2014
DOI: 10.1016/j.csr.2014.05.013
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Modelling the inherent optical properties and estimating the constituents׳ concentrations in turbid and eutrophic waters

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Cited by 24 publications
(14 citation statements)
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“…Therefore, to improve the ocean colour estimates, it is essential to develop the robust regional algorithms for the coastal waters. An accurate estimation of ocean colour of bio-optical variables in the complex coastal waters is still a challenging task (Gokul et al, 2014). The bio-optical properties of the coastal water bodies are understudied (Tilstone et al, 2013;Ferreira et al, 2014) due to the optical complexity of the waters.…”
Section: Introductionmentioning
confidence: 99%
“…Therefore, to improve the ocean colour estimates, it is essential to develop the robust regional algorithms for the coastal waters. An accurate estimation of ocean colour of bio-optical variables in the complex coastal waters is still a challenging task (Gokul et al, 2014). The bio-optical properties of the coastal water bodies are understudied (Tilstone et al, 2013;Ferreira et al, 2014) due to the optical complexity of the waters.…”
Section: Introductionmentioning
confidence: 99%
“…This bio‐optical algorithm was demonstrated to be very effective in terms of accurate estimation of chlorophyll and discriminating algal bloom patches in coastal waters rather than using global algorithms (e.g., OC3 and OC4v4). Inherent optical properties such as absorption ( a ( λ ) = a w ( λ )+ a p ( λ )+ a cdom ( λ )) and backscattering ( b b ( λ ) = b w ( λ )+ b p ( λ )) were derived from the existing models [ Shanmugam et al ., ; Gokul et al ., ; Varunan and Shanmugam , ; Sundarabalan and Shanmugam , ]. The pure water absorption and backscattering coefficients were added with these particulate terms to obtain the respective total absorption and backscattering coefficients.…”
Section: Methodsmentioning
confidence: 99%
“…The predictive model takes the form as, acdom/d=acdom/d(λr)×eS(λλr) where λ r is the reference wavelength at 443 nm and S is the spectral slope coefficient (nm −1 ). The a d ( 443 ) and a cdom ( 443 ) values are estimated by empirical methods [ Gokul et al ., ] that relate to the remote sensing reflectance in equations and , ad(443)=0.3314×true(Rrstrue(620true)Rrs(490)true)1.516 acdom(443)=0.1005×true(Rrstrue(555true)Rrs(443)true)1.4499 …”
Section: Approachmentioning
confidence: 99%
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“…The concentration of water constituents can fluctuate significantly over a short time period, making it necessary to continuously monitor bodies of water [1]. Unlike in situ campaigns that provide point measurements, remote sensing techniques can detect the spatial and temporal variation in water bodies [2][3][4].…”
Section: Introductionmentioning
confidence: 99%