Please use this identifier to cite or link to this item: https://hdl.handle.net/20.500.14279/1342
DC FieldValueLanguage
dc.contributor.authorClarke, Brian A.-
dc.contributor.authorClayton, Chris R I-
dc.contributor.authorHadjimitsis, Diofantos G.-
dc.contributor.authorHadjimitsis, Marinos G.-
dc.date.accessioned2009-06-02T10:56:27Zen
dc.date.accessioned2013-05-17T05:23:08Z-
dc.date.accessioned2015-12-02T10:20:13Z-
dc.date.available2009-06-02T10:56:27Zen
dc.date.available2013-05-17T05:23:08Z-
dc.date.available2015-12-02T10:20:13Z-
dc.date.issued2006-06-
dc.identifier.citationWater Resources Management, 2006, vol. 20, no. 3, pp. 449-465en_US
dc.identifier.issn15731650-
dc.identifier.urihttps://hdl.handle.net/20.500.14279/1342-
dc.description.abstractDetermination of turbidity is a common component of water-quality assessments. In regions where there are a lot of inland waters such as dams, sampling even a small proportion of those dams for monitoring and assessing water quality is cost prohibitive. Satellite remote sensing has the potential to be a powerful tool for assessing water quality over large spatial scales. The overall objective of this study was to examine whether Landsat-5 TM (Thematic Mapper) and Landsat-7 ETM+ (Enhanced Thematic Mapper) could be used to measure turbidity across theKourris Dam, which is the biggest dam in Cyprus. This paper presents the results obtained by applying the linear regression analysis in order to examine the relationship between the turbidity measurements measured in-situ during the satellite overpass against at-satellite atmospheric corrected reflectance values. It has been found that the reflectance, after atmospheric correction, at LandsatTMBands 1 and 3 is strongly related with turbidity levels after linear regression analysis. The most significant correlation was occurred when reflectance in TM band 3 and logarithmic reflectance in TM band 3 were correlated with turbidity measurements. Indeed, the correlation coefficient (R) when atmospheric corrected reflectance (ρ) in the LandsatTMband 3 were correlated against turbidity, before atmospheric correction was R = 0.38 and after atmospheric correction was R = 1; and when atmospheric corrected logarithmic reflectance (Log ρ) in the Landsat TM band 3 were correlated against turbidity, before atmospheric correction was R = 0.46 and after atmospheric correction was R = 1.en_US
dc.formatpdfen_US
dc.language.isoenen_US
dc.relation.ispartofWater Resources Managementen_US
dc.rights© Springeren_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/us/*
dc.subjectWater qualityen_US
dc.subjectTurbidityen_US
dc.subjectSpectral characteristicsen_US
dc.subjectLinear regressionen_US
dc.subjectEarth observationen_US
dc.subjectDamsen_US
dc.titleDetermination of Turbidity in Kourris Dam in Cyprus Utilizing Landsat TM Remotely Sensed Dataen_US
dc.typeArticleen_US
dc.collaborationFrederick Institute of Technologyen_US
dc.subject.categoryEarth and Related Environmental Sciencesen_US
dc.journalsHybrid Open Accessen_US
dc.countryCyprusen_US
dc.subject.fieldNatural Sciencesen_US
dc.publicationPeer Revieweden_US
dc.identifier.doi10.1007/s11269-006-3089-yen_US
dc.dept.handle123456789/54en
dc.relation.issue3en_US
dc.relation.volume20en_US
cut.common.academicyear2006-2007en_US
dc.identifier.spage449en_US
dc.identifier.epage465en_US
item.grantfulltextnone-
item.openairecristypehttp://purl.org/coar/resource_type/c_6501-
item.fulltextNo Fulltext-
item.languageiso639-1en-
item.cerifentitytypePublications-
item.openairetypearticle-
crisitem.journal.journalissn1573-1650-
crisitem.journal.publisherSpringer Nature-
crisitem.author.deptDepartment of Civil Engineering and Geomatics-
crisitem.author.facultyFaculty of Engineering and Technology-
crisitem.author.orcid0000-0002-2684-547X-
crisitem.author.parentorgFaculty of Engineering and Technology-
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