Sensitivity of QBO teleconnection to model circulation biases

The Quasi-biennial oscillation (QBO) in the equatorial stratospheric winds is known to modulate the extratropical atmospheric circulation so that an easterly QBO phase is associated with a weaker Arctic stratospheric vortex and a negative North Atlantic Oscillation in winter. The link can potentiall...

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Published in:Scientific Reports
Main Authors: Karpechko, A., Tyrrell, N., Rast, S.
Format: Article in Journal/Newspaper
Language:English
Published: 2021
Subjects:
Online Access:http://hdl.handle.net/21.11116/0000-0008-34F4-A
http://hdl.handle.net/21.11116/0000-000C-D543-8
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record_format openpolar
spelling ftpubman:oai:pure.mpg.de:item_3291604 2023-08-27T04:07:40+02:00 Sensitivity of QBO teleconnection to model circulation biases Karpechko, A. Tyrrell, N. Rast, S. 2021-04 application/pdf http://hdl.handle.net/21.11116/0000-0008-34F4-A http://hdl.handle.net/21.11116/0000-000C-D543-8 eng eng info:eu-repo/semantics/altIdentifier/doi/10.1002/qj.4014 http://hdl.handle.net/21.11116/0000-0008-34F4-A http://hdl.handle.net/21.11116/0000-000C-D543-8 Quarterly Journal of the Royal Meteorological Society info:eu-repo/semantics/article 2021 ftpubman https://doi.org/10.1002/qj.4014 2023-08-02T01:44:53Z The Quasi-biennial oscillation (QBO) in the equatorial stratospheric winds is known to modulate the extratropical atmospheric circulation so that an easterly QBO phase is associated with a weaker Arctic stratospheric vortex and a negative North Atlantic Oscillation in winter. The link can potentially be used to improve seasonal forecasts and is usually captured by climate models but with a smaller magnitude than that in observations. Here, the sensitivity of the QBO teleconnection to biases in model circulation is explored in an atmosphere-only model ECHAM6 with an internally generated QBO, by contrasting simulations by an original, biased model, and a model version in which biases are artificially reduced. We find that the strength of the winter mean Arctic stratospheric vortex response is better reproduced by the bias-corrected model. On the other hand, the response is delayed by 1 month and there is no improvement in the tropospheric response. Stronger response of the polar vortex in the bias-corrected model is likely associated with larger magnitude of QBO winds and better-represented stratospheric mean climate and planetary wave fluxes, but the exact mechanism remains unclear. The results of this study have implications for seasonal forecast model development. © 2021 Royal Meteorological Society. Article in Journal/Newspaper Arctic North Atlantic North Atlantic oscillation Max Planck Society: MPG.PuRe Arctic Scientific Reports 11 1
institution Open Polar
collection Max Planck Society: MPG.PuRe
op_collection_id ftpubman
language English
description The Quasi-biennial oscillation (QBO) in the equatorial stratospheric winds is known to modulate the extratropical atmospheric circulation so that an easterly QBO phase is associated with a weaker Arctic stratospheric vortex and a negative North Atlantic Oscillation in winter. The link can potentially be used to improve seasonal forecasts and is usually captured by climate models but with a smaller magnitude than that in observations. Here, the sensitivity of the QBO teleconnection to biases in model circulation is explored in an atmosphere-only model ECHAM6 with an internally generated QBO, by contrasting simulations by an original, biased model, and a model version in which biases are artificially reduced. We find that the strength of the winter mean Arctic stratospheric vortex response is better reproduced by the bias-corrected model. On the other hand, the response is delayed by 1 month and there is no improvement in the tropospheric response. Stronger response of the polar vortex in the bias-corrected model is likely associated with larger magnitude of QBO winds and better-represented stratospheric mean climate and planetary wave fluxes, but the exact mechanism remains unclear. The results of this study have implications for seasonal forecast model development. © 2021 Royal Meteorological Society.
format Article in Journal/Newspaper
author Karpechko, A.
Tyrrell, N.
Rast, S.
spellingShingle Karpechko, A.
Tyrrell, N.
Rast, S.
Sensitivity of QBO teleconnection to model circulation biases
author_facet Karpechko, A.
Tyrrell, N.
Rast, S.
author_sort Karpechko, A.
title Sensitivity of QBO teleconnection to model circulation biases
title_short Sensitivity of QBO teleconnection to model circulation biases
title_full Sensitivity of QBO teleconnection to model circulation biases
title_fullStr Sensitivity of QBO teleconnection to model circulation biases
title_full_unstemmed Sensitivity of QBO teleconnection to model circulation biases
title_sort sensitivity of qbo teleconnection to model circulation biases
publishDate 2021
url http://hdl.handle.net/21.11116/0000-0008-34F4-A
http://hdl.handle.net/21.11116/0000-000C-D543-8
geographic Arctic
geographic_facet Arctic
genre Arctic
North Atlantic
North Atlantic oscillation
genre_facet Arctic
North Atlantic
North Atlantic oscillation
op_source Quarterly Journal of the Royal Meteorological Society
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1002/qj.4014
http://hdl.handle.net/21.11116/0000-0008-34F4-A
http://hdl.handle.net/21.11116/0000-000C-D543-8
op_doi https://doi.org/10.1002/qj.4014
container_title Scientific Reports
container_volume 11
container_issue 1
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