Numerical simulation of an intensive upwelling event in the northeastern part of the Black Sea at the IO RAS hydrophysical testing site
The paper discusses mathematical simulation of intensive coastal upwelling observed in the northeastern part of the Black Sea in the water area of the hydrophysical test site of the Shirshov Institute of Oceanology, Russian Academy of Sciences, in September 2013. The simulation was carried out with...
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Veröffentlicht in: | Oceanology (Washington. 1965) 2017-09, Vol.57 (5), p.615-620 |
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creator | Divinsky, B. V. Kuklev, S. B. Zatsepin, A. G. |
description | The paper discusses mathematical simulation of intensive coastal upwelling observed in the northeastern part of the Black Sea in the water area of the hydrophysical test site of the Shirshov Institute of Oceanology, Russian Academy of Sciences, in September 2013. The simulation was carried out with the MIKE 21/3 Coupled Model FM combined hydrodynamic model of the Danish Hydraulics Institute (DHI). The calculation results are compared with the data of direct instrumental observations carried out in the IO RAS hydrophysical survey area. The essential role of surface wind waves in the formation of the observed temperature profiles is demonstrated, as well as the necessity of taking it into account when considering peculiarities in the vertical circulation of coastal waters. |
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The essential role of surface wind waves in the formation of the observed temperature profiles is demonstrated, as well as the necessity of taking it into account when considering peculiarities in the vertical circulation of coastal waters.</description><subject>Coastal environments</subject><subject>Coastal upwelling</subject><subject>Coastal waters</subject><subject>Computational fluid dynamics</subject><subject>Computer simulation</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Fluid flow</subject><subject>Hydraulics</subject><subject>Hydrodynamics</subject><subject>Marine Physics</subject><subject>Mathematical models</subject><subject>Ocean circulation</subject><subject>Oceanography</subject><subject>Profiles</subject><subject>Simulation</subject><subject>Surface wind</subject><subject>Surveying</subject><subject>Temperature profile</subject><subject>Temperature profiles</subject><subject>Upwelling</subject><subject>Water circulation</subject><subject>Wind waves</subject><issn>0001-4370</issn><issn>1531-8508</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp1UMtKAzEUDaJgrX6Au4Dr0WQyj2RZxUehWLC6HjKTO23qNDMmmUq_wN8207oQxNWBe16Xg9AlJdeUsuRmQQihCcsJzUlCCONHaERTRiOeEn6MRgMdDfwpOnNuHRQ0EXyEvp77DVhdyQY7vekb6XVrcFtjabA2HozTW8B99wlNo80SwxaMDwz2K8CmtQGk82AN7qT1g3EgbhtZveMFSCz9_jCd45fJAq92yrbdauf2hR6cHzKd9nCOTmrZOLj4wTF6e7h_vXuKZvPH6d1kFlWMZj5SEpSqVZyKNE-rSlUxZJypNOY0UYJlnJZ5LOtSEiVKnmYxkExAWTLgZUalYmN0dcjtbPvRhweKddtbEyoLKlIeNomFCCp6UFW2dc5CXXRWb6TdFZQUw97Fn72DJz54XNCaJdhfyf-avgHE_YPJ</recordid><startdate>20170901</startdate><enddate>20170901</enddate><creator>Divinsky, B. 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G.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c316t-daeddfd259575ccdc2e683d52814d93681b72afba0d9b8562e069ebb3e8b61ad3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2017</creationdate><topic>Coastal environments</topic><topic>Coastal upwelling</topic><topic>Coastal waters</topic><topic>Computational fluid dynamics</topic><topic>Computer simulation</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Fluid flow</topic><topic>Hydraulics</topic><topic>Hydrodynamics</topic><topic>Marine Physics</topic><topic>Mathematical models</topic><topic>Ocean circulation</topic><topic>Oceanography</topic><topic>Profiles</topic><topic>Simulation</topic><topic>Surface wind</topic><topic>Surveying</topic><topic>Temperature profile</topic><topic>Temperature profiles</topic><topic>Upwelling</topic><topic>Water circulation</topic><topic>Wind waves</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Divinsky, B. 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The calculation results are compared with the data of direct instrumental observations carried out in the IO RAS hydrophysical survey area. The essential role of surface wind waves in the formation of the observed temperature profiles is demonstrated, as well as the necessity of taking it into account when considering peculiarities in the vertical circulation of coastal waters.</abstract><cop>Moscow</cop><pub>Pleiades Publishing</pub><doi>10.1134/S0001437017040038</doi><tpages>6</tpages></addata></record> |
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subjects | Coastal environments Coastal upwelling Coastal waters Computational fluid dynamics Computer simulation Earth and Environmental Science Earth Sciences Fluid flow Hydraulics Hydrodynamics Marine Physics Mathematical models Ocean circulation Oceanography Profiles Simulation Surface wind Surveying Temperature profile Temperature profiles Upwelling Water circulation Wind waves |
title | Numerical simulation of an intensive upwelling event in the northeastern part of the Black Sea at the IO RAS hydrophysical testing site |
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