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Contribution of changes in atmospheric circulation patterns to extreme temperature trends

Daniel E. Horton (), Nathaniel C. Johnson, Deepti Singh, Daniel L. Swain, Bala Rajaratnam and Noah S. Diffenbaugh
Additional contact information
Daniel E. Horton: Stanford University
Nathaniel C. Johnson: International Pacific Research Center, University of Hawaii at Manoa
Deepti Singh: Stanford University
Daniel L. Swain: Stanford University
Bala Rajaratnam: Stanford University
Noah S. Diffenbaugh: Stanford University

Nature, 2015, vol. 522, issue 7557, 465-469

Abstract: This study identifies statistically significant trends in mid-atmospheric circulation patterns that partially explain observed changes in extreme temperature occurrence over Eurasia and North America; although the underlying cause of circulation pattern trends remains uncertain, most extreme temperature trends are shown to be consistent with thermodynamic warming.

Date: 2015
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DOI: 10.1038/nature14550

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