Projected changes in persistent extreme summer weather events: The role of quasi-resonant amplification
Persistent episodes of extreme weather in the Northern Hemisphere summer have been associated with highamplitude quasi-stationary atmospheric Rossby waves, with zonal wave numbers 6 to 8 resulting from the phenomenon of quasi-resonant amplification (QRA). A fingerprint for the occurrence of QRA can...
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ftleibnizopen:oai:oai.leibnizopen.de:ri_SeYsBBwLIz6xGTeq7 2023-11-12T04:12:24+01:00 Projected changes in persistent extreme summer weather events: The role of quasi-resonant amplification Mann, Michael E. Rahmstorf, Stefan Kornhuber, Kai Steinman, Byron A. Miller, Sonya K. Petri, Stefan Coumou, Dim 2018 application/pdf https://oa.tib.eu/renate/handle/123456789/11332 https://doi.org/10.34657/10367 eng eng Washington, DC [u.a.] : Assoc. CC BY-NC 4.0 Unported https://creativecommons.org/licenses/by-nc/4.0 Science Advances 4 (2018), Nr. 10 Anthropogenic aerosols Business-as-usual Coupled Model Intercomparison Project Extreme weather events Northern Hemispheres Quasi-stationary Radiative forcings Surface temperatures 500 333.7 570 article Text 2018 ftleibnizopen https://doi.org/10.34657/10367 2023-10-30T00:36:20Z Persistent episodes of extreme weather in the Northern Hemisphere summer have been associated with highamplitude quasi-stationary atmospheric Rossby waves, with zonal wave numbers 6 to 8 resulting from the phenomenon of quasi-resonant amplification (QRA). A fingerprint for the occurrence of QRA can be defined in terms of the zonally averaged surface temperature field. Examining state-of-the-art [Coupled Model Intercomparison Project Phase 5 (CMIP5)] climate model projections, we find that QRA events are likely to increase by ∼50% this century under business-as-usual carbon emissions, but there is considerable variation among climate models. Some predict a near tripling of QRA events by the end of the century, while others predict a potential decrease. Models with amplified Arctic warming yield the most pronounced increase in QRA events. The projections are strongly dependent on assumptions regarding the nature of changes in radiative forcing associated with anthropogenic aerosols over the next century. One implication of our findings is that a reduction in midlatitude aerosol loading could actually lead to Arctic de-amplification this century, ameliorating potential increases in persistent extreme weather events. publishedVersion Article in Journal/Newspaper Arctic Unknown |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
ftleibnizopen |
language |
English |
topic |
Anthropogenic aerosols Business-as-usual Coupled Model Intercomparison Project Extreme weather events Northern Hemispheres Quasi-stationary Radiative forcings Surface temperatures 500 333.7 570 |
spellingShingle |
Anthropogenic aerosols Business-as-usual Coupled Model Intercomparison Project Extreme weather events Northern Hemispheres Quasi-stationary Radiative forcings Surface temperatures 500 333.7 570 Mann, Michael E. Rahmstorf, Stefan Kornhuber, Kai Steinman, Byron A. Miller, Sonya K. Petri, Stefan Coumou, Dim Projected changes in persistent extreme summer weather events: The role of quasi-resonant amplification |
topic_facet |
Anthropogenic aerosols Business-as-usual Coupled Model Intercomparison Project Extreme weather events Northern Hemispheres Quasi-stationary Radiative forcings Surface temperatures 500 333.7 570 |
description |
Persistent episodes of extreme weather in the Northern Hemisphere summer have been associated with highamplitude quasi-stationary atmospheric Rossby waves, with zonal wave numbers 6 to 8 resulting from the phenomenon of quasi-resonant amplification (QRA). A fingerprint for the occurrence of QRA can be defined in terms of the zonally averaged surface temperature field. Examining state-of-the-art [Coupled Model Intercomparison Project Phase 5 (CMIP5)] climate model projections, we find that QRA events are likely to increase by ∼50% this century under business-as-usual carbon emissions, but there is considerable variation among climate models. Some predict a near tripling of QRA events by the end of the century, while others predict a potential decrease. Models with amplified Arctic warming yield the most pronounced increase in QRA events. The projections are strongly dependent on assumptions regarding the nature of changes in radiative forcing associated with anthropogenic aerosols over the next century. One implication of our findings is that a reduction in midlatitude aerosol loading could actually lead to Arctic de-amplification this century, ameliorating potential increases in persistent extreme weather events. publishedVersion |
format |
Article in Journal/Newspaper |
author |
Mann, Michael E. Rahmstorf, Stefan Kornhuber, Kai Steinman, Byron A. Miller, Sonya K. Petri, Stefan Coumou, Dim |
author_facet |
Mann, Michael E. Rahmstorf, Stefan Kornhuber, Kai Steinman, Byron A. Miller, Sonya K. Petri, Stefan Coumou, Dim |
author_sort |
Mann, Michael E. |
title |
Projected changes in persistent extreme summer weather events: The role of quasi-resonant amplification |
title_short |
Projected changes in persistent extreme summer weather events: The role of quasi-resonant amplification |
title_full |
Projected changes in persistent extreme summer weather events: The role of quasi-resonant amplification |
title_fullStr |
Projected changes in persistent extreme summer weather events: The role of quasi-resonant amplification |
title_full_unstemmed |
Projected changes in persistent extreme summer weather events: The role of quasi-resonant amplification |
title_sort |
projected changes in persistent extreme summer weather events: the role of quasi-resonant amplification |
publisher |
Washington, DC [u.a.] : Assoc. |
publishDate |
2018 |
url |
https://oa.tib.eu/renate/handle/123456789/11332 https://doi.org/10.34657/10367 |
genre |
Arctic |
genre_facet |
Arctic |
op_source |
Science Advances 4 (2018), Nr. 10 |
op_rights |
CC BY-NC 4.0 Unported https://creativecommons.org/licenses/by-nc/4.0 |
op_doi |
https://doi.org/10.34657/10367 |
_version_ |
1782330955581620224 |