2018
DOI: 10.1109/tgrs.2018.2849026
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An Optical Algorithm to Estimate Downwelling Diffuse Attenuation Coefficient in the Red Sea

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Cited by 11 publications
(14 citation statements)
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“…This parameter was also regarded as better than SST to represent the photosynthetic rate of VGPM model in the Southern Sea [100]. As a good indicator of phytoplankton growth, KD490 can show short-term phytoplankton blooms and physical processes (anticyclonic and cyclonic eddies) in the Red Sea [102]. The absorption-based models using remotely sensed data could minimize the impacts of pigment packaging, colored dissolved organic matter (CDOM), and non-algal matter, in order to reach both lower bias and higher standard deviation evaluated by in situ datasets in the Arctic Ocean [103].…”
Section: Discussionmentioning
confidence: 99%
“…This parameter was also regarded as better than SST to represent the photosynthetic rate of VGPM model in the Southern Sea [100]. As a good indicator of phytoplankton growth, KD490 can show short-term phytoplankton blooms and physical processes (anticyclonic and cyclonic eddies) in the Red Sea [102]. The absorption-based models using remotely sensed data could minimize the impacts of pigment packaging, colored dissolved organic matter (CDOM), and non-algal matter, in order to reach both lower bias and higher standard deviation evaluated by in situ datasets in the Arctic Ocean [103].…”
Section: Discussionmentioning
confidence: 99%
“…variables including CHL, suspended particles, nutrients and oxygen demonstrate the coupling between various scales of physical forcing and variability with biogeochemical dynamics (e.g Mahadevan et al 2012;Mignot et al 2014). The use of bio-optical variables from both remote sensing and in-situ observations has yielded new insights into the biogeochemical functioning of Red Sea (Acker et al 2008;Brewin et al 2015;Gittings et al 2018;Racault et al 2015;Raitsos et al 2013;Tiwari et al 2018b;Zarokanellos et al 2017b;Kheireddine et al 2020) In a phytoplankton dominated regime a number of optical properties will covary with CHL concentration (Bricaud et al 1988;Siegel et al 2005), but other non-algal constituents are capable of absorbing and scattering light, such as detrital particles, CDOM, and suspended solids, which all contribute independently to ocean color (Loisel et al 2002(Loisel et al , 2007Maritorena and Siegel 2005;Tiwari et al 2018a). The present study aims to address the influence of wind mixing, mesoscale eddies, and lateral advection on the optical properties.…”
Section: Accepted Articlementioning
confidence: 99%
“…In a phytoplankton dominated regime, many optical properties will covary with CHL concentration (Bricaud et al., 1988; Siegel et al., 2005), but other nonalgal constituents are capable of absorbing and scattering light, such as detrital particles, CDOM, and suspended solids, which all contribute independently to ocean color (Loisel et al., 2002, 2007; Maritorena & Siegel, 2005; Tiwari, Sarma, et al., 2018). This study aims to address the influence of wind mixing, mesoscale eddies, and lateral advection on optical properties.…”
Section: Introductionmentioning
confidence: 99%
“…Following [66], accuracy assessments of the algorithms are presented through standard statistical errors (root mean square error (RMSE), bias (ψ), the mean absolute percentage difference (|ψ|)), and the linear regression (i.e., slope, intercept, and coefficient of determination (R 2 )). Mathematically, the value of ψ is derived from the following:…”
Section: Model Accuracy Assessmentmentioning
confidence: 99%