Spatial structure and variability of fields of currents, attenuation factor of light, and temperature in the surface layer of the northwest part of the Black Sea

Agafonov, E. A.; Kaminsky, S. T.; Kukushkin, A. S.; Prokhorenko, Yu. A.

doi:10.1007/bf02519306

Cited by 2 publications

(5 citation statements)

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“…As follows from Figs. 1 and 2 [9], the values of current velocity in the Karkinit Bay in winter somewhat decrease as compared with its values in autumn.…”

Section: Seasonal Variations Of the Inflows Of Water Into The Karkinimentioning

confidence: 71%

“…2). At the same time, the Karkinit Bay was, most likely, characterized by the presence of anticyclonic circulation [4,5,9], which is indirectly confirmed by the direction of current vectors near its west boundary. As follows from Figs.…”

Section: Seasonal Variations Of the Inflows Of Water Into The Karkinimentioning

confidence: 92%

“…Examples of the indicated types of motion of waters can be found in Figs. 1 and 2, where the schemes of the surface currents for autumn and summer are presented according to the data from [9]. In autumn, after the northwest (NW) and west (W) winds with velocities of 8-12 m/sec (here and in what follows, the geographical directions of the winds are denoted by their first letters), the surface current in the Karkinit Bay had the well-pronounced anticyclonic direction (according to the data of electromagnetic current meters) (Fig.…”

Section: Seasonal Variations Of the Inflows Of Water Into The Karkinimentioning

confidence: 99%

“…Schematic diagram of the surface currents in the northwest part of the Black Sea in March 1984 according to the data presented in[9].…”

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confidence: 99%

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Seasonal freshening and salinization of waters in the Karkinit Bay

Pukhtyar

2007

Phys Oceanogr

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551.465On the basis on the experimental hydrological data accumulated in the database of the Marine Hydrophysical Institute of the Ukrainian National Academy of Sciences and the meteorological data of the Marine Department of the Ukrainian Scientific-Research Hydrometeorological Institute, we study the characteristics of seasonal variability of the processes of renewal, freshening, and salinization of waters in the Karkinit Bay. We analyze and estimate the repeatability of the inflows of salt and freshened waters from the sea as well as the variations of the areas occupied by these waters in the water area of the bay depending on the seasonal and wind conditions. For the spring-summer period, we estimate the period of renewal of waters in the upper layer of the main part of the bay (11-14 days). A time interval of possible absence of noticeable water exchange between the main and east shallow parts of the bay (of about two months) is revealed in the summer-autumn period.

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“…As follows from Figs. 1 and 2 [9], the values of current velocity in the Karkinit Bay in winter somewhat decrease as compared with its values in autumn.…”

Section: Seasonal Variations Of the Inflows Of Water Into The Karkinimentioning

confidence: 71%

Section: Seasonal Variations Of the Inflows Of Water Into The Karkinimentioning

confidence: 92%

Section: Seasonal Variations Of the Inflows Of Water Into The Karkinimentioning

confidence: 99%

“…Schematic diagram of the surface currents in the northwest part of the Black Sea in March 1984 according to the data presented in[9].…”

mentioning

confidence: 99%

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Seasonal freshening and salinization of waters in the Karkinit Bay

Pukhtyar

2007

Phys Oceanogr

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“…In Zmiinyi Island waters, measured environmental variables showed pronounced seasonal variation; the maximum values of temperature and salinity during the June to September period were accompanied by the smallest concentrations of dissolved oxygen, probably due to the decreased solubility at higher temperatures and algal blooms characteristic of the NWBS during summer (Knowler et al 2001;Kideys 2002). The absence of any significant correlation between seasonal Danube outflow and environmental variables (above all salinity) near Zmiinyi Island could be attributed to the fact that the island is located near the northern edge of the Danube Delta, while the sea currents run primarily from north to south along the coast in this region (Klimok et al 1990;Agafonov et al 2000;Oguz et al 2002).…”

Section: Environmental Analysismentioning

confidence: 99%

The fish community in Zmiinyi Island waters: structure and determinants

2012

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show abstract

Spatial structure and variability of fields of currents, attenuation factor of light, and temperature in the surface layer of the northwest part of the Black Sea

Cited by 2 publications

References 1 publication

Seasonal freshening and salinization of waters in the Karkinit Bay

Seasonal freshening and salinization of waters in the Karkinit Bay

The fish community in Zmiinyi Island waters: structure and determinants

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