Potential Links Between Tropospheric and Stratospheric Circulation Extremes During Early 2020
February‐March 2020 was marked by highly anomalous large‐scale circulations in the Northern extratropical troposphere and stratosphere. The Atlantic jet reached extreme strength, linked to some of the strongest and most persistent positive values of the Arctic Oscillation index on record, which prov...
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ftsubggeo:oai:e-docs.geo-leo.de:11858/9979 2023-05-15T15:01:56+02:00 Potential Links Between Tropospheric and Stratospheric Circulation Extremes During Early 2020 Rupp, Philip Loeffel, Sheena Garny, Hella Chen, Xiaoyang Pinto, Joaquim G. Birner, Thomas Loeffel, Sheena; 2 Deutsches Zentrum für Luft‐ und Raumfahrt (DLR) Institut für Physik der Atmosphäre Oberpfaffenhofen Germany Garny, Hella; 2 Deutsches Zentrum für Luft‐ und Raumfahrt (DLR) Institut für Physik der Atmosphäre Oberpfaffenhofen Germany Chen, Xiaoyang; 3 Institute of Meteorology and Climate Research Karlsruhe Institute of Technology Karlsruhe Germany Pinto, Joaquim G.; 3 Institute of Meteorology and Climate Research Karlsruhe Institute of Technology Karlsruhe Germany Birner, Thomas; 1 Meteorological Institute Munich Ludwig‐Maximilians‐University Munich Germany 2022-02-07 https://doi.org/10.1029/2021JD035667 http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/9979 eng eng doi:10.1029/2021JD035667 http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/9979 This is an open access article under the terms of the Creative Commons Attribution‐NonCommercial‐NoDerivs License, which permits use and distribution in any medium, provided the original work is properly cited, the use is non‐commercial and no modifications or adaptations are made. CC-BY-NC-ND ddc:551.5 strat‐trop coupling wave reflection event Arctic oscillation index stratospheric polar vortex circulation extremes ensemble simulations doc-type:article 2022 ftsubggeo https://doi.org/10.1029/2021JD035667 2022-11-09T06:51:42Z February‐March 2020 was marked by highly anomalous large‐scale circulations in the Northern extratropical troposphere and stratosphere. The Atlantic jet reached extreme strength, linked to some of the strongest and most persistent positive values of the Arctic Oscillation index on record, which provided conditions for extreme windstorms hitting Europe. Likewise, the stratospheric polar vortex reached extreme strength that persisted for an unusually long period. Past research indicated that such circulation extremes occurring throughout the troposphere‐stratosphere system are dynamically coupled, although the nature of this coupling is still not fully understood and generally difficult to quantify. We employ sets of numerical ensemble simulations to statistically characterize the mutual coupling of the early 2020 extremes. We find the extreme vortex strength to be linked to the reflection of upward propagating planetary waves and the occurrence of this reflection to be sensitive to the details of the vortex structure. Our results show an overall robust coupling between tropospheric and stratospheric anomalies: ensemble members with polar vortex exceeding a certain strength tend to exhibit a stronger tropospheric jet and vice versa. Moreover, members exhibiting a breakdown of the stratospheric circulation (e.g., sudden stratospheric warming) tend to lack periods of persistently enhanced tropospheric circulation. Despite indications for vertical coupling, our simulations underline the role of internal variability within each atmospheric layer. The circulation extremes during early 2020 may be viewed as resulting from a fortuitous alignment of dynamical evolutions within the troposphere and stratosphere, aided by each layer's modification of the other layer's boundary condition. Key Points Large‐ensemble simulations are needed to fully characterize coupled extremes in the polar vortex and tropospheric jet in early 2020. Details of the vortex structure play an important role in promoting either reflection or ... Article in Journal/Newspaper Arctic GEO-LEOe-docs (FID GEO) Arctic Journal of Geophysical Research: Atmospheres 127 3 |
institution |
Open Polar |
collection |
GEO-LEOe-docs (FID GEO) |
op_collection_id |
ftsubggeo |
language |
English |
topic |
ddc:551.5 strat‐trop coupling wave reflection event Arctic oscillation index stratospheric polar vortex circulation extremes ensemble simulations |
spellingShingle |
ddc:551.5 strat‐trop coupling wave reflection event Arctic oscillation index stratospheric polar vortex circulation extremes ensemble simulations Rupp, Philip Loeffel, Sheena Garny, Hella Chen, Xiaoyang Pinto, Joaquim G. Birner, Thomas Loeffel, Sheena; 2 Deutsches Zentrum für Luft‐ und Raumfahrt (DLR) Institut für Physik der Atmosphäre Oberpfaffenhofen Germany Garny, Hella; 2 Deutsches Zentrum für Luft‐ und Raumfahrt (DLR) Institut für Physik der Atmosphäre Oberpfaffenhofen Germany Chen, Xiaoyang; 3 Institute of Meteorology and Climate Research Karlsruhe Institute of Technology Karlsruhe Germany Pinto, Joaquim G.; 3 Institute of Meteorology and Climate Research Karlsruhe Institute of Technology Karlsruhe Germany Birner, Thomas; 1 Meteorological Institute Munich Ludwig‐Maximilians‐University Munich Germany Potential Links Between Tropospheric and Stratospheric Circulation Extremes During Early 2020 |
