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<ArticleSet>
<Article>
<Journal>
				<PublisherName>University of Tehran</PublisherName>
				<JournalTitle>Earth Observation and Geomatics Engineering</JournalTitle>
				<Issn>2588-4352</Issn>
				<Volume>2</Volume>
				<Issue>1</Issue>
				<PubDate PubStatus="epublish">
					<Year>2018</Year>
					<Month>06</Month>
					<Day>01</Day>
				</PubDate>
			</Journal>
<ArticleTitle>On the use of two L1 norm minimization methods in geodetic networks</ArticleTitle>
<VernacularTitle></VernacularTitle>
			<FirstPage>1</FirstPage>
			<LastPage>8</LastPage>
			<ELocationID EIdType="pii">66945</ELocationID>
			
<ELocationID EIdType="doi">10.22059/eoge.2018.256034.1021</ELocationID>
			
			<Language>EN</Language>
<AuthorList>
<Author>
					<FirstName>Alireza</FirstName>
					<LastName>Amiri-Simkooei</LastName>
<Affiliation>Department of Geomatics Engineering, Faculty of Civil Engineering and Transportation, University of Isfahan, Isfahan, Iran</Affiliation>
<Identifier Source="ORCID">0000-0002-2952-0160</Identifier>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2017</Year>
					<Month>11</Month>
					<Day>05</Day>
				</PubDate>
			</History>
		<Abstract>&lt;span&gt;L1 norm adjustment is a powerful technique to detect gross errors in geodetic observations. This paper&lt;br /&gt;&lt;span&gt;investigates the results of two formulations that provide the L1 norm adjustment of a linear functional model.&lt;br /&gt;&lt;span&gt;The usual method for implementation of the L1 norm adjustment leads to solving a linear programming (LP)&lt;br /&gt;&lt;span&gt;problem. The formulation of the L1 norm minimization is presented based on the LP problem for a rank&lt;br /&gt;&lt;span&gt;deficient linear(ized) system of equations. Then, an alternative technique is explained based on the least&lt;br /&gt;&lt;span&gt;squares residuals. The results are tested on both linear and non-linear functional models, which confirm the&lt;br /&gt;&lt;span&gt;efficiency of both formulations. The results also indicate that the L1 norm minimization, compared to the&lt;br /&gt;&lt;span&gt;weighted least squares method, is a robust technique for the detection of blunders in geodetic observations.&lt;br /&gt;&lt;span&gt;Finally, this contribution presents a data snooping procedure to the residuals obtained by the L1 norm&lt;br /&gt;&lt;span&gt;minimization method.&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br /&gt;&lt;/span&gt;</Abstract>
		<ObjectList>
			<Object Type="keyword">
			<Param Name="value">L1 norm minimization</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Data snooping procedure</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Linear programming problem</Param>
			</Object>
		</ObjectList>
<ArchiveCopySource DocType="pdf">https://eoge.ut.ac.ir/article_66945_30a9f86bc9c7449f56c187dc57bb4494.pdf</ArchiveCopySource>
</Article>

<Article>
<Journal>
				<PublisherName>University of Tehran</PublisherName>
				<JournalTitle>Earth Observation and Geomatics Engineering</JournalTitle>
				<Issn>2588-4352</Issn>
				<Volume>2</Volume>
				<Issue>1</Issue>
				<PubDate PubStatus="epublish">
					<Year>2018</Year>
					<Month>06</Month>
					<Day>01</Day>
				</PubDate>
			</Journal>
<ArticleTitle>Automatic change detection in remotely sensed hyperspectral imagery (Case study: wetlands and waterbodies)</ArticleTitle>
<VernacularTitle></VernacularTitle>
			<FirstPage>9</FirstPage>
			<LastPage>25</LastPage>
			<ELocationID EIdType="pii">66946</ELocationID>
			
