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    A new method accurately flags optically shallow waters in ocean color remote sensing by considering seafloor reflectance, water clarity, and bathymetry. This improves data quality for marine geophysical parameter retrieval.

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    Area of Science:

    • Oceanography
    • Remote Sensing
    • Geophysics

    Background:

    • Ocean-color remote sensing derives marine geophysical parameters from water-leaving radiances.
    • Optically shallow regions, like coral reefs and sand banks, can bias ocean color data due to seafloor reflections.
    • Current methods often mask these areas using only bathymetric data.

    Purpose of the Study:

    • To develop an improved method for flagging optically shallow pixels in ocean color datasets.
    • To account for bathymetry, water clarity, and seafloor albedo in identifying optically shallow areas.
    • To enhance the quality control of derived ocean color products.

    Main Methods:

    • Developed a new approach to flag optically shallow pixels by integrating bathymetry, water clarity, and seafloor albedo.
    • Predicted water column optical depth at 547 nm (ζ(547)) from bathymetric and optical properties.
    • Used radiative transfer modeling to establish a threshold (ζ(547) = 20) for flagging, also flagging waters shallower than 5m.

    Main Results:

    • The new method successfully flags potentially optically shallow pixels by considering multiple factors.
    • Radiative transfer modeling identified a conservative threshold for flagging based on seafloor reflectance.
    • Analysis showed varying bathymetric datasets can influence the optically shallow flag.

    Conclusions:

    • The developed optically shallow flag enhances the quality control of ocean color data products.
    • This flag can be utilized to switch between algorithms for optically deep and shallow waters.
    • The method provides a more robust approach to handling seafloor reflectance contamination in remote sensing data.