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

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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 100g-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. © 2011 Author(s).

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Kurkina, O. E., & Talipova, T. G. (2011). Huge internal waves in the vicinity of the Spitsbergen Island (Barents Sea). Natural Hazards and Earth System Science, 11(3), 981–986. https://doi.org/10.5194/nhess-11-981-2011

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