A chlorophyll-dependent semianalytical reflectance model derived from field measurements of absorption and backscattering coefficients within the Southern Ocean

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Determination of spectral absorption coefficients of particles, dissolved material and phytoplankton for discrete water samples (2000, methodology): “Reynolds et al. (2001) and Stramska et al. (2000) have reported reasonable closure between estimates of absorption using these methods, radiometric observations and modeling.”
Particle optical backscattering along a chlorophyll gradient in the upper layer of the eastern South Pacific Ocean (2007, methodology): “Only recently have coincident field data become available for relating [Chl] to bbp(λ) (Balch et al., 2001; Reynolds et al., 2001; Twardowski et al., 2001; Stramska et al., 2003; Sullivan et al., 2005; Stramska et al., 2006; Whitmire et al., 2007).”
Optimization of a semianalytical ocean color model for global-scale applications. (2002, methodology): “0.635 660, ( 7 ) where the bw values are taken from Morel.11 When we use the equation relating Kd443 to the absorption and scattering coefficients proposed by Kirk,29”
Submesoscale physical‐biogeochemical coupling across the Ligurian current (northwestern Mediterranean) using a bio‐optical glider (2008, background): “Based on theoretical studies and in-situ studies (e.g., Reynolds et al. 2001; Stramska et al. 2003), c has been proposed as an index characterizing the slope of the particle size distribution for particles lower than 10 mm (Loisel et al. 2006).”