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Natural Hazards and Earth System Sciences An interactive open-access journal of the European Geosciences Union
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Volume 11, issue 3
Nat. Hazards Earth Syst. Sci., 11, 981–986, 2011
https://doi.org/10.5194/nhess-11-981-2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: Extreme and rogue waves

Nat. Hazards Earth Syst. Sci., 11, 981–986, 2011
https://doi.org/10.5194/nhess-11-981-2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 25 Mar 2011

Research article | 25 Mar 2011

Huge internal waves in the vicinity of the Spitsbergen Island (Barents Sea)

O. E. Kurkina1,2,3 and T. G. Talipova4 O. E. Kurkina and T. G. Talipova
  • 1Institute of Cybernetics, Tallinn University of Technology, Tallinn, Estonia
  • 2State University The Higher School of Economics, Nizhny Novgorod Branch, Nizhny Novgorod, Russia
  • 3Nizhny Novgorod State Technical University, Nizhny Novgorod, Russia
  • 4Institute of Applied Physics of Russian Academy of Sciences, Nizhny Novgorod, Russia

Abstract. The generation of huge amplitude internal waves by the barotropic tide in the Barents Sea at high latitudes is examined using the numerical model of the Euler 2-D equations for incompressible stratified fluid. The area considered is located between the Spitsbergen (Svalbard) Island and the Franz-Victoria Trough with a cross-section of 350 km length. There are two underwater hills about 100–150 m high on the background depth of about 300 m. It is shown that intensive nonlinear internal waves with amplitudes up to 50 m and lengths of about 6–12 km are generated in this zone. The total height of such waves is huge and they must be considered as a significant factor of the environment in this basin.

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