Bio-Optical Modeling and Remote Sensing of Inland Waters 2017
DOI: 10.1016/b978-0-12-804644-9.00007-0
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Bio-optical Modeling of Sun-Induced Chlorophyll- a Fluorescence

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Cited by 8 publications
(6 citation statements)
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“…SIF was retrieved from in-situ, airborne and spaceborne measurements in SNAP using the Fluorescence Line Height (FLH) algorithm, an established empirical algorithm that exploits radiances at and around the SIF emission in three spectral bands (for this work 665 nm, 681 nm and 709 nm). For more details on the algorithm approach, its general formula and the selected spectral bands see [11], [12], [13]. The FLH method is typically used in the open ocean since low signal from elastic scattering provides good resulting baseline curves [14], [15] .…”
Section: Methodsmentioning
confidence: 99%
See 1 more Smart Citation
“…SIF was retrieved from in-situ, airborne and spaceborne measurements in SNAP using the Fluorescence Line Height (FLH) algorithm, an established empirical algorithm that exploits radiances at and around the SIF emission in three spectral bands (for this work 665 nm, 681 nm and 709 nm). For more details on the algorithm approach, its general formula and the selected spectral bands see [11], [12], [13]. The FLH method is typically used in the open ocean since low signal from elastic scattering provides good resulting baseline curves [14], [15] .…”
Section: Methodsmentioning
confidence: 99%
“…The FLH method is typically used in the open ocean since low signal from elastic scattering provides good resulting baseline curves [14], [15] . High TChla and TSM concentrations in optically complex waters could significantly affect FLH results due to a peak from the elastic reflectance overlapping with the fluorescence signal and therefore potentially contaminating fluorescence retrieval [11].…”
Section: Methodsmentioning
confidence: 99%
“…As discussed above, however, fluorescence per chla (or more correctly per absorbed photon) is not constant. For this reason, a number of studies have explored the use of SIF signatures as a diagnostic tool to assess phytoplankton physiological state (e.g., Letelier et al, 1997;Morrison, 2003;Schallenberg et al, 2008;Behrenfeld et al, 2009;O'Malley et al, 2014;Gilerson and Huot, 2017). Remote sensing of phytoplankton physiology over entire ocean basins would significantly advance the development of global primary productivity models.…”
Section: St-chlf and The Interpretation Of Sun Induced Chlfmentioning
confidence: 99%
“…The models can be roughly divided into analytical methods and empirical methods [29][30][31]. The former is to use the theory of radiation transfer to deduce the optical characteristics of each component in the water column, which extends the semi-analytical methods and quasi-analytical methods, generally used to estimate concentrations of chlorophyll-a(Chla), total suspended solids and other optically active substances [29]. For example, Lee et al put forward a quasi-analytical model for Chl-a in class II water in 2002 [32].…”
Section: Introductionmentioning
confidence: 99%