<ELocationID EIdType="doi">10.22059/eoge.2018.238510.1010</ELocationID>
			
			<Language>EN</Language>
<AuthorList>
<Author>
					<FirstName>Mahdi</FirstName>
					<LastName>Hasanlou</LastName>
<Affiliation>School of Surveying and Geospatial Engineering, College of Engineering, University of Tehran, Tehran</Affiliation>
<Identifier Source="ORCID">0000-0002-7254-4475</Identifier>

</Author>
<Author>
					<FirstName>Seyd Teymoor</FirstName>
					<LastName>Seydi</LastName>
<Affiliation>School of Surveying and Geospatial Engineering, College of Engineering, University of Tehran, Tehran</Affiliation>
<Identifier Source="ORCID">0000-0002-3678-4877</Identifier>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2017</Year>
					<Month>07</Month>
					<Day>24</Day>
				</PubDate>
			</History>
		<Abstract>&lt;span&gt;Wetlands are one of the important types of ecosystems that play a fundamental role in the environment and&lt;br /&gt;&lt;span&gt;provide significant benefits due to the resources that they contain. Therefore, it is necessary to monitor the&lt;br /&gt;&lt;span&gt;changes in these ecosystems. &lt;span&gt;The alterations in Earth’s ecosystems caused by the natural activities, such as&lt;br /&gt;&lt;span&gt;drought, as well as human activities and population growth has been affecting the wetlands and waterbodies&lt;br /&gt;&lt;span&gt;area. Therefore, for achieving a better detection of these changes over time, it is important to generate&lt;br /&gt;&lt;span&gt;descriptive location maps based on the characteristics of wetlands. Hyperspectral images have shown&lt;br /&gt;&lt;span&gt;potential use in many applications due to their high spectral resolution, and consequently, their high&lt;br /&gt;&lt;span&gt;informative value. This study presents a hybrid procedure for automatic detection of changes in wetlands&lt;br /&gt;&lt;span&gt;using a new approach which can provide more details about the changes with high accuracy. The hybrid&lt;br /&gt;&lt;span&gt;proposed method is based on incorporating chronochrome, Z-score analysis, Otsu algorithm, simplex via&lt;br /&gt;&lt;span&gt;split augmented lagrangian (SISAL), Harsanyi&lt;span&gt;–&lt;span&gt;Farrand&lt;span&gt;–&lt;span&gt;Chang (HFC), Pearson correlation coefficient&lt;br /&gt;&lt;span&gt;(PCC), and support vector machine (SVM) to detect changes using hyperspectral imagery. The proposed&lt;br /&gt;&lt;span&gt;method in the first step, produce a training data for tuning SVM and kernel parameters. The second step,&lt;br /&gt;&lt;span&gt;predicted change areas based on a chronochrome algorithm and binary change map obtained using SVM&lt;br /&gt;&lt;span&gt;classifier. The third step, the amplitude of changes is created by Z-Score analysis and binary change mask.&lt;br /&gt;&lt;span&gt;Finally, the multiple change map is produced based on the estimation of number and extraction of&lt;br /&gt;&lt;span&gt;endmembers and similarity measure. The proposed method evaluated and compared the performances with&lt;br /&gt;&lt;span&gt;other common hyperspectral change detection methods using three real-world datasets of multi-temporal&lt;br /&gt;&lt;span&gt;hyperspectral imagery. The empirical results reveal the superiority of the proposed hybrid method in&lt;br /&gt;&lt;span&gt;extracting the change map with an overall accuracy of nearly 96% and a kappa coefficient of 0.89 while&lt;br /&gt;&lt;span&gt;other hyperspectral change detection methods have the overall accuracy lower than 93% and kappa&lt;br /&gt;&lt;span&gt;coefficient 0.80. In addition, this hybrid method can provide ‘multiple changes’ as well as the magnitude of&lt;br /&gt;&lt;span&gt;extracted changes.&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br /&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;</Abstract>
		<ObjectList>
			<Object Type="keyword">
			<Param Name="value">Change detection</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Hyperspectral</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Wetlands</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Multiple-change</Param>
			</Object>
		</ObjectList>
<ArchiveCopySource DocType="pdf">https://eoge.ut.ac.ir/article_66946_cdc8b0d6dc924ba4ede94704f8446ca6.pdf</ArchiveCopySource>
</Article>

