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<Article>
<Journal>
				<PublisherName>University of Tehran</PublisherName>
				<JournalTitle>Desert</JournalTitle>
				<Issn>2008-0875</Issn>
				<Volume>18</Volume>
				<Issue>1</Issue>
				<PubDate PubStatus="epublish">
					<Year>2013</Year>
					<Month>01</Month>
					<Day>01</Day>
				</PubDate>
			</Journal>
<ArticleTitle>Spatial Analysis of Meteorological Drought in Iran from 1965 to2003</ArticleTitle>
<VernacularTitle></VernacularTitle>
			<FirstPage>63</FirstPage>
			<LastPage>71</LastPage>
			<ELocationID EIdType="pii">36276</ELocationID>
			
<ELocationID EIdType="doi">10.22059/jdesert.2013.36276</ELocationID>
			
			<Language>EN</Language>
<AuthorList>
<Author>
					<FirstName>J.</FirstName>
					<LastName>Bazrafshan</LastName>
<Affiliation>Irrigation and Reclamation Engineering Department, University of Tehran, Iran</Affiliation>

</Author>
<Author>
					<FirstName>A.</FirstName>
					<LastName>Khalili</LastName>
<Affiliation>Irrigation and Reclamation Engineering Department, University of Tehran, Iran</Affiliation>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2013</Year>
					<Month>02</Month>
					<Day>23</Day>
				</PubDate>
			</History>
		<Abstract>The present study examined year-to-year variations in areas affected by drought during a period of 39 water years&lt;br /&gt;in Iran. Ninety-five meteorological stations were chosen to provide near-continuous long-term records, although&lt;br /&gt;some data was missing (less than 10%). The missing data points were estimated using a linear correlation method&lt;br /&gt;between the reference station with the missing data points and a neighboring station that had a complete record. At all&lt;br /&gt;stations, the standard index of annual precipitation (SIAP) was calculated for water year (sum of precipitation from&lt;br /&gt;October 1 to September 31). The geo-statistical method of weighting moving average (WMA) was applied to a 2×2&lt;br /&gt;km grid network map of Iran and the geographical distribution of SIAP was calculated and displayed. From this, the&lt;br /&gt;percentage of area affected by severe, moderate, and mild drought was computed for each year; the frequency of&lt;br /&gt;drought was analyzed by severity and the behaviors of the most extensive historical droughts were determined. The&lt;br /&gt;results showed that: a) the maximum frequency of severe drought was 5.1 times and moderate drought was 23.1 times&lt;br /&gt;per 100 years; b) the most extensive droughts (more than 80% of the country) occurred during 1970-1971 (82.21%),&lt;br /&gt;1988-1989 (92.05%), and 1999-2000 (96.27%); and c) drought spread in Iran beginning from the northwestern and&lt;br /&gt;southeastern regions, gradually extending to the central regions.</Abstract>
		<ObjectList>
			<Object Type="keyword">
			<Param Name="value">Drought</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Severity</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">extent</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Geo-Statistics</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Iran</Param>
			</Object>
		</ObjectList>
<ArchiveCopySource DocType="pdf">https://jdesert.ut.ac.ir/article_36276_b25d8a53280855e5a10ceedcdda64ed2.pdf</ArchiveCopySource>
</Article>
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