The downward influence of stratospheric sudden warmings
<jats:title>Abstract</jats:title> <jats:p>The coupling between the stratosphere and the troposphere following two major stratospheric sudden warmings is studied in the Canadian Middle Atmosphere Model using a nudging technique by which the zonal-mean evolution of the reference sudd...
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ftunivcam:oai:www.repository.cam.ac.uk:1810/245496 2024-02-04T10:02:49+01:00 The downward influence of stratospheric sudden warmings Hitchcock, P Simpson, IR 2014 application/pdf https://www.repository.cam.ac.uk/handle/1810/245496 English eng eng American Meteorological Society http://dx.doi.org/10.1175/jas-d-14-0012.1 Journal of the Atmospheric Sciences https://www.repository.cam.ac.uk/handle/1810/245496 DSpace@Cambridge license 37 Earth Sciences 3708 Oceanography 3701 Atmospheric Sciences Article 2014 ftunivcam 2024-01-11T23:24:42Z <jats:title>Abstract</jats:title> <jats:p>The coupling between the stratosphere and the troposphere following two major stratospheric sudden warmings is studied in the Canadian Middle Atmosphere Model using a nudging technique by which the zonal-mean evolution of the reference sudden warmings are artificially induced in an ~100-member ensemble spun off from a control simulation. Both reference warmings are taken from a freely running integration of the model. One event is a displacement, the other is a split, and both are followed by extended recoveries in the lower stratosphere. The methodology permits a statistically robust study of their influence on the troposphere below.</jats:p> <jats:p>The nudged ensembles exhibit a tropospheric annular mode response closely analogous to that seen in observations, confirming the downward influence of sudden warmings on the troposphere in a comprehensive model. This tropospheric response coincides more closely with the lower-stratospheric annular mode anomalies than with the midstratospheric wind reversal. In addition to the expected synoptic-scale eddy feedback, the planetary-scale eddies also reinforce the tropospheric wind changes, apparently responding directly to the stratospheric anomalies.</jats:p> <jats:p>Furthermore, despite the zonal symmetry of the stratospheric perturbation, a highly zonally asymmetric near-surface response is produced, corresponding to a strongly negative phase of the North Atlantic Oscillation with a much weaker response over the Pacific basin that matches composites of sudden warmings from the Interim ECMWF Re-Analysis (ERA-Interim). Phase 5 of the Coupled Model Intercomparison Project models exhibit a similar response, though in most models the response’s magnitude is underrepresented.</jats:p> PH acknowledges support from ERC project no 267760 - ACCI and an NSERC Postdoctoral Fellowship. IRS was supported by a Lamont-Doherty Earth Observatory postdoctoral fellowship and NSF award ... Article in Journal/Newspaper North Atlantic North Atlantic oscillation Apollo - University of Cambridge Repository Pacific |
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Apollo - University of Cambridge Repository |
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language |
English |
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37 Earth Sciences 3708 Oceanography 3701 Atmospheric Sciences |
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37 Earth Sciences 3708 Oceanography 3701 Atmospheric Sciences Hitchcock, P Simpson, IR The downward influence of stratospheric sudden warmings |
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37 Earth Sciences 3708 Oceanography 3701 Atmospheric Sciences |
description |
<jats:title>Abstract</jats:title> <jats:p>The coupling between the stratosphere and the troposphere following two major stratospheric sudden warmings is studied in the Canadian Middle Atmosphere Model using a nudging technique by which the zonal-mean evolution of the reference sudden warmings are artificially induced in an ~100-member ensemble spun off from a control simulation. Both reference warmings are taken from a freely running integration of the model. One event is a displacement, the other is a split, and both are followed by extended recoveries in the lower stratosphere. The methodology permits a statistically robust study of their influence on the troposphere below.</jats:p> <jats:p>The nudged ensembles exhibit a tropospheric annular mode response closely analogous to that seen in observations, confirming the downward influence of sudden warmings on the troposphere in a comprehensive model. This tropospheric response coincides more closely with the lower-stratospheric annular mode anomalies than with the midstratospheric wind reversal. In addition to the expected synoptic-scale eddy feedback, the planetary-scale eddies also reinforce the tropospheric wind changes, apparently responding directly to the stratospheric anomalies.</jats:p> <jats:p>Furthermore, despite the zonal symmetry of the stratospheric perturbation, a highly zonally asymmetric near-surface response is produced, corresponding to a strongly negative phase of the North Atlantic Oscillation with a much weaker response over the Pacific basin that matches composites of sudden warmings from the Interim ECMWF Re-Analysis (ERA-Interim). Phase 5 of the Coupled Model Intercomparison Project models exhibit a similar response, though in most models the response’s magnitude is underrepresented.</jats:p> PH acknowledges support from ERC project no 267760 - ACCI and an NSERC Postdoctoral Fellowship. IRS was supported by a Lamont-Doherty Earth Observatory postdoctoral fellowship and NSF award ... |
format |
Article in Journal/Newspaper |
author |
Hitchcock, P Simpson, IR |
author_facet |
Hitchcock, P Simpson, IR |
author_sort |
Hitchcock, P |
title |
The downward influence of stratospheric sudden warmings |
title_short |
The downward influence of stratospheric sudden warmings |
title_full |
The downward influence of stratospheric sudden warmings |
title_fullStr |
The downward influence of stratospheric sudden warmings |
title_full_unstemmed |
The downward influence of stratospheric sudden warmings |
title_sort |
downward influence of stratospheric sudden warmings |
publisher |
American Meteorological Society |
publishDate |
2014 |
url |
https://www.repository.cam.ac.uk/handle/1810/245496 |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
North Atlantic North Atlantic oscillation |
genre_facet |
North Atlantic North Atlantic oscillation |
op_relation |
https://www.repository.cam.ac.uk/handle/1810/245496 |
op_rights |
DSpace@Cambridge license |
_version_ |
1789969780802846720 |