V.V. Gorbatskiy

Krylov State Research Center

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СБ

С. Б. Куклев

Institute of Oceanology. PP Shirshov Russian Academy of Sciences

K. D. Sabinin

Acoustic Institute named after NN Andreev

АГ

А. Г. Зацепин

Institute of Oceanology. PP Shirshov Russian Academy of Sciences

V. A. Telegin

Institute of Terrestrial Magnetism Ionosphere and Radio Wave Propagation

A.Y.C. Yu

Krylov State Research Center

Alexey Kuleshov

Institute of Oceanology. PP Shirshov Russian Academy of Sciences

Vadim Sivkov

Institute of Oceanology. PP Shirshov Russian Academy of Sciences

Yury Zhurov

Institute of Oceanology. PP Shirshov Russian Academy of Sciences

Cooperative Institutions

Institute of Oceanology. PP Shirshov Russian Academy of Sciences

Russian Academy of Sciences

Krylov State Research Center

ORCID

Sandia National Laboratories

University of Science and Technology of China

Fairchild Semiconductor (United States)

Stanford University

Immanuel Kant Baltic Federal University

Klaipėda University

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Doppler HF Radar Application for the Study of Spatial Structure of Currents in the Black Sea

Physical Oceanography (2017)

V.V. Gorbatskiy K. D. Sabinin V. A. Telegin А. Г. Зацепин С. Б. Куклев

Introduction.The technology of surface current velocity measurement by Doppler radars in the coastal zones of the seas and oceans has been developed and used in different countries, such as the USA, Canada, United Kingdom, France, Australia and Japan for almost 40 years [1].Various companies produce Doppler HF radars (for example, SeaSonde radars by CODAR Ocean Sensors (USA) [2] and WERA by Helzel Messtechnik GmbH (Germany) [3]), which measure the velocity of surface currents in the coastal zone from 0.5-5 to 20-200 km from the shore with a 0.5-5 km spatial resolution, depending on the operational frequency range and the range of measurements.In the presence of the large amount of radars

Black Sea

10.22449/1573-160x-2017-3-58-68

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Surface current measurements with ship-borne Doppler HF radar

International Radar Symposium (2013)

V.V. Gorbatskiy A.Y.C. Yu

The paper presents application results for high-frequency Doppler radar system SeaSonde™ by CODAR Ocean Sensors meant for measurement of surface currents in Kara Sea water areas from ship board. The developed measurement guidelines enabled collecting on-line data on currents structure in the area featuring high variability of hydrometeorological parameters. The obtained data ensure assessment of quantitative characteristics of current tidal instability in the investigated water area and demonstrate relationship between surface current parameters and spatial nonuniformity of water salinity. Such nonuniformity in this case is stipulated by intensive river discharge in the measured area.

Hydrometeorology

Wave radar

Current meter

On board

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Muddy contourites in the Baltic Sea: an example of a shallow-water contourite system

Geological Society London Memoirs (2002)

Vadim Sivkov V.V. Gorbatskiy Alexey Kuleshov Yury Zhurov

Abstract Bottom currents in the Baltic Sea have had a pronounced effect on the nature and distribution of sediments throughout the Holocene. Due to the intermittent nature of water exchange between the North and the Baltic Seas, the flow of bottom currents is impermanent. Well-developed nepheloid layers are commonly associated with these bottom currents, and provide evidence that active re-suspension and sediment transport is taking place. Periodically intensified inflow from the North Sea through the Baltic Sea gateway has led to erosion of narrow elongate channels, and associated deposition of small elongate patch drifts and contourite levees. The latter two are best developed on the left flanks of the channels. As a result of strong lateral sediment transport, the overall thickness of muddy contourite layers increases towards the steeper slopes of the sea which are situated on the right-hand side of the inflows. Muddy contourites of the Baltic Sea are predominantly terrigenous in composition, made up of soft, black sulphidic muds that are enriched in organic carbon and manganese. Both enrichments are caused by high biological productivity and periodic stagnation of near-bottom waters. Atypically for most oceanic contourites, these shallow-water organic-rich contourites are finely laminated and generally unbioturbated.

Contourite

Baltic sea

paleoceanography

10.1144/gsl.mem.2002.022.01.10

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Citations (21)

The Doppler short-wave radar applied to studying spatial structure of currents in the Black Sea

Morskoy gidrofizicheskiy zhurnal (2017)

V.V. Gorbatskiy K. D. Sabinin V. A. Telegin А. Г. Зацепин С. Б. Куклев

Black Sea

10.22449/0233-7584-2017-3-63-73

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