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Reasons for the appearance of the maximum near 700 nm in the radiance spectrum emitted by the ocean layer
Vasil'kov, A.P.; Kopelevich, O.V. (1982). Reasons for the appearance of the maximum near 700 nm in the radiance spectrum emitted by the ocean layer. Oceanology 22(6): 697-701
In: Oceanology. Maik Nauka/Springer: Moscow. ISSN 0001-4370; e-ISSN 1531-8508, more
Peer reviewed article  
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  • Vasil'kov, A.P.
  • Kopelevich, O.V.
Abstract
    Using model calculations it is shown that the appearance of this maximum is explained by the corresponding minimum in the absorption spectrum of seawater which arises when the chlorophyll concentration exceeds ~1 mg • m-3.
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