Revisiting the Identification of Wintertime Atmospheric Circulation Regimes in the Euro-Atlantic Sector
Swinda K.J. Falkena, Jana de Wiljes, Antje Weisheimer, Theodore G., Shepherd

TL;DR
This study revisits the identification of winter atmospheric circulation regimes in the Euro-Atlantic sector, revealing six regimes instead of four and demonstrating that incorporating a persistence constraint improves regime stability.
Contribution
It introduces a new clustering approach using full field data and a persistence constraint, leading to more accurate and stable regime identification than traditional EOF-based methods.
Findings
Six regimes identified instead of four with full data clustering.
Opposite regimes exhibit symmetry, enhancing understanding of circulation patterns.
Persistence constraints extend regime durations without altering occurrence rates.
Abstract
Atmospheric circulation is often clustered in so-called circulation regimes, which are persistent and recurrent patterns. For the Euro-Atlantic sector in winter, most studies identify four regimes: the Atlantic Ridge, the Scandinavian Blocking and the two phases of the North Atlantic Oscillation. These results are obtained by applying k-means clustering to the first several empirical orthogonal functions (EOFs) of geopotential height data. Studying the observed circulation in reanalysis data, it is found that when the full field data is used for the k-means cluster analysis instead of the EOFs, the optimal number of clusters is no longer four but six. The two extra regimes that are found are the opposites of the Atlantic Ridge and Scandinavian Blocking, meaning they have a low-pressure area roughly where the original regimes have a high-pressure area. This introduces an appealing…
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