Particulate backscattering retrieval from remotely-sensed turbidity in various coastal and riverine turbid waters

The semi-empirical algorithm of [1] for the estimation of turbidity (T) from marine reflectance (?w) is calibrated and validated using a large dataset of in situ measurements collected in various waters, for use with any ocean colour hyperspectral sensor, and with Sentinel-2, Landsat 8 and Pléiades...

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Publicado: 2016
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Acceso en línea:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_03796566_vSP-740_n_p_Nechad
http://hdl.handle.net/20.500.12110/paper_03796566_vSP-740_n_p_Nechad
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Sumario:The semi-empirical algorithm of [1] for the estimation of turbidity (T) from marine reflectance (?w) is calibrated and validated using a large dataset of in situ measurements collected in various waters, for use with any ocean colour hyperspectral sensor, and with Sentinel-2, Landsat 8 and Pléiades spectral bands. The relationship between particulate backscattering coefficient (bbp) and side-scattering (T) is investigated through simulation of Fournier-Forand phase functions, assuming variable particles size and composition, and through T and bbp in situ measurements in clear to extremely turbid waters.