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Please use this identifier to cite or link to this item: https://elib.bsu.by/handle/123456789/323017
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dc.contributor.authorTsydenov, B.O.-
dc.contributor.authorSukhovilo, N.Y.-
dc.contributor.authorTrunov, N.S.-
dc.contributor.authorDegi, D.V.-
dc.date.accessioned2024-12-12T14:54:21Z-
dc.date.available2024-12-12T14:54:21Z-
dc.date.issued2024-
dc.identifier.citationE3S Web of Conferences Volume 2024; 510: 03018ru
dc.identifier.urihttps://elib.bsu.by/handle/123456789/323017-
dc.description.abstractThe results of numerical modeling of the dynamics of the spring thermal bar into Lake Dolgoe (Belarus), obtained using meteorological data from the Sharkovshchina station for April 2023, are presented. The dependence of the horizontal movement of the thermal bar front on the wind direction is revealed: the northern wind accelerates it, and the eastern wind slows it down. Modeled temperature distributions showed warming of water not only in the area where the channel flows from Lake Svyadovo, but also in the middle shallow part of the body of waterru
dc.description.sponsorshipThis study was funded by the Russian Science Foundation (project No. 24-47-10001, https://rscf.ru/en/project/24-47-10001/) and the Belarusian Republican Foundation for Fundamental Research (project No. %23\u0420 $ -001).ru
dc.language.isoenru
dc.publisherEDP Sciencesru
dc.rightsinfo:eu-repo/semantics/openAccessru
dc.subjectЭБ БГУ::ЕСТЕСТВЕННЫЕ И ТОЧНЫЕ НАУКИ::Геофизикаru
dc.titleNumerical modeling of the dynamics of the spring thermal bar in Lake Dolgoe (Belarus): preliminary resultsru
dc.typeconference paperru
dc.rights.licenseCC BY 4.0ru
dc.identifier.DOI10.1051/e3sconf/202451003018-
dc.identifier.scopus85190596417-
Appears in Collections:Кафедра общего землеведения и гидрометеорологии (статьи)

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