Features of Eddy Generation in the Barents Sea Under Conditions of the Polar Front Weakening

A study of eddy generation in the northern Barents Sea was conducted using satellite radar data in conditions of a complete absence of ice and a weakened Polar Temperature Front in July 2022. Based on the analysis of 89 satellite radar images, 598 eddy formations were identified in ice-free water. 432 eddies had a cyclonic rotation type (72%), 166 had an anticyclonic rotation type (28%). The influence of the Polar Temperature Front, wind conditions, tidal currents and bottom relief variability on eddy generation was analyzed. It was found that the main cause of eddy formation in the Barents Sea is the instability of currents resulting from their interaction with bottom relief features.

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Publication Details

Journal
Rossijskij žurnal nauk o zemle/Russian journal of earth sciences
Published
2025-08-08
DOI
https://doi.org/10.2205/2025es001008
Primary Topic
Arctic and Antarctic ice dynamics
Type
article
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article

Features of Eddy Generation in the Barents Sea Under Conditions of the Polar Front Weakening

Larisa Petrenko, Igor Kozlov, А. А. Коник
Rossijskij žurnal nauk o zemle/Russian journal of earth sciences
Arctic and Antarctic ice dynamics
article

Features of Eddy Generation in the Barents Sea Under Conditions of the Polar Front Weakening

Larisa Petrenko, Igor Kozlov, А. А. Коник
article en

Abstract

A study of eddy generation in the northern Barents Sea was conducted using satellite radar data in conditions of a complete absence of ice and a weakened Polar Temperature Front in July 2022. Based on the analysis of 89 satellite radar images, 598 eddy formations were identified in ice-free water. 432 eddies had a cyclonic rotation type (72%), 166 had an anticyclonic rotation type (28%). The influence of the Polar Temperature Front, wind conditions, tidal currents and bottom relief variability on eddy generation was analyzed. It was found that the main cause of eddy formation in the Barents Sea is the instability of currents resulting from their interaction with bottom relief features.

Rossijskij žurnal nauk o zemle/Russian journal of earth sciences
Institute of Oceanology. PP Shirshov Russian Academy of Sciences (RU)
Openalex Percentile: Top 67%
Arctic and Antarctic ice dynamics
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