The detection of ocean color changes, thought to be due to chlorophyll concentrations and gelbstoffe variations, is attempted from high altitude (11.3km) and low altitude (0.3km). The atmospheric back scattering is shown to reduce contrast, but not sufficiently to obscure color change detection at high altitudes. (Author)


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    Title :

    Detection of Ocean Color Changes from High Altitudes


    Contributors:
    W. A. Hovis (author) / M. L. Forman (author) / L. R. Blaine (author)

    Publication date :

    1973


    Size :

    30 pages


    Type of media :

    Report


    Type of material :

    No indication


    Language :

    English




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