2014
DOI: 10.1016/j.pocean.2013.12.008
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A review of ocean color remote sensing methods and statistical techniques for the detection, mapping and analysis of phytoplankton blooms in coastal and open oceans

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Cited by 475 publications
(324 citation statements)
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“…In the optically complex and very diverse coastal zone, separating the contribution of chl a from other colored constituents [namely particulate inorganic matter (PIM), and colored dissolved organic matter (CDOM)] in the water column is notoriously difficult due to the rapidly changing concentrations of CDOM and PIM coming from sediment resuspension, river plume, and land runoff (Blondeau-Patissier et al, 2014). In turbid tidal flat and adjacent coastal areas, the main challenge arises from the difficulty to detect chl a from the high load of suspended particulate matter (SPM).…”
Section: Introductionmentioning
confidence: 99%
“…In the optically complex and very diverse coastal zone, separating the contribution of chl a from other colored constituents [namely particulate inorganic matter (PIM), and colored dissolved organic matter (CDOM)] in the water column is notoriously difficult due to the rapidly changing concentrations of CDOM and PIM coming from sediment resuspension, river plume, and land runoff (Blondeau-Patissier et al, 2014). In turbid tidal flat and adjacent coastal areas, the main challenge arises from the difficulty to detect chl a from the high load of suspended particulate matter (SPM).…”
Section: Introductionmentioning
confidence: 99%
“…Unlike the previous indices, FAI was originally applied for detecting cyanobacteria and macro-algae in shallow, turbid fresh water and coastal areas, such as Lake Taihu (China), the Yellow Sea (China), Tampa Bay (USA), and the Gulf of Mexico [23][24][25]. The FAI is used in combination with pre-determined thresholds to help separate land, cloud or sediments from pixels associated with surface algal scums, thereby making it more sensitive to turbid water and shallow depths than other indices [26].…”
Section: Introductionmentioning
confidence: 99%
“…For data assimilation for Taihu Lake, Qi et al (2014) [42] used Chla data products derived from the red and NIR bands (645 and 859 nm) of MODIS [43] , which suffer from interferences of sediment resuspension. Indeed, despite the effort in the past decade on algorithm development for inland water bodies [20,23,24,[44][45][46][47][48][49][50], for a number of reasons there is no reliable Chla algorithm that can be applied to MODIS data in near real-time for the purposes of both timely information delivery and data assimilation for Taihu Lake.…”
Section: Introductionmentioning
confidence: 99%