gesjGEOGRAPHY, ENVIRONMENT, SUSTAINABILITYGEOGRAPHY, ENVIRONMENT, SUSTAINABILITY2071-93882542-1565Russian Geographical Society10.24057/2071-9388-2018-67gesj-687Research ArticleENVIRONMENTОкружающая средаNew Possibilities In The Study Of Coastal Upwellings In The Southeastern Baltic Sea With Using Thermistor ChainKrechikViktor

Shirshov Institute of Oceanology.

Moscow.

MyslenkovStanislav

Shirshov Institute of Oceanology, RAS; Marine forecast division, Hydrometeorological Research Centre of the Russian Federation.

Moscow.

stasocean@gmail.comKapustinaMaria

Shirshov Institute of Oceanology.

Moscow.

Russian Academy of SciencesRussian FederationLomonosov Moscow State University; Russian Academy of Sciences; Hydrometeorological Research Centre of the Russian FederationRussian Federation2019070520191224461Copyright © Krechik V., Myslenkov S., Kapustina M., 20192019Krechik V., Myslenkov S., Kapustina M.Krechik V., Myslenkov S., Kapustina M.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://ges.rgo.ru/jour/article/view/687

The article gives an analysis of a unique data of the thermistor chain, which installed on the D-6 oil platform in the coastal zone of the Baltic Sea. In total 10 temperature sensors were installed at different depths with a recording  interval of 1 min, the depth at the installation site was 29 m. Based on satellite data, ship measurements  and thermistor chain observation  the characteristics  and dynamics of the sharp decrease in water temperature which registered in the south-eastern  Baltic Sea (Gdansk Bay area), during June 5-12, 2016 are analyzed. The temperature decreasing caused by the simultaneous action of at least two factors: wind-driven Ekman upwelling and advection of cold water. Scales of temporal  and spatial  variability  of water temperature in a coastal zone of the south-eastern Baltic Sea near the coast of the Kaliningrad region are described. This event led to the considerable SST (sea sur face temperature) drop by more than 8 °C for two days. The rate of reduction of its temperature during certain upwelling periods can reach 0.3-0.4 ºС per hour, but the maximum  warming  rate between  phases varies from 0.25 to 0.28 ºС per hour. This dramatically changed  the conditions of the thermal balance of the sea sur face. The width of the upwelling, as seen in the SST data, was about 25 km. Satellite data were supplemented with data of a thermistor  chain and C TD measurements. The high correlation between  water temperature variability and changes in wind parameters: when the wind speed has decreased and its direction has changed, the response of the vertical thermal structure has occurred very quickly, sometimes within 1 hour. Thermistor chain data allow to evaluate the vertical temperature distribution and get more detailed analysis of temporal  variability and short pulsations of upwelling.

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The authors declare that there are no conflicts of interest present.