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Contribution of changes in atmospheric circulation patterns to extreme temperature trends

TitleContribution of changes in atmospheric circulation patterns to extreme temperature trends
Publication TypeJournal Article
Year of Publication2015
AuthorsHorton D.E, Johnson N.C, Singh D., Swain D.L, Rajaratnam B., Diffenbaugh N.S
Date Published2015/06
Type of ArticleArticle
ISBN Number0028-0836
Accession NumberWOS:000356782900047
Keywordsamplification; arctic sea-ice; global climate-change; midlatitude weather; planetary-waves; uncertainty; weather extremes; winters

Surface weather conditions are closely governed by the large-scale circulation of the Earth's atmosphere. Recent increases in the occurrence of some extreme weather phenomena(1,2) have led to multiple mechanistic hypotheses linking changes in atmospheric circulation to increasing probability of extreme events(3-5). However, observed evidence of long-term change in atmospheric circulation remains inconclusive(6-8). Here we identify statistically significant trends in the occurrence of atmospheric circulation patterns, which partially explain observed trends in surface temperature extremes over seven mid-latitude regions of the Northern Hemisphere. Using self-organizing map cluster analysis(9-12), we detect robust circulation pattern trends in a subset of these regions during both the satellite observation era (1979-2013) and the recent period of rapid Arctic sea-ice decline (1990-2013). Particularly substantial influences include the contribution of increasing trends in anticyclonic circulations to summer and autumn hot extremes over portions of Eurasia and North America, and the contribution of increasing trends in northerly flow to winter cold extremes over central Asia. Our results indicate that although a substantial portion of the observed change in extreme temperature occurrence has resulted from regional-and global-scale thermodynamic changes, the risk of extreme temperatures over some regions has also been altered by recent changes in the frequency, persistence and maximum duration of regional circulation patterns.

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