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Palabras clave – provistas por la editorial

atmosphere; radiative transfer; ocean colour; phytoplankton pigments; satellite radiometry; light scattering by pure water; upward radiance; CDOM and ENSO; chromophoric dissolved organic matter; irradiance quartet; PFT; FerryBox; marine sensors; Kallemeter; DOM; retrieval uncertainty; particle dynamics; suspended sediment; downward irradiance; sea ice heterogeneity; optical properties; inelastic processes; MERIS; bottom mapping; FDOM; NASA PACE mission; volume scattering function; ocean color algorithm validation; Gelbstoff; hyperspectral; ocean euphotic zone; light scattering; ocean color database; upwelling radiance distribution; degree of linear polarization; light scattering measurements; polarization; 3D Monte Carlo numerical simulations; apparent optical properties; EEMS; machine learning; bulk refractive index; sensor noise; remote-sensing reflectance; coated-sphere model; PARAFAC; forward modeling; coral reef; oceanic carbon; chlorophyll-a; fractal structure; shallow water; melt ponds; canopy; coral; phytoplankton; backscattering ratio; CDOM climatology; remote sensing; algorithm development; ocean; LISST-VSF instrument; bathymetry; suspended matter; anomalous properties of water; optical modelling; marine optics; derivative; coupled systems; ocean color; light scattering by pure seawater; CDOM spectral slope; Gershun equation; inverse problems; ocean optics; vertical attenuation coefficient; organic carbon; marine particles; CDOM; seawater component; global oceans; vector radiative transfer; radiative transfer approximation; oceanic light field; Mueller matrix; Trondheimsfjord; Norway; volume and surface integral methods; ocean color remote sensing; natural organic matter; inherent optical properties; dissolved organic carbon