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

Absorption

Signal attenuation

Data modeling

Ocean optics

Water

Coastal modeling

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