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<!DOCTYPE ArticleSet PUBLIC "-//NLM//DTD PubMed 2.7//EN" "https://dtd.nlm.nih.gov/ncbi/pubmed/in/PubMed.dtd">
<ArticleSet>
<Article>
<Journal>
				<PublisherName>University of Tabriz</PublisherName>
				<JournalTitle>Water and Soil Science</JournalTitle>
				<Issn>2008-5133</Issn>
				<Volume>21</Volume>
				<Issue>1</Issue>
				<PubDate PubStatus="epublish">
					<Year>2014</Year>
					<Month>04</Month>
					<Day>30</Day>
				</PubDate>
			</Journal>
<ArticleTitle>Comparsion of Hybrid and Nash Models for Derivation of Instantaneous Unit Hydrograph (Case Study: Lighvan Watershed)</ArticleTitle>
<VernacularTitle>Comparsion of Hybrid and Nash Models for Derivation of Instantaneous Unit Hydrograph (Case Study: Lighvan Watershed)</VernacularTitle>
			<FirstPage>29</FirstPage>
			<LastPage>41</LastPage>
			<ELocationID EIdType="pii">1243</ELocationID>
			
			
			<Language>FA</Language>
<AuthorList>
<Author>
					<FirstName>A</FirstName>
					<LastName>Ahmadin</LastName>
<Affiliation></Affiliation>

</Author>
<Author>
					<FirstName>A</FirstName>
					<LastName>Fakheri  Fard</LastName>
<Affiliation></Affiliation>

</Author>
<Author>
					<FirstName>MA</FirstName>
					<LastName>Gorbani</LastName>
<Affiliation></Affiliation>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2014</Year>
					<Month>04</Month>
					<Day>30</Day>
				</PubDate>
			</History>
		<Abstract>In the Nash model, the number of reservoirs and storage coefficient describe the complete shape of &lt;em&gt;IUH&lt;/em&gt;. In this model, the number of reservoirs which should be an integer values is generally a fractional value when derived from the observed data, and that is a major limitation for the model. Furthermore, a single linear reservoir of the Nash model yields an &lt;em&gt;IUH&lt;/em&gt; without a rising limb which is physically unrealistic. To simulate a complete &lt;em&gt;IUH &lt;/em&gt;with rising limb, the Nash model requires a minimum of two reservoirs connected in series. Splitting the Nash single linear reservoir into two serially connected reservoirs of unequal storage coefficients K&lt;sub&gt;1 &lt;/sub&gt;andK&lt;sub&gt;2&lt;/sub&gt; (one hybrid unit), a hybrid model is introduced for derivation of a synthetic unit hydrograph. In this study,the Lighvan watershed was considered for application of the hybrid model. To exhibit the applicability of  the hybrid model, the results, are compared with the Nash model results, using &lt;em&gt;STDER&lt;/em&gt; and Nash-Satkolif output model values. The present approach yields &lt;em&gt;STDER&lt;/em&gt; values lower and Nash-Satkolif output model values higher than those of the Nash method. Thus, the present approach performs better than the Nash method.
 </Abstract>
			<OtherAbstract Language="FA">In the Nash model, the number of reservoirs and storage coefficient describe the complete shape of &lt;em&gt;IUH&lt;/em&gt;. In this model, the number of reservoirs which should be an integer values is generally a fractional value when derived from the observed data, and that is a major limitation for the model. Furthermore, a single linear reservoir of the Nash model yields an &lt;em&gt;IUH&lt;/em&gt; without a rising limb which is physically unrealistic. To simulate a complete &lt;em&gt;IUH &lt;/em&gt;with rising limb, the Nash model requires a minimum of two reservoirs connected in series. Splitting the Nash single linear reservoir into two serially connected reservoirs of unequal storage coefficients K&lt;sub&gt;1 &lt;/sub&gt;andK&lt;sub&gt;2&lt;/sub&gt; (one hybrid unit), a hybrid model is introduced for derivation of a synthetic unit hydrograph. In this study,the Lighvan watershed was considered for application of the hybrid model. To exhibit the applicability of  the hybrid model, the results, are compared with the Nash model results, using &lt;em&gt;STDER&lt;/em&gt; and Nash-Satkolif output model values. The present approach yields &lt;em&gt;STDER&lt;/em&gt; values lower and Nash-Satkolif output model values higher than those of the Nash method. Thus, the present approach performs better than the Nash method.
 </OtherAbstract>
		<ObjectList>
			<Object Type="keyword">
			<Param Name="value">Hybrid model</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Unit hydrograph</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Nash model</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Storage reservoirs</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Lighvan watershed</Param>
			</Object>
		</ObjectList>
<ArchiveCopySource DocType="pdf">https://water-soil.tabrizu.ac.ir/article_1243_7acc640ba0343bc26c8042fac68f7b5f.pdf</ArchiveCopySource>
</Article>
</ArticleSet>
