/Environmental Status/Biogeochemistry
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Monthly mean of backscattering coefficient (bbp) at 490nm (2002-2012) for coastal areas, at global scale, for MERIS sensor, with POLYMER atmospheric corrections. Ref: Loisel in prep.
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Monthly mean of Dissolved Organic Carbone (DOC) (2002-2012) for coastal areas, at global scale, for MERIS sensor, with POLYMER atmospheric corrections. Ref: V Vantrepotte, F Danhiez, H Loisel, S Ouillon, X Mériaux, A Cauvin and D Dessailly. CDOM-DOC relationship in contrasted coastalwaters: implication for DOC retrieval from ocean color remote sensing observation. OPTICS EXPRESS 33 Vol. 23, No. 1 DOI:10.1364/OE.23.000033 2015
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Monthly mean of absorption coefficient minus water absorption (anw) at 412nm (2002-2012) for coastal areas, at global scale, for MERIS sensor, with POLYMER atmospheric corrections. Ref: Loisel (in prep)
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Monthly mean of diffuse attenuation coefficient (Kd) at 490nm (2002-2012), from Jamet et al (2012), for coastal areas, at global scale, for MERIS sensor, with POLYMER atmospheric corrections. Ref: Jamet et al, Retrieval of the spectral diffuse attenuation coefficient Kd(l) in open and coastal ocean waters using a neural network inversion, J. Geophys. Res., 117, C10023, doi:10.1029/2012JC008076.
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90th percentile calculated during the productive period of the WFD (March-October) from 2015 to 2020, from the MODIS Chl-a algorithm processed by OC5 IFREMER/ARGANS (Gohin et al 2002, Gohin 2011).
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Monthly mean of Suspended Particulate Matter (2002-2012) using Han (2016) algorithm for coastal areas, at global scale, for MERIS sensor, with POLYMER atmospheric corrections. Ref: Bing Han, Hubert Loisel, Vincent Vantrepotte, Xavier Mériaux, Philippe Bryère,Sylvain Ouillon, David Dessailly, Qianguo Xing and Jianhua Zhu. Development of a Semi-Analytical Algorithm for the Retrieval of Suspended Particulate Matter rom Remote Sensing over Clear to Very Turbid Waters Remote Sens. 8, 211; doi:10.3390/rs8030211 2016
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90th percentile of non-algal suspended matter calculated during the productive period of the WFD (March-October) from 2015 to 2020, from the MODIS algorithm processed by OC5 IFREMER/ARGANS (Gohin et al 2002, Gohin 2011).
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