Radiative transfer modelling in atmosphere, water, and on the air-water surface was used to create an algorithm and
computer code for satellite monitoring Chinese estuarine and coastal waters. The atmospheric part of the algorithm is
based on the Reference Evaluation of Solar Transmittance (REST) model for calculation of optical properties of the
atmosphere from the top of the atmosphere to the target; for modelling optical properties from target towards satellite's
sensor, an optical reciprocity principle has been used. An algorithm uses estimates derived from three different sources:
1) the MODIS-based software; 2) radiative transfer equations, and 3) well-known empirical relationships between
measured parameters and optical depths and transmittances for such atmospheric components as molecules, aerosols,
ozone, nitrogen dioxide, precipitable water vapor and uniformly mixed gases. Using this model allowed us to derive a
reliable relationship relating an important parameter, the diffuse-to-global solar incoming irradiance ratio, to the aerosol
optical thickness, solar zenith angle and wavelength. The surface and underwater parts of the algorithm contained
theoretical and semi-empirical relationships between inherent (such as absorption, scattering and backscattering
coefficients) and apparent (remote-sensing reflectance and diffuse attenuation coefficient, Kd) optical properties, and
suspended sediment concentration (SSC) measured in the Yangtze River Estuary and its adjacent coastal area. The first
false colour maps of SSC and Kd demonstrated a well accordance with the multi-year field observations in the region,
and suggest promise for use of this algorithm for the regular monitoring of Chinese and worldwide natural waters.
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