A regional mathematical model of the lower atmosphere’s wind system, built previously at the Polar Geophysical Institute, is used to explore the early stages of the genesis of polar lows at European Arctic latitudes. The mathematical model generates three-dimensional distributions of atmospheric parameters in the height range of 0 to 15 km over a constrained region of the Earth’s surface by numerically solving nonsimplified gas dynamic equations. The establishment of a polar low can be triggered by the emergence of a convexity in the arctic front’s shape during a one-day period, according to simulation data.

Author (s) Details

Igor V. Mingalev
Polar Geophysical Institute, Russian Academy of Sciences, Academgorodok Str. 26a,  Apatity 184209, Murmansk Region, Russia and Apatity Branch of the Murmansk Arctic State University, Lesnaiy Str. 29, Apatity 184209, Murmansk Region, Russia.

Konstantin G. Orlov
Polar Geophysical Institute, Russian Academy of Sciences, Academgorodok Str. 26a, Apatity 184209, Murmansk Region, Russia.

Victor S. Mingalev
Polar Geophysical Institute, Russian Academy of Sciences, Academgorodok Str. 26a, Apatity 184209, Murmansk Region, Russia.

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