The Downward Influence of Stratospheric Sudden Warmings

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 ensem...

Full description

Bibliographic Details
Main Authors: Hitchcock, Peter, Simpson, Isla R.
Format: Article in Journal/Newspaper
Language:English
Published: American Meteorological Society 2014
Subjects:
Online Access:https://doi.org/10.7916/D8PV6JWD
id ftcolumbiauniv:oai:academiccommons.columbia.edu:10.7916/D8PV6JWD
record_format openpolar
spelling ftcolumbiauniv:oai:academiccommons.columbia.edu:10.7916/D8PV6JWD 2023-05-15T17:34:25+02:00 The Downward Influence of Stratospheric Sudden Warmings Hitchcock, Peter Simpson, Isla R. 2014 https://doi.org/10.7916/D8PV6JWD English eng American Meteorological Society https://doi.org/10.7916/D8PV6JWD Meteorology Atmosphere Upper Mathematics Articles 2014 ftcolumbiauniv https://doi.org/10.7916/D8PV6JWD 2019-04-04T08:13:28Z 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. 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. 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. Article in Journal/Newspaper North Atlantic North Atlantic oscillation Columbia University: Academic Commons Pacific
institution Open Polar
collection Columbia University: Academic Commons
op_collection_id ftcolumbiauniv
language English
topic Meteorology
Atmosphere
Upper
Mathematics
spellingShingle Meteorology
Atmosphere
Upper
Mathematics
Hitchcock, Peter
Simpson, Isla R.
The Downward Influence of Stratospheric Sudden Warmings
topic_facet Meteorology
Atmosphere
Upper
Mathematics
description 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. 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. 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.
format Article in Journal/Newspaper
author Hitchcock, Peter
Simpson, Isla R.
author_facet Hitchcock, Peter
Simpson, Isla R.
author_sort Hitchcock, Peter
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://doi.org/10.7916/D8PV6JWD
geographic Pacific
geographic_facet Pacific
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_relation https://doi.org/10.7916/D8PV6JWD
op_doi https://doi.org/10.7916/D8PV6JWD
_version_ 1766133237226143744