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An Anomalous Record-High Internal Wave Train on the Black Sea Shelf, Generated by an Atmospheric Front

  • OCEANOLOGY
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Abstract

This paper reports the data obtained on the anomalous train of soliton-like internal record-high waves in the Black Sea (h = ~16 m). Such a train was detected at a depth of ~30 m in October 2015 on the shelf near Gelendzhik with the use of an acoustic Doppler current profiler and a chain of thermistors and by processing of a space radar image obtained from the SENTINEL-1A satellite. The intensive atmospheric front revealed by meteorological data generated such internal waves, which are anomalous for the Black Sea.

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ACKNOWLEDGMENTS

This work was supported by the Ministry of Education and Science of the Russian Federation, project no. RFMEFI57716X0234.

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Authors and Affiliations

  1. AEROCOSMOS Research Institute for Aerospace Monitoring, 105064, Moscow, Russia

    V. G. Bondur, A. N. Serebryany & V. V. Zamshin

  2. Shirshov Institute of Oceanology, Russian Academy of Sciences, 117997, Moscow, Russia

    A. N. Serebryany

Authors
  1. V. G. Bondur
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  2. A. N. Serebryany
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  3. V. V. Zamshin
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Correspondence to V. G. Bondur.

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Translated by E. Maslennikova

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Bondur, V.G., Serebryany, A.N. & Zamshin, V.V. An Anomalous Record-High Internal Wave Train on the Black Sea Shelf, Generated by an Atmospheric Front. Dokl. Earth Sc. 483, 1519–1523 (2018). https://doi.org/10.1134/S1028334X18120012

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  • DOI: https://doi.org/10.1134/S1028334X18120012

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