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<Article>
<Journal>
				<PublisherName>University of Tehran Press</PublisherName>
				<JournalTitle>Desert</JournalTitle>
				<Issn>2008-0875</Issn>
				<Volume>10</Volume>
				<Issue>1</Issue>
				<PubDate PubStatus="epublish">
					<Year>2005</Year>
					<Month>12</Month>
					<Day>01</Day>
				</PubDate>
			</Journal>
<ArticleTitle>DIURNAL BEHAVIOR OF LAND SURFACE TEMPERATURE IN LUT DESERT</ArticleTitle>
<VernacularTitle></VernacularTitle>
			<FirstPage>19</FirstPage>
			<LastPage>28</LastPage>
			<ELocationID EIdType="pii">31878</ELocationID>
			
<ELocationID EIdType="doi">10.22059/jdesert.2005.31878</ELocationID>
			
			<Language>EN</Language>
<AuthorList>
<Author>
					<FirstName>S. K.</FirstName>
					<LastName>Alavipanah</LastName>
<Affiliation>Associate Prof,Faculty of Geography,University of Tehran</Affiliation>

</Author>
<Author>
					<FirstName>A. A.</FirstName>
					<LastName>Shamsipour</LastName>
<Affiliation>Ph.D. Canditate,Faculty of Geography,University of Tehran</Affiliation>

</Author>
<Author>
					<FirstName>M.</FirstName>
					<LastName>Jafer Beglo</LastName>
<Affiliation>Associate Prof,Faculty of Geography.University of Tehran</Affiliation>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2014</Year>
					<Month>07</Month>
					<Day>02</Day>
				</PubDate>
			</History>
		<Abstract>analyses and thermal infrared channels 4 and 5 NOAA- AVHRR images. &lt;br /&gt;This research was carried out in Lut Desert located in center of sub-tropical divergence dominant in&#039; Iranian &lt;br /&gt;plateau. The physical and thermal properties of the various desert surfaces have been determined using &lt;br /&gt;correlation relationships between the desert variables including: dark sand, normal sand, marl, saline soil, soil &lt;br /&gt;depth (10 cm), wet and dry bulb temperature in daytimes with the interval of two hours from 6 AM to 20 P.M &lt;br /&gt;within 15 days. &lt;br /&gt;The result shows that thermal conductivity, thermal capacity, physico-chemical properties of the studied &lt;br /&gt;materials and other thermal properties, are the most important factors affecting correlation coefficients. The &lt;br /&gt;highest correlation obtained around the sunrise (6 AM) and especially before and after the sunset (18, 20 &lt;br /&gt;P.M). Minimum correlations were obtained around the noon at soil depth and the best fitted models are linear &lt;br /&gt;for light sand and marl in 18, 20 P.M and non-linear for soil depth and marl in 18 P.M. Therefore it is generally &lt;br /&gt;concluded that the study of diurnal behavior of land surface temperatures might be useful for thermal image &lt;br /&gt;interpretation.</Abstract>
<ArchiveCopySource DocType="pdf">https://jdesert.ut.ac.ir/article_31878_c9983db52a1a36f441f30c5412feff81.pdf</ArchiveCopySource>
</Article>
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