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fbtwitterlinkedinvimeoflicker grey 14rssslideshare1
Polyakov, Igorv (1994)
Publisher: Co-Action Publishing
Journal: Polar Research
Languages: English
Types: Article

Classified by OpenAIRE into

arxiv: Physics::Atmospheric and Oceanic Physics, Physics::Geophysics, Astrophysics::Earth and Planetary Astrophysics, Physics::Fluid Dynamics
A three-dimensional structure of the M2 tidal currents has been reproduced by mathematical modelling. The possibility of energy transfer from the tidal barotropic motion to large-scale baroclinic circulation of the Arctic Ocean has been estimated. It has been shown that the bottom relief plays an important role in the formation of the large-scale pattern of the baroclinic fields. The hypothesis has been proposed that the M2 tide may support the near-slope convection of the East-Siberian and Laptev seas. Polar Research13 (2), 219–232
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