geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-3609Research ArticleНаучные сообщенияShort communicationsПриливо-отливные формы мезорельефа дна восточной части Белого моряTidal mesorelief at the bottom of the eastern part of the White SeaЛевченкоО. В.LevchenkoO. V.ЩербаковФ. А.ShcherbakovF. A.Институт океанологии РАНРоссия199916012024048592Copyright © Левченко О.В., Щербаков Ф.А., 20242024Левченко О.В., Щербаков Ф.А.Levchenko O.V., Shcherbakov F.A.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://geomorphology.igras.ru/jour/article/view/3609

The data obtained by the parametric fathometer "Arasound" in 1997 during the run of the research ship "Academician Sergey Vavilov" in the easter part of the White Sea were processed. Six accumulative and two erosion tidal landform types are characterized. Sand ridges, sand waves of two types, sand ripple and glib sands may be mentioned among accumulative forms. The conditions of such landform existence and their distribution within the area are discussed.

The data obtained by the parametric fathometer "Arasound" in 1997 during the run of the research ship "Academician Sergey Vavilov" in the easter part of the White Sea were processed. Six accumulative and two erosion tidal landform types are characterized. Sand ridges, sand waves of two types, sand ripple and glib sands may be mentioned among accumulative forms. The conditions of such landform existence and their distribution within the area are discussed.

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