Vertical light attenuation in the northwestern shelf of the Black Sea in the spring period: direct measurements, modeling, and satellite data

V. V. Suslin; A. A. Latushkin; O. V. Martynov

doi:10.1117/12.2503272

13 December 2018 Vertical light attenuation in the northwestern shelf of the Black Sea in the spring period: direct measurements, modeling, and satellite data

V. V. Suslin, A. A. Latushkin, O. V. Martynov

Author Affiliations +

Proceedings Volume 10833, 24th International Symposium on Atmospheric and Ocean Optics: Atmospheric Physics; 108333I (2018) https://doi.org/10.1117/12.2503272
Event: XXIV International Symposium, Atmospheric and Ocean Optics, Atmospheric Physics, 2018, Tomsk, Russian Federation

Abstract

In the paper a joint analysis of direct measurements of the seawater vertical diffuse attenuation coefficient with a satellite product was carried out for several stations on the northwestern shelf of the Black Sea in late April and early May 2017. An attempt to model the empirical spectrum of the seawater vertical diffuse attenuation revealed a number features of that were explained by the peculiarity of the vertical structure, namely, by the presence of an optically active layer, which is typical for the considered period of time and is associated with the thermocline formation process.

Citation Download Citation

V. V. Suslin, A. A. Latushkin, and O. V. Martynov "Vertical light attenuation in the northwestern shelf of the Black Sea in the spring period: direct measurements, modeling, and satellite data", Proc. SPIE 10833, 24th International Symposium on Atmospheric and Ocean Optics: Atmospheric Physics, 108333I (13 December 2018); https://doi.org/10.1117/12.2503272

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