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<Article>
<Journal>
				<PublisherName>Gorgan University of Agricultural Sciences</PublisherName>
				<JournalTitle>International Journal of Plant Production</JournalTitle>
				<Issn>1735-6814</Issn>
				<Volume>6</Volume>
				<Issue>2</Issue>
				<PubDate PubStatus="epublish">
					<Year>2012</Year>
					<Month>08</Month>
					<Day>11</Day>
				</PubDate>
			</Journal>
<ArticleTitle>Regional climate change scenarios and their impacts on
water requirements for wheat production in Iran</ArticleTitle>
<VernacularTitle></VernacularTitle>
			<FirstPage>239</FirstPage>
			<LastPage>266</LastPage>
			<ELocationID EIdType="pii">778</ELocationID>
			
<ELocationID EIdType="doi">10.22069/ijpp.2012.778</ELocationID>
			
			<Language>EN</Language>
<AuthorList>
<Author>
					<FirstName>Gh.R.</FirstName>
					<LastName>Roshan</LastName>
<Affiliation>Department of Geography, Golestan University, Gorgan, Iran.</Affiliation>

</Author>
<Author>
					<FirstName>S.W.</FirstName>
					<LastName>Grab</LastName>
<Affiliation>School of Geography, Archaeology and Environmental Studies, University of Witwatersrand, South Africa.</Affiliation>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2012</Year>
					<Month>08</Month>
					<Day>11</Day>
				</PubDate>
			</History>
		<Abstract>We simulate the effect of climate change on water requirements of cold season&lt;br /&gt;wheat in various climatic zones of Iran. The research considers both observed&lt;br /&gt;climate (temperature and precipitation) changes during recent decades (1960-2009)&lt;br /&gt;based on instrumental records and projected future changes to 2100 based on the&lt;br /&gt;MAGICC/SCENGEN 5.3 compound model. 20 General Circulation models are used&lt;br /&gt;based on a single scenario known as P50, which is the average of SRES or emission&lt;br /&gt;scenarios. Results indicate that whilst winter precipitation has marginally increased&lt;br /&gt;across the country as a whole, a significant decline in mean spring precipitation is&lt;br /&gt;recorded between 1960 and 2009. However, considerable variability in trends is&lt;br /&gt;measured across various climatic regions of Iran. Mean annual temperature / rainfall&lt;br /&gt;changes in the various climate zones of Iran for the period 1960-2009 follow: +0.1 °C&lt;br /&gt;/ decade / +0.43 mm / decade in arid regions, -0.1 °C / decade / -1.7 mm / decade in&lt;br /&gt;semi-arid regions, +0.1 °C / decade / -1.33 mm / decade in Mediterranean / semihumid&lt;br /&gt;regions and -0.01 °C / decade / -0.04 mm / decade in humid / hyper humid&lt;br /&gt;regions. Temperature projections to 2100 indicate an overall temperature rise of ca.&lt;br /&gt;4.25 °C relative to that for 1961-1990, with increases projected for all climatic&lt;br /&gt;regions of Iran. Despite an overall projected mean precipitation increase of 36% for&lt;br /&gt;the year 2100, relative to that for 1961-1990, these are insufficient to compensate for&lt;br /&gt;temperature increases. Consequently, calculated water deficits during the growing&lt;br /&gt;season (autumn to spring) in Iran’s wheat producing areas are expected to increase&lt;br /&gt;from 5.2% in 1980 to over 23% by 2050 and 38% by 2100.</Abstract>
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<ArchiveCopySource DocType="pdf">https://ijpp.gau.ac.ir/article_778_ae28ecee2a64b34fc54abf185a3fb8c0.pdf</ArchiveCopySource>
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