirstName>Akram</FirstName>
					<LastName>Mirhashemei</LastName>
<Affiliation>BA in Natural Geography, Lorestan, Iran</Affiliation>

</Author>
<Author>
					<FirstName>Mohammad</FirstName>
					<LastName>Rostami Fath Abadi</LastName>
<Affiliation>BA in Natural Geography, Lorestan, Iran</Affiliation>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2016</Year>
					<Month>10</Month>
					<Day>01</Day>
				</PubDate>
			</History>
		<Abstract>&lt;strong&gt;Abstract&lt;/strong&gt;
Ghare Sou basin is one of the sub-basins of Karkeh River located in Kermanshah, West of Iran. In spite of not being a flood-prone area in terms of physiography, severe floods have occurred in this region. The main aim of the present study is to present an overview of &lt;em&gt;thermodynamic&lt;/em&gt;and &lt;em&gt;synoptic&lt;/em&gt;conditions affecting precipitations causing extreme flows. Accordingly, two databases were made use of: a) data including discharge and daily precipitation measured at the basin area covering the period of 1389-1351 and b) data including air temperature, air pressure, geopotential height, zonal and meridional wind speed, specific and relative humidity related to the levels of 1000, 850, 700, 500, 600, 400, 300, 250, 150, and 100 hPa provided on the NCEP / NCAR for each six-hour monitoring. Then, with application of the probability distribution method, the ultimate limit of type I with a ten thousand-year return period of 02/247 cubic meters per second per day discharge threshold was specified as diagnostic criteria for exceptional flows. Finally, five floods were extracted for explanation, among which one sample was analyzed. The obtained results revealed that during rainy days, blocking systems such as Rex, Omega, cut-off low, and high-pressure stack systems in the middle levels of the atmosphere were dominant over Mediterranean and Middle East region; the mentioned patterns revealed disruption of normal atmosphere. Moreover, analyses of the indexes and thermodynamic charts were indicative of non-modular arithmetic of maximum indexes and maximum conditional instability with maximum precipitation. Hence, acquaintance with synoptic conditions of systems leading to floods can be of great significance in presenting flood warnings before occurrence of any crises.
 </Abstract>
			<OtherAbstract Language="FA">&lt;strong&gt;Abstract&lt;/strong&gt;
Ghare Sou basin is one of the sub-basins of Karkeh River located in Kermanshah, West of Iran. In spite of not being a flood-prone area in terms of physiography, severe floods have occurred in this region. The main aim of the present study is to present an overview of &lt;em&gt;thermodynamic&lt;/em&gt;and &lt;em&gt;synoptic&lt;/em&gt;conditions affecting precipitations causing extreme flows. Accordingly, two databases were made use of: a) data including discharge and daily precipitation measured at the basin area covering the period of 1389-1351 and b) data including air temperature, air pressure, geopotential height, zonal and meridional wind speed, specific and relative humidity related to the levels of 1000, 850, 700, 500, 600, 400, 300, 250, 150, and 100 hPa provided on the NCEP / NCAR for each six-hour monitoring. Then, with application of the probability distribution method, the ultimate limit of type I with a ten thousand-year return period of 02/247 cubic meters per second per day discharge threshold was specified as diagnostic criteria for exceptional flows. Finally, five floods were extracted for explanation, among which one sample was analyzed. The obtained results revealed that during rainy days, blocking systems such as Rex, Omega, cut-off low, and high-pressure stack systems in the middle levels of the atmosphere were dominant over Mediterranean and Middle East region; the mentioned patterns revealed disruption of normal atmosphere. Moreover, analyses of the indexes and thermodynamic charts were indicative of non-modular arithmetic of maximum indexes and maximum conditional instability with maximum precipitation. Hence, acquaintance with synoptic conditions of systems leading to floods can be of great significance in presenting flood warnings before occurrence of any crises.
 </OtherAbstract>
		<ObjectList>
			<Object Type="keyword">
			<Param Name="value">Blocking System</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Ghare Sou basin</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">indicators of instability</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Sudanese system</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">synoptic analysis</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Thermodynamic analysis</Param>
			</Object>
		</ObjectList>
<ArchiveCopySource DocType="pdf">https://jhsci.ut.ac.ir/article_59276_2184a955f5e3f826dca976f6f7500c63.pdf</ArchiveCopySource>
</Article>
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