New metrics and evidence are presented that support a linkage between rapid Arctic warming, relative to Northern hemisphere mid-latitudes, and more frequent high-amplitude (wavy) jet-stream configurations that favor persistent weather patterns. We find robust relationships among seasonal and regional patterns of weaker poleward thickness gradients, weaker zonal upper-level winds, and a more meridional flow direction. These results suggest that as the Arctic continues to warm faster than elsewhere in response to rising greenhouse-gas concentrations, the frequency of extreme weather events caused by persistent jet-stream patterns will increase.
%0 Journal Article
%1 Francis2015Evidence
%A Francis, Jennifer A.
%A Vavrus, Stephen J.
%D 2015
%J Environmental Research Letters
%K Arctic MySeclifirmWTwork MyUKCPStorylinesWork climatechange dynamics jet seaice
%N 1
%P 014005+
%R 10.1088/1748-9326/10/1/014005
%T Evidence for a wavier jet stream in response to rapid Arctic warming
%U http://dx.doi.org/10.1088/1748-9326/10/1/014005
%V 10
%X New metrics and evidence are presented that support a linkage between rapid Arctic warming, relative to Northern hemisphere mid-latitudes, and more frequent high-amplitude (wavy) jet-stream configurations that favor persistent weather patterns. We find robust relationships among seasonal and regional patterns of weaker poleward thickness gradients, weaker zonal upper-level winds, and a more meridional flow direction. These results suggest that as the Arctic continues to warm faster than elsewhere in response to rising greenhouse-gas concentrations, the frequency of extreme weather events caused by persistent jet-stream patterns will increase.
@article{Francis2015Evidence,
abstract = {New metrics and evidence are presented that support a linkage between rapid Arctic warming, relative to Northern hemisphere mid-latitudes, and more frequent high-amplitude (wavy) jet-stream configurations that favor persistent weather patterns. We find robust relationships among seasonal and regional patterns of weaker poleward thickness gradients, weaker zonal upper-level winds, and a more meridional flow direction. These results suggest that as the Arctic continues to warm faster than elsewhere in response to rising greenhouse-gas concentrations, the frequency of extreme weather events caused by persistent jet-stream patterns will increase.},
added-at = {2018-06-18T21:23:34.000+0200},
author = {Francis, Jennifer A. and Vavrus, Stephen J.},
biburl = {https://www.bibsonomy.org/bibtex/212d675f812ada97ddbcafcd4230a7ec8/pbett},
citeulike-article-id = {13474771},
citeulike-linkout-0 = {http://dx.doi.org/10.1088/1748-9326/10/1/014005},
citeulike-linkout-1 = {http://iopscience.iop.org/1748-9326/10/1/014005},
comment = {(private-note)See also http://www.bbc.co.uk/news/science-environment-26023166},
day = 01,
doi = {10.1088/1748-9326/10/1/014005},
interhash = {a9f0538637703d16868fc6a49ea7fd1f},
intrahash = {12d675f812ada97ddbcafcd4230a7ec8},
issn = {1748-9326},
journal = {Environmental Research Letters},
keywords = {Arctic MySeclifirmWTwork MyUKCPStorylinesWork climatechange dynamics jet seaice},
month = jan,
number = 1,
pages = {014005+},
posted-at = {2015-08-14 13:44:26},
priority = {2},
timestamp = {2020-02-27T18:18:21.000+0100},
title = {Evidence for a wavier jet stream in response to rapid Arctic warming},
url = {http://dx.doi.org/10.1088/1748-9326/10/1/014005},
volume = 10,
year = 2015
}