The relevance of the location of blocking highs for stratospheric variability in a changing climate

Previous research shows that blocking highs (BHs) influence wintertime polar stratospheric variability through the modulation of the climatological planetary waves (PWs) depending on the BH location. BHs over the Euro-Atlantic sector tend to enhance the upward PW propagation, and those over the nort...

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Main Authors: Ayarzagüena Porras, Blanca, Orsolini, Yvan J., Langematz, Ulrike, Abalichin, Janna, Kubin, Anne
Format: Article in Journal/Newspaper
Language:English
Published: American Meteorological Society 2015
Subjects:
Online Access:https://hdl.handle.net/20.500.14352/91800
https://doi.org/10.1175/jcli-d-14-00210.1
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author Ayarzagüena Porras, Blanca
Orsolini, Yvan J.
Langematz, Ulrike
Abalichin, Janna
Kubin, Anne
author_facet Ayarzagüena Porras, Blanca
Orsolini, Yvan J.
Langematz, Ulrike
Abalichin, Janna
Kubin, Anne
author_sort Ayarzagüena Porras, Blanca
collection Docta Complutense (Universidad Complutense