<Article>
<Journal>
				<PublisherName>University of Tehran</PublisherName>
				<JournalTitle>Earth Observation and Geomatics Engineering</JournalTitle>
				<Issn>2588-4352</Issn>
				<Volume>2</Volume>
				<Issue>1</Issue>
				<PubDate PubStatus="epublish">
					<Year>2018</Year>
					<Month>06</Month>
					<Day>01</Day>
				</PubDate>
			</Journal>
<ArticleTitle>Numerical determination of the geodesic curves: the solution of a two-point boundary value problem</ArticleTitle>
<VernacularTitle></VernacularTitle>
			<FirstPage>26</FirstPage>
			<LastPage>35</LastPage>
			<ELocationID EIdType="pii">66947</ELocationID>
			
<ELocationID EIdType="doi">10.22059/eoge.2018.257564.1023</ELocationID>
			
			<Language>EN</Language>
<AuthorList>
<Author>
					<FirstName>Mohammad Reza</FirstName>
					<LastName>Seif</LastName>
<Affiliation>Department of Surveying Engineering, Arak University of Technology, Arak, Iran</Affiliation>

</Author>
<Author>
					<FirstName>Emad</FirstName>
					<LastName>Ghalenoei</LastName>
<Affiliation>Department of Geomatics Engineering, University of Calgary, Calgary, Alberta, Canada</Affiliation>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2017</Year>
					<Month>10</Month>
					<Day>20</Day>
				</PubDate>
			</History>
		<Abstract>&lt;span&gt;In this paper, we suggest a simple iterative method to find the geodesic path on a surface parameterized by&lt;br /&gt;&lt;span&gt;orthogonal curvilinear system between two given points based on solving Boundary Value Problem. In this&lt;br /&gt;&lt;span&gt;supposed method, an iterative algorithm is used for finding the sufficient initial values as the destination&lt;br /&gt;&lt;span&gt;point agree with the boundary conditions. Geodesic determination between two given points is formulated&lt;br /&gt;&lt;span&gt;for a general surface, and specially tested for reference ellipsoid which has many applications in&lt;br /&gt;&lt;span&gt;geosciences and geodesy. Accuracy of the method is independent on the distant between two points on the&lt;br /&gt;&lt;span&gt;surface. Moreover, it can be used in aviation and sailings for finding the shortest path between start and&lt;br /&gt;&lt;span&gt;destination points.&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br /&gt;&lt;/span&gt;</Abstract>
		<ObjectList>
			<Object Type="keyword">
			<Param Name="value">Geodesic</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">geodetic computation</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Boundary Value Problem</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Reference ellipsoid</Param>
			</Object>
		</ObjectList>
<ArchiveCopySource DocType="pdf">https://eoge.ut.ac.ir/article_66947_b329ce8007bd614cdd6f213f2e08792b.pdf</ArchiveCopySource>
</Article>

<Article>
<Journal>
				<PublisherName>University of Tehran</PublisherName>
				<JournalTitle>Earth Observation and Geomatics Engineering</JournalTitle>
				<Issn>2588-4352</Issn>
				<Volume>2</Volume>
				<Issue>1</Issue>
				<PubDate PubStatus="epublish">
					<Year>2018</Year>
					<Month>06</Month>
					<Day>01</Day>
				</PubDate>
			</Journal>
<ArticleTitle>Extraction of ground points from LiDAR data based on slope and progressive window thresholding (SPWT)</ArticleTitle>
<VernacularTitle></VernacularTitle>
			<FirstPage>36</FirstPage>
			<LastPage>44</LastPage>
			<ELocationID EIdType="pii">66949</ELocationID>
			
