A GCM study of the influence of equatorial winds on the timing of sudden stratospheric warmings

A full troposphere-stratosphere-mesosphere global circulation model is used in a set of idealised experiments to investigate the sensitivity of the Northern Hemisphere winter stratospheric flow to improvements in the equatorial zonal winds. The model shows significant sensitivity to variability in t...

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Main Authors: Pascoe, C, Gray, L, Scaife, A
Format: Journal article
Language:English
Published: 2006
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author Pascoe, C
Gray, L
Scaife, A
author_facet Pascoe, C
Gray, L
Scaife, A
author_sort Pascoe, C
collection OXFORD
description A full troposphere-stratosphere-mesosphere global circulation model is used in a set of idealised experiments to investigate the sensitivity of the Northern Hemisphere winter stratospheric flow to improvements in the equatorial zonal winds. The model shows significant sensitivity to variability in the upper equatorial stratosphere, the imposition of SAO and QBO like variability in this region advances the timing of midwinter sudden warmings by about one month. Perturbations to the lower equatorial stratosphere are mainly found to influence early winter polar variability. These results suggest that it is important to pay attention to the capability of models to simulate realistic variability in the upper equatorial stratosphere. Copyright 2006 by the American Geophysical Union.
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spelling oxford-uuid:c75d8f08-30de-4a38-8862-23c74ac9978d2022-03-27T06:44:30ZA GCM study of the influence of equatorial winds on the timing of sudden stratospheric warmingsJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:c75d8f08-30de-4a38-8862-23c74ac9978dEnglishSymplectic Elements at Oxford2006Pascoe, CGray, LScaife, AA full troposphere-stratosphere-mesosphere global circulation model is used in a set of idealised experiments to investigate the sensitivity of the Northern Hemisphere winter stratospheric flow to improvements in the equatorial zonal winds. The model shows significant sensitivity to variability in the upper equatorial stratosphere, the imposition of SAO and QBO like variability in this region advances the timing of midwinter sudden warmings by about one month. Perturbations to the lower equatorial stratosphere are mainly found to influence early winter polar variability. These results suggest that it is important to pay attention to the capability of models to simulate realistic variability in the upper equatorial stratosphere. Copyright 2006 by the American Geophysical Union.
spellingShingle Pascoe, C
Gray, L
Scaife, A
A GCM study of the influence of equatorial winds on the timing of sudden stratospheric warmings
title A GCM study of the influence of equatorial winds on the timing of sudden stratospheric warmings
title_full A GCM study of the influence of equatorial winds on the timing of sudden stratospheric warmings
title_fullStr A GCM study of the influence of equatorial winds on the timing of sudden stratospheric warmings
title_full_unstemmed A GCM study of the influence of equatorial winds on the timing of sudden stratospheric warmings
title_short A GCM study of the influence of equatorial winds on the timing of sudden stratospheric warmings
title_sort gcm study of the influence of equatorial winds on the timing of sudden stratospheric warmings
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