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Forecasting extreme stratospheric polar vortex events

Abstract:
Extreme polar vortex events known as sudden stratospheric warmings can influence surface winter weather conditions, but their timing is difficult to predict. Here, we examine factors that influence their occurrence, with a focus on their timing and vertical extent. We consider the roles of the troposphere and equatorial stratosphere separately, using a split vortex event in January 2009 as the primary case study. This event cannot be reproduced by constraining wind and temperatures in the troposphere alone, even when the equatorial lower stratosphere is in the correct phase of the quasi biennial oscillation. When the flow in the equatorial upper stratosphere is also constrained, the timing and spatial evolution of the vortex event is captured remarkably well. This highlights an influence from this region previously unrecognised by the seasonal forecast community. We suggest that better representation of the flow in this region is likely to improve predictability of extreme polar vortex events and hence their associated impacts at the surface.
Publication status:
Published
Peer review status:
Peer reviewed

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Publisher copy:
10.1038/s41467-020-18299-7

Authors


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Institution:
University of Oxford
Division:
MPLS
Department:
Physics
Sub department:
Atmos Ocean & Planet Physics
Oxford college:
St Cross College
Role:
Author
ORCID:
0000-0002-7803-9277
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Role:
Author
ORCID:
0000-0003-1127-0279
More by this author
Role:
Author
ORCID:
0000-0001-9485-5082


Publisher:
Springer Nature
Journal:
Nature Communications More from this journal
Volume:
11
Issue:
1
Article number:
4630
Publication date:
2020-09-15
Acceptance date:
2020-08-14
DOI:
EISSN:
2041-1723
Pmid:
32934223


Language:
English
Keywords:
Pubs id:
1132653
Local pid:
pubs:1132653
Deposit date:
2020-10-28

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