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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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 |
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Open Polar |
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Max Planck Society: MPG.PuRe |
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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 |
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11 |
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1 |
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1775348401669406720 |