topic_facet |
ddc:551.5 strat‐trop coupling wave reflection event Arctic oscillation index stratospheric polar vortex circulation extremes ensemble simulations |
description |
February‐March 2020 was marked by highly anomalous large‐scale circulations in the Northern extratropical troposphere and stratosphere. The Atlantic jet reached extreme strength, linked to some of the strongest and most persistent positive values of the Arctic Oscillation index on record, which provided conditions for extreme windstorms hitting Europe. Likewise, the stratospheric polar vortex reached extreme strength that persisted for an unusually long period. Past research indicated that such circulation extremes occurring throughout the troposphere‐stratosphere system are dynamically coupled, although the nature of this coupling is still not fully understood and generally difficult to quantify. We employ sets of numerical ensemble simulations to statistically characterize the mutual coupling of the early 2020 extremes. We find the extreme vortex strength to be linked to the reflection of upward propagating planetary waves and the occurrence of this reflection to be sensitive to the details of the vortex structure. Our results show an overall robust coupling between tropospheric and stratospheric anomalies: ensemble members with polar vortex exceeding a certain strength tend to exhibit a stronger tropospheric jet and vice versa. Moreover, members exhibiting a breakdown of the stratospheric circulation (e.g., sudden stratospheric warming) tend to lack periods of persistently enhanced tropospheric circulation. Despite indications for vertical coupling, our simulations underline the role of internal variability within each atmospheric layer. The circulation extremes during early 2020 may be viewed as resulting from a fortuitous alignment of dynamical evolutions within the troposphere and stratosphere, aided by each layer's modification of the other layer's boundary condition. Key Points Large‐ensemble simulations are needed to fully characterize coupled extremes in the polar vortex and tropospheric jet in early 2020. Details of the vortex structure play an important role in promoting either reflection or ... |
format |
Article in Journal/Newspaper |
author |
Rupp, Philip Loeffel, Sheena Garny, Hella Chen, Xiaoyang Pinto, Joaquim G. Birner, Thomas Loeffel, Sheena; 2 Deutsches Zentrum für Luft‐ und Raumfahrt (DLR) Institut für Physik der Atmosphäre Oberpfaffenhofen Germany Garny, Hella; 2 Deutsches Zentrum für Luft‐ und Raumfahrt (DLR) Institut für Physik der Atmosphäre Oberpfaffenhofen Germany Chen, Xiaoyang; 3 Institute of Meteorology and Climate Research Karlsruhe Institute of Technology Karlsruhe Germany Pinto, Joaquim G.; 3 Institute of Meteorology and Climate Research Karlsruhe Institute of Technology Karlsruhe Germany Birner, Thomas; 1 Meteorological Institute Munich Ludwig‐Maximilians‐University Munich Germany |
author_facet |
Rupp, Philip Loeffel, Sheena Garny, Hella Chen, Xiaoyang Pinto, Joaquim G. Birner, Thomas Loeffel, Sheena; 2 Deutsches Zentrum für Luft‐ und Raumfahrt (DLR) Institut für Physik der Atmosphäre Oberpfaffenhofen Germany Garny, Hella; 2 Deutsches Zentrum für Luft‐ und Raumfahrt (DLR) Institut für Physik der Atmosphäre Oberpfaffenhofen Germany Chen, Xiaoyang; 3 Institute of Meteorology and Climate Research Karlsruhe Institute of Technology Karlsruhe Germany Pinto, Joaquim G.; 3 Institute of Meteorology and Climate Research Karlsruhe Institute of Technology Karlsruhe Germany Birner, Thomas; 1 Meteorological Institute Munich Ludwig‐Maximilians‐University Munich Germany |
author_sort |
Rupp, Philip |
title |
Potential Links Between Tropospheric and Stratospheric Circulation Extremes During Early 2020 |
title_short |
Potential Links Between Tropospheric and Stratospheric Circulation Extremes During Early 2020 |
title_full |
Potential Links Between Tropospheric and Stratospheric Circulation Extremes During Early 2020 |
title_fullStr |
Potential Links Between Tropospheric and Stratospheric Circulation Extremes During Early 2020 |
title_full_unstemmed |
Potential Links Between Tropospheric and Stratospheric Circulation Extremes During Early 2020 |
title_sort |
potential links between tropospheric and stratospheric circulation extremes during early 2020 |
publishDate |
2022 |
url |
https://doi.org/10.1029/2021JD035667 http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/9979 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic |
genre_facet |
Arctic |
op_relation |
doi:10.1029/2021JD035667 http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/9979 |
op_rights |
This is an open access article under the terms of the Creative Commons Attribution‐NonCommercial‐NoDerivs License, which permits use and distribution in any medium, provided the original work is properly cited, the use is non‐commercial and no modifications or adaptations are made. |
op_rightsnorm |
CC-BY-NC-ND |
op_doi |
https://doi.org/10.1029/2021JD035667 |
container_title |
Journal of Geophysical Research: Atmospheres |
container_volume |
127 |
container_issue |
3 |
_version_ |
1766333938189467648 |