Deriving inherent optical properties from water color: a multiband quasi-analytical algorithm for optically deep waters.

By Z. Lee, K. Carder, Robert Arnone. Applied Optics, 2002

1,627 citations recorded by the source corpus.

Subfields: Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/c0716255965a355245757132919a55956bab791f

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Citations in the corpus

Particle optical backscattering along a chlorophyll gradient in the upper layer of the eastern South Pacific Ocean (2007, methodology): “, roughly within a factor of 2 or 3) than those for other inherent optical properties. Prior to this study, two main propositions existed that included [Chl] below 0.1 mg m−3, one formulated by Morel and Maritorena (2001) and the other by Behrenfeld et al.”
An Ocean-Colour Time Series for Use in Climate Studies: The Experience of the Ocean-Colour Climate Change Initiative (OC-CCI) (2019, methodology): “The Quasi-Analytical algorithm (QAA) of [19,67] was selected for producing the IOPs.”
Seamless retrievals of chlorophyll-a from Sentinel-2 (MSI) and Sentinel-3 (OLCI) in inland and coastal waters: A machine-learning approach (2020, background): “…relies on estimates of phytoplankton specific absorption ( a ph ∗ ) peaks within the red portions of the spectrum, e.g., a ph ∗ (670) (Gons, 1999; Lee et al., 2002; Odermatt et al., 2018; Schroeder et al., 2007) and has proven to perform sa-tisfactorily in some aquatic ecosystems (Odermatt et…”
A model for the diffuse attenuation coefficient of downwelling irradiance (2005, methodology): “The accuracy for a and bb derived from remote-sensing reflectance can be within 15% [Hoge and Lyon, 1996; Lee et al., 2002; Loisel and Stramski, 2000; Loisel et al., 2001], in contrast to the factor of 2 error in derived [C] [Gordon and Morel, 1983; O’Reilly et al.”
Secchi disk depth: A new theory and mechanistic model for underwater visibility (2015, positive): “Further, r w can be converted to R rs following Lee et al. (2002), and R rspc was taken as the R rs value corresponding to the wavelength with minimum K d .”
Summary diagrams for coupled hydrodynamic-ecosystem model skill assessment (2009, background): “The latter two products were determined from the multiband quasi-analytic algorithm (Lee et al., 2002), which estimates total absorption coefficients over SeaWiFS visible bands and then further decomposes them into phytoplankton and detrital contributions.”
Deriving optical metrics of coastal phytoplankton biomass from ocean colour (2012, neutral): “These fall broadly into two classes of algorithms—empirical band-ratio algorithms, which are derived from the statistical relationship between the ratio of two or more wavebands (blue and green) of remote sensing reflectance, Rrs (sr−1; see Table 1 for a list of symbols and units) and in situ measur”
Sensor Capability and Atmospheric Correction in Ocean Colour Remote Sensing (2015, methodology): “These estimates are then used to derive the biological and biogeochemical properties of the water, such as concentrations of phytoplankton and chlorophyll-a [31], total suspended matter [32–34], coloured dissolved organic matter (CDOM) and detritus, or the inherent optical properties (IOPs) of the w”
A Comprehensive Review on Water Quality Parameters Estimation Using Remote Sensing Techniques (2016, methodology): “Therefore, inversion of remote sensing data provides an efficient method to estimate CDOM concentration within large spatial and temporal scale [141,142].”
An approach for developing Landsat-5 TM-based retrieval models of suspended particulate matter concentration with the assistance of MODIS (2013, background): “Water-leaving radiances are captured by remote sensing sensor and used to estimate water quality parameters, and they are affected by the inherent optical properties of water body, the most fundamental parameters of which are absorption and backscattering coefficients (Lee et al., 2002).”
Space‐based lidar measurements of global ocean carbon stocks (2013, methodology): “…(22°N, 40°W) (Methods S1, sections c and d) and (2) MODIS-Aqua satellite ocean color b bp products from the Garver-Siegel-Maritorena (GSM) inversion algorithm [ Garver and Siegel , 1997; Maritorena et al ., 2002; Siegel et al ., 2002] and the Quasi-Analytical Algorithm (QAA) [ Lee et al ., 2002].”