Stratospheric Harbingers of Anomalous Weather Regimes

Observations show that large variations in the strength of the stratospheric circulation, appearing first above ∼50 kilometers, descend to the lowermost stratosphere and are followed by anomalous tropospheric weather regimes. During the 60 days after the onset of these events, average surface pressu...

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Published in:Science
Main Authors: Baldwin, Mark P., Dunkerton, Timothy J.
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 2001
Subjects:
Online Access:http://dx.doi.org/10.1126/science.1063315
https://www.science.org/doi/pdf/10.1126/science.1063315
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spelling craaas:10.1126/science.1063315 2024-06-23T07:49:40+00:00 Stratospheric Harbingers of Anomalous Weather Regimes Baldwin, Mark P. Dunkerton, Timothy J. 2001 http://dx.doi.org/10.1126/science.1063315 https://www.science.org/doi/pdf/10.1126/science.1063315 en eng American Association for the Advancement of Science (AAAS) Science volume 294, issue 5542, page 581-584 ISSN 0036-8075 1095-9203 journal-article 2001 craaas https://doi.org/10.1126/science.1063315 2024-06-13T04:01:44Z Observations show that large variations in the strength of the stratospheric circulation, appearing first above ∼50 kilometers, descend to the lowermost stratosphere and are followed by anomalous tropospheric weather regimes. During the 60 days after the onset of these events, average surface pressure maps resemble closely the Arctic Oscillation pattern. These stratospheric events also precede shifts in the probability distributions of extreme values of the Arctic and North Atlantic Oscillations, the location of storm tracks, and the local likelihood of mid-latitude storms. Our observations suggest that these stratospheric harbingers may be used as a predictor of tropospheric weather regimes. Article in Journal/Newspaper Arctic North Atlantic AAAS Resource Center (American Association for the Advancement of Science) Arctic Science 294 5542 581 584
institution Open Polar
collection AAAS Resource Center (American Association for the Advancement of Science)
op_collection_id craaas
language English
description Observations show that large variations in the strength of the stratospheric circulation, appearing first above ∼50 kilometers, descend to the lowermost stratosphere and are followed by anomalous tropospheric weather regimes. During the 60 days after the onset of these events, average surface pressure maps resemble closely the Arctic Oscillation pattern. These stratospheric events also precede shifts in the probability distributions of extreme values of the Arctic and North Atlantic Oscillations, the location of storm tracks, and the local likelihood of mid-latitude storms. Our observations suggest that these stratospheric harbingers may be used as a predictor of tropospheric weather regimes.
format Article in Journal/Newspaper
author Baldwin, Mark P.
Dunkerton, Timothy J.
spellingShingle Baldwin, Mark P.
Dunkerton, Timothy J.
Stratospheric Harbingers of Anomalous Weather Regimes
author_facet Baldwin, Mark P.
Dunkerton, Timothy J.
author_sort Baldwin, Mark P.
title Stratospheric Harbingers of Anomalous Weather Regimes
title_short Stratospheric Harbingers of Anomalous Weather Regimes
title_full Stratospheric Harbingers of Anomalous Weather Regimes
title_fullStr Stratospheric Harbingers of Anomalous Weather Regimes
title_full_unstemmed Stratospheric Harbingers of Anomalous Weather Regimes
title_sort stratospheric harbingers of anomalous weather regimes
publisher American Association for the Advancement of Science (AAAS)
publishDate 2001
url http://dx.doi.org/10.1126/science.1063315
https://www.science.org/doi/pdf/10.1126/science.1063315
geographic Arctic
geographic_facet Arctic
genre Arctic
North Atlantic
genre_facet Arctic
North Atlantic
op_source Science
volume 294, issue 5542, page 581-584
ISSN 0036-8075 1095-9203
op_doi https://doi.org/10.1126/science.1063315
container_title Science
container_volume 294
container_issue 5542
container_start_page 581
op_container_end_page 584
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