<ELocationID EIdType="doi">10.22059/eoge.2018.240284.1012</ELocationID>
			
			<Language>EN</Language>
<AuthorList>
<Author>
					<FirstName>Pejman</FirstName>
					<LastName>Rashidi</LastName>
<Affiliation>School of Surveying and Geospatial Engineering, College of Engineering, University of Tehran,</Affiliation>

</Author>
<Author>
					<FirstName>Heidar</FirstName>
					<LastName>Rastiveis</LastName>
<Affiliation>School of Surveying and Geospatial Engineering, College of Engineering, University of Tehran, Tehran, Iran</Affiliation>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2017</Year>
					<Month>08</Month>
					<Day>22</Day>
				</PubDate>
			</History>
		<Abstract>&lt;span&gt;Filtering of airborne LiDAR point clouds has broad applications, such as Digital Terrain Model (DTM)&lt;br /&gt;&lt;span&gt;generation and three-dimensional urban modeling. Although several methods have been developed to&lt;br /&gt;&lt;span&gt;separate the point clouds into ground and non-ground points, there are some challenges to identify the&lt;br /&gt;&lt;span&gt;complex objects such as bridge and eccentric roofs. In this study, a new algorithm based on the Slope and&lt;br /&gt;&lt;span&gt;Progressive Window Thresholding (SPWT) is proposed for ground filtering of LiDAR data. This algorithm&lt;br /&gt;&lt;span&gt;is based on both multi-scale and slope methods that have strong effects on filtering the LiDAR data. The&lt;br /&gt;&lt;span&gt;proposed algorithm utilizes the slope between adjacent points and the elevation information of points in a&lt;br /&gt;&lt;span&gt;local window to detect non-ground objects. Therefore, not only it benefits from vertical information in each&lt;br /&gt;&lt;span&gt;local window to detect the non-ground points, but it also uses the neighbor information in directional&lt;br /&gt;&lt;span&gt;scanning, and it prevents the errors introduced by the sensitivity to direction. According to the physical&lt;br /&gt;&lt;span&gt;characteristics of the ground surface and the size of objects, the best threshold values are considered. In&lt;br /&gt;&lt;span&gt;order to evaluate the performance of the SPWT method, both low and high resolution datasets were applied&lt;br /&gt;&lt;span&gt;that their average overall accuracy were reported to be 94.21% and 93.08%, respectively. These results&lt;br /&gt;&lt;span&gt;proved that, irrespective of data resolution, the SPWT method could effectively remove the non-ground&lt;br /&gt;&lt;span&gt;points from airborne LiDAR data.&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br /&gt;&lt;/span&gt;</Abstract>
		<ObjectList>
			<Object Type="keyword">
			<Param Name="value">Ground Filtering</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">LiDAR</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Points Cloud</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">DEM Generation</Param>
			</Object>
		</ObjectList>
<ArchiveCopySource DocType="pdf">https://eoge.ut.ac.ir/article_66949_a301201e2ef370952b865591469f1b37.pdf</ArchiveCopySource>
</Article>

<Article>
<Journal>
				<PublisherName>University of Tehran</PublisherName>
				<JournalTitle>Earth Observation and Geomatics Engineering</JournalTitle>
				<Issn>2588-4352</Issn>
				<Volume>2</Volume>
				<Issue>1</Issue>
				<PubDate PubStatus="epublish">
					<Year>2018</Year>
					<Month>06</Month>
					<Day>01</Day>
				</PubDate>
			</Journal>
<ArticleTitle>Assessing the impact of cold and warm ENSO on drought over Iran</ArticleTitle>
<VernacularTitle></VernacularTitle>
			<FirstPage>45</FirstPage>
			<LastPage>55</LastPage>
			<ELocationID EIdType="pii">66950</ELocationID>
			
