An Anomalous Record-High Internal Wave Train on the Black Sea Shelf, Generated by an Atmospheric Front
- Authors: Bondur V.G.1, Serebryany A.N.1,2, Zamshin V.V.1
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Affiliations:
- AEROCOSMOS Research Institute for Aerospace Monitoring
- Shirshov Institute of Oceanology, Russian Academy of Sciences
- Issue: Vol 483, No 2 (2018)
- Pages: 1519-1523
- Section: Oceanology
- URL: https://journals.rcsi.science/1028-334X/article/view/194418
- DOI: https://doi.org/10.1134/S1028334X18120012
- ID: 194418
Cite item
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.
About the authors
V. G. Bondur
AEROCOSMOS Research Institute for Aerospace Monitoring
Author for correspondence.
Email: vgbondur@aerocosmos.info
Russian Federation, Moscow, 105064
A. N. Serebryany
AEROCOSMOS Research Institute for Aerospace Monitoring; Shirshov Institute of Oceanology, Russian Academyof Sciences
Email: vgbondur@aerocosmos.info
Russian Federation, Moscow, 105064; Moscow, 117997
V. V. Zamshin
AEROCOSMOS Research Institute for Aerospace Monitoring
Email: vgbondur@aerocosmos.info
Russian Federation, Moscow, 105064
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