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Bio-optical algorithm evaluation for MODIS for western Canada coastal waters: An exploratory approach using in situ reflectance
Authors:NM Komick  MPF Costa
Affiliation:a Fisheries and Ocean Canada, Pacific Biological Station, 3190 Hammond Bay Rd., Nanaimo BC, Canada V9T 6N7
b Department of Geography, University of Victoria, PO Box 3050, Victoria BC, Canada V8W 3P5
c Fisheries and Ocean Canada, Institute of Ocean Sciences, PO Box 6000, Sidney BC, Canada V8L 4B2
Abstract:Biophysical and above-water reflectance measurements collected in 2006 were used to evaluate the OC3M, standard GSM01, and a modified version of the GSM01 algorithms for estimating chlorophyll-a (chl) concentrations in the Strait of Georgia, located off the southwest coast of Canada. The Strait was generally a case 2 water body, transitioning from chromophoric dissolved organic matter (CDOM) dominant in the central region to possibly particulate dominant in Fraser River plume regions. Results showed that the OC3M algorithm was somewhat effective (R2 = 0.550) outside the most turbid areas of the Fraser River plume. However, a systematic overestimation of lower chl concentrations was found, which may have been related to the higher CDOM absorption observed throughout the Strait. The standard GSM01 algorithm had moderately good agreement with measured CDOM absorption (R2 = 0.593) and total suspended solids (TSS) concentrations (R2 = 0.888), but was ineffective at estimating chl concentrations. Localized characterization of the CDOM absorption, through a hyperbolic CDOM model, improved the modified GSM01 results with slightly better agreement with measure CDOM absorption (R2 = 0.614) and TSS concentrations (R2 = 0.933). When the modified GSM01 algorithm was limited to regions with lower combined CDOM and non-algal particulate absorption (adg (443) < 0.7 m− 1), it was more effective then the OC3M algorithm at estimating chl concentrations. This suggests that a threshold value on the adg (443) or bbp (443) estimated by the GSM01 algorithm may be beneficial for limiting turbidity influence on the algorithm. The further reinterpretation of phytoplankton absorption from the modified GSM01 algorithm with a two-component phytoplankton model resulted in a chl relationship with an R2 = 0.677 and a linear slope closer to one.
Keywords:Bio-optical  Chlorophyll  Coastal  Canada  Strait of Georgia  MODIS  Remote sensing  Ocean colour  Ocean color
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