<ELocationID EIdType="doi">10.22059/eoge.2018.257714.1022</ELocationID>
			
			<Language>EN</Language>
<AuthorList>
<Author>
					<FirstName>Zahir</FirstName>
					<LastName>Nikraftar</LastName>
<Affiliation>Department of Geomatics Engineering, Shahid Rajaee Teacher Training University, Tehran, Iran</Affiliation>

</Author>
<Author>
					<FirstName>Ali</FirstName>
					<LastName>Sam-Khaniani</LastName>
<Affiliation>Babol Noshirvani University of Technology, Civil Engineering Department, P.O.Box 484, Shariati Ave, Babol,Mazandaran 47148-71167, Iran</Affiliation>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2017</Year>
					<Month>12</Month>
					<Day>01</Day>
				</PubDate>
			</History>
		<Abstract>&lt;span&gt;The impacts of El Niño Southern Oscillation (ENSO) on climate change and in the global scale are well&lt;br /&gt;&lt;span&gt;known, and have attracted the attention of researchers since the twentieth century. The study of ENSO&lt;br /&gt;&lt;span&gt;impact on climate using precipitation and near surface temperature data from re-analysis products makes&lt;br /&gt;&lt;span&gt;global and long-term analyses of this phenomenon possible. The common method to analyze the ENSO&lt;br /&gt;&lt;span&gt;impact is to quantify the probability of extreme drought occurrences when the surface temperatures of&lt;br /&gt;&lt;span&gt;central-east equatorial Pacific sea are abnormal. Although the results are always uncertain due to the&lt;br /&gt;&lt;span&gt;complexity of atmospheric teleconnections, application of the recently available gridded datasets helps one&lt;br /&gt;&lt;span&gt;to conduct more precise modeling and predictions. Spatiotemporal patterns of ENSO impact from 1980 to&lt;br /&gt;&lt;span&gt;the end of 2013 for four ENSO indices (e.g. Nino 3.4, MEI, ONI, SOI) over Iran was investigated in this&lt;br /&gt;&lt;span&gt;study. Spatial maps of the Pearson correlation coefficients and a composite analysis were obtained between&lt;br /&gt;&lt;span&gt;the GPCC precipitation and temperature dataset with ENSO states. In addition, the frequency maps of&lt;br /&gt;&lt;span&gt;extreme drought conditions during ENSO states were acquired. The results show that the western (along the&lt;br /&gt;&lt;span&gt;range of Zagros Mountain) and northern (along the Alborz Mountain and the coastlines of the Caspian Sea&lt;br /&gt;&lt;span&gt;to Khorasan Province) regions are more affected by ENSO events. The Pearson correlation coefficient for&lt;br /&gt;&lt;span&gt;all four ENSO indices over the mentioned regions was determined to be about 0.70 for precipitation datasets&lt;br /&gt;&lt;span&gt;and -0.70 for temperature datasets. The frequency analysis of extreme drought based and CZI (Chinese Z&lt;br /&gt;&lt;span&gt;Index) and ENSO phases shows that the western and northeast parts of Iran are more affected by centraleast equatorial Pacific teleconnections. Composite analysis for all four ENSO indices shows the precipitation&lt;br /&gt;&lt;span&gt;(over the rainy months)/temperature (over the summer months) anomalies, for the El Niño states about +25&lt;br /&gt;&lt;span&gt;(mm)/ -0.5˚ (C) and for the La Niña states about -25 (mm)/+0.6˚ to 1˚ (C).&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br /&gt;&lt;/span&gt;</Abstract>
		<ObjectList>
			<Object Type="keyword">
			<Param Name="value">Southern Oscillation Index</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Climate</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">GPCC datasets</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Chinese Z Index</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Teleconnectios</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Composite analysis</Param>
			</Object>
		</ObjectList>
<ArchiveCopySource DocType="pdf">https://eoge.ut.ac.ir/article_66950_1a455a59e5fb212b5d6ce937cdbc2b80.pdf</ArchiveCopySource>
</Article>

<Article>
<Journal>
				<PublisherName>University of Tehran</PublisherName>
				<JournalTitle>Earth Observation and Geomatics Engineering</JournalTitle>
				<Issn>2588-4352</Issn>
				<Volume>2</Volume>
				<Issue>1</Issue>
				<PubDate PubStatus="epublish">
					<Year>2018</Year>
					<Month>06</Month>
					<Day>01</Day>
				</PubDate>
			</Journal>
<ArticleTitle>A comparison of four methods for extracting Land Surface Emissivity and Temperature in the Thermal Infrared Hyperspectral Data</ArticleTitle>
<VernacularTitle></VernacularTitle>
			<FirstPage>56</FirstPage>
			<LastPage>63</LastPage>
			<ELocationID EIdType="pii">66951</ELocationID>
			
<ELocationID EIdType="doi">10.22059/eoge.2018.239666.1011</ELocationID>
			
			<Language>EN</Language>
<AuthorList>
<Author>
					<FirstName>Faeze</FirstName>
					<LastName>Soleimani Vosta Kolaei</LastName>
<Affiliation>School of Surveying and Geospatial Engineering, College of Engineering, University of Tehran, Tehran, Iran</Affiliation>

</Author>
<Author>
					<FirstName>Mehdi</FirstName>
					<LastName>Akhoondzadeh</LastName>
<Affiliation>School of Surveying and Geospatial Engineering, College of Engineering, University of Tehran, Tehran, Iran</Affiliation>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2017</Year>
					<Month>08</Month>
					<Day>12</Day>
				</PubDate>
			</History>
		<Abstract>&lt;span&gt;Land Surface Temperature (LST) and Land Surface Emissivity (LSE) are two important physical properties&lt;br /&gt;&lt;span&gt;of Earth&#039;s surface. LST retrieval plays a valuable role in environmental studies. Therefore, in order to&lt;br /&gt;&lt;span&gt;estimate LST accurately, it is necessary to obtain LSEs. The HyTES (Hyperspectral Thermal Emission&lt;br /&gt;&lt;span&gt;Spectrometer) instrument has 256 spectral bands covering the thermal infrared (TIR) spectral range. Due to&lt;br /&gt;&lt;span&gt;a large number of narrow bandwidths of HyTES, this sensor can produce the accurate LST and LSEs. The&lt;br /&gt;&lt;span&gt;main goal of this paper is to evaluate the accuracy of LSE and LST retrieval methods from HyTES data and&lt;br /&gt;&lt;span&gt;to improve the accuracy of the Normalization (NOR) method. For this purpose, four different methods have&lt;br /&gt;&lt;span&gt;been considered to retrieve LSE: (i) the Reference Channel method (REF), (ii) the Emissivity Normalization&lt;br /&gt;&lt;span&gt;method, (iii) the Alpha emissivity method (AlPHA) and (iv) a method to improve the NOR algorithm. The&lt;br /&gt;&lt;span&gt;first three methods have been widely used with thermal multispectral data in other researches. These&lt;br /&gt;&lt;span&gt;methods were used with HyTES hyperspectral data in this paper; the fourth is a new method that improved&lt;br /&gt;&lt;span&gt;the accuracy of the NOR method. The results of quality assessment show that the emissivity RMSEs of the&lt;br /&gt;&lt;span&gt;REF, NOR, ALPHA methods and the new proposed method are 0.021, 0.815, 0.034 and 0.0201,&lt;br /&gt;&lt;span&gt;respectively. Also, LST RMSEs of the REF and NOR methods are less than 1.5 K.&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br /&gt;&lt;/span&gt;</Abstract>
		<ObjectList>
			<Object Type="keyword">
			<Param Name="value">LSE</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">HyTES</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">REF</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">ALPHA</Param>
			</Object>
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<ArchiveCopySource DocType="pdf">https://eoge.ut.ac.ir/article_66951_fe70e659d72db7250c46906baa6e8a0b.pdf</ArchiveCopySource>
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