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Determination of turbidity in Kourris Dam in Cyprus utilizing Landsat TM remotely sensed data.

Determination of turbidity in Kourris Dam in Cyprus utilizing Landsat TM remotely sensed data.
Determination of turbidity in Kourris Dam in Cyprus utilizing Landsat TM remotely sensed data.
Determination 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 the Kourris 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.
dams, earth observation, linear regression, spectral characteristics, turbidity, water quality
0920-4741
449-465
Hadjimitsis, D.G.
273ac886-343c-49d6-8810-b542cecc3fa1
Hadjimitsis, M.G.
ef0e8ffa-eca8-4529-ae64-399528eb5fe5
Clayton, C.
8397d691-b35b-4d3f-a6d8-40678f233869
Clarke, B.A.
999f9efe-bc38-4130-a5a2-7a95d5856316
Hadjimitsis, D.G.
273ac886-343c-49d6-8810-b542cecc3fa1
Hadjimitsis, M.G.
ef0e8ffa-eca8-4529-ae64-399528eb5fe5
Clayton, C.
8397d691-b35b-4d3f-a6d8-40678f233869
Clarke, B.A.
999f9efe-bc38-4130-a5a2-7a95d5856316

Hadjimitsis, D.G., Hadjimitsis, M.G., Clayton, C. and Clarke, B.A. (2006) Determination of turbidity in Kourris Dam in Cyprus utilizing Landsat TM remotely sensed data. Water Resources Management, 20 (3), 449-465. (doi:10.1007/s11269-006-3089-y).

Record type: Article

Abstract

Determination 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 the Kourris 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.

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More information

Submitted date: January 2005
Published date: June 2006
Additional Information: Hadjimitsis D.G., Hadjimitsis MG, Clayton C. R. I., Clarke BA, (2006). "Determination of turbidity in Kourris Dam in Cyprus utilizing Landsat TM remotely sensed data.." Water Resources Management, 20, 3, 449-465
Keywords: dams, earth observation, linear regression, spectral characteristics, turbidity, water quality

Identifiers

Local EPrints ID: 53372
URI: http://eprints.soton.ac.uk/id/eprint/53372
ISSN: 0920-4741
PURE UUID: e799045a-74f0-4eb7-bc1c-a96e3269b9fe
ORCID for C. Clayton: ORCID iD orcid.org/0000-0003-0071-8437

Catalogue record

Date deposited: 22 Jul 2008
Last modified: 16 Mar 2024 03:12

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Contributors

Author: D.G. Hadjimitsis
Author: M.G. Hadjimitsis
Author: C. Clayton ORCID iD
Author: B.A. Clarke

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