2013
DOI: 10.1134/s0001437013030107
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Long-term variability of the water transparency (Secchi Depth) in the Sea of Azov

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Cited by 5 publications
(3 citation statements)
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“…The total water discharge into the Black Sea constitutes around 53-55 km 3 /yr, while the total inflow ranges between 36 and 38 km 3 /yr [31]. This mixing of riverine and marine water results in a large salinity gradient (2-12 psu) and high TSS concentrations over the whole sea (average 19.1 mg/L [31,40]), with an average organic carbon content of 16.5% [40]. Due to the large discharge of nutrients and sediment (~25.8 mg/L TSS), the river deltas not only serve as spawning grounds for a variety of commercially valuable fish species but are also pollution hotspots [31,37,41].…”
Section: Site Description and Model Input Variablesmentioning
confidence: 99%
“…The total water discharge into the Black Sea constitutes around 53-55 km 3 /yr, while the total inflow ranges between 36 and 38 km 3 /yr [31]. This mixing of riverine and marine water results in a large salinity gradient (2-12 psu) and high TSS concentrations over the whole sea (average 19.1 mg/L [31,40]), with an average organic carbon content of 16.5% [40]. Due to the large discharge of nutrients and sediment (~25.8 mg/L TSS), the river deltas not only serve as spawning grounds for a variety of commercially valuable fish species but are also pollution hotspots [31,37,41].…”
Section: Site Description and Model Input Variablesmentioning
confidence: 99%
“…In March and June 2016 methods for the operative remote monitoring of the Taganrog Bay and Don estuary aquatic environment state were tested, based on analyzing the shape of the spectra of the spectral brightness of the radiation ascending from the water [22]. Expeditionary materials significantly replenished the oceanographic database of the Southern Scientific Center of the Russian Academy of Sciences [23]: based on field and archival data, the long-term dynamics of organic matter and carbon, transparency and salinity of the Azov Sea [24][25][26] were estimated. The characteristics of small-scale variability of temperature, salinity, internal waves and fluctuations in the level of the Black Sea were calculated [27][28][29].…”
Section: Research Vessel Denebmentioning
confidence: 99%
“…The increase of particles in the water column causes light attenuation and decreases the water transparency (James et al, 2004;Sorokina and Kulygin, 2013). Accompanying sediment resuspension are an enhanced exchange between the porewater and overlying water and the adsorption and desorption of resuspended particles, factors that influence phosphorus and nitrogen cycling across the sediment-water interface (You et al, 2007b;de Vicente et al, 2010;Kalnejais et al, 2010;Couceiro et al, 2013;Tammeorg et al, 2013).…”
Section: Introductionmentioning
confidence: 99%