2010
DOI: 10.1016/j.rse.2009.09.017
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MODIS imagery of turbid plumes in San Diego coastal waters during rainstorm events

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Cited by 59 publications
(35 citation statements)
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“…Radiance or reflectance values measured in the band 1 have been used as qualitative proxy for amounts of total suspended matter (TSM) (e.g. Lahet and Stramski, 2010) or integrated in empirical bio-optical algorithms to quantify the concentrations of TSM (mg.l -1 ) or the turbidity levels (NTU) in marine waters (e.g. Miller andMcKee 2004, Petus et al 2010).…”
Section: Methodsmentioning
confidence: 99%
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“…Radiance or reflectance values measured in the band 1 have been used as qualitative proxy for amounts of total suspended matter (TSM) (e.g. Lahet and Stramski, 2010) or integrated in empirical bio-optical algorithms to quantify the concentrations of TSM (mg.l -1 ) or the turbidity levels (NTU) in marine waters (e.g. Miller andMcKee 2004, Petus et al 2010).…”
Section: Methodsmentioning
confidence: 99%
“…However, spatial and temporal variations in river plume events are modulated by a number of factors including storms and discharge strength (e.g. Lahet andStramski, 2010, Lihan et al, 2008), coefficients and tidal cycles (e.g. Valente and da Silva, 2006), magnitude and direction of wind stress (e.g.…”
Section: Introductionmentioning
confidence: 99%
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“…These daily products provide surface reflectance at 250-m resolution for band 1 (620-670 nm) and 500-m resolution for band 4 (545-565 nm). We used band 1 as a qualitative proxy for amounts of turbidity (sediment dominated) levels, because earlier studies has found that reflectance centered on 645 nm had high and constant sensitivity to suspended particles and was often integrated into empirical bio-optical algorithms to quantify the total suspended sediment (mg/L) or turbidity levels (NTU) (Lahet and Stramski, 2010;Aurin et al, 2013;Park and Latrubesse, 2014;Petus et al, 2014;Fernández-Nóvoa et al, 2015). Band 4 was used for depicting sea surface salinity patterns, because SR at the green-blue range is a better indicator of surface salinity than other visible spectrum wavelengths (Hu et al, 2004;Ahn et al, 2008;Palacios et al, 2009).…”
Section: Satellite Data 231 Modis Reflectancementioning
confidence: 99%
“…The optical properties of coastal surface waters can be used to distinguish turbid plume water from ambient water masses (Lahet and Stramski, 2010). Supervised classification of ocean color data has been successfully employed to develop link between light absorption of Chromophoric Dissolved Organic Matter (CDOM) and surface salinity in Columbia River plume (Palacios et al, 2009).…”
Section: Introductionmentioning
confidence: 99%