Morphometry and Internal Structure of Stamukhas in the Ice-covered Seas of Russia

Morphometry and Internal Structure of Stamukhas in the Ice-covered Seas of Russia

A method for studying stamukhas using the modern field equipment is considered. The peculiarities of morphometric characteristics and parameters of the internal structure of stamukhas are analyzed. The interrelation between the consolidated layer thickness and the accumulated freezing degree days is...

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Veröffentlicht in:Russian meteorology and hydrology 2020-04, Vol.45 (4), p.260-268
Hauptverfasser: Mironov, E. U., Guzenko, R. B., Porubaev, V. S., Kharitonov, V. V., Kornishin, K. A., Efimov, Ya. O.
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Atmospheric Sciences
Earth and Environmental Science
Earth Sciences
Meteorology
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container_end_page 268
container_issue 4
container_start_page 260
container_title Russian meteorology and hydrology
container_volume 45
creator Mironov, E. U.
Guzenko, R. B.
Porubaev, V. S.
Kharitonov, V. V.
Kornishin, K. A.
Efimov, Ya. O.
description A method for studying stamukhas using the modern field equipment is considered. The peculiarities of morphometric characteristics and parameters of the internal structure of stamukhas are analyzed. The interrelation between the consolidated layer thickness and the accumulated freezing degree days is derived for different seas. The comparative analysis of morphometric characteristics and the consolidated layer in the ice-covered seas of Russia is carried out. It is shown that the formation of stamukhas in different regions has specific features depending on the depth, bottom topography, drift characteristics, ice thickness, and dates of fast ice formation. The maximum thickness of the consolidated layer is registered in the Kara and Laptev seas.
doi_str_mv 10.3103/S1068373920040068
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Earth and Environmental Science
Earth Sciences
Meteorology
title Morphometry and Internal Structure of Stamukhas in the Ice-covered Seas of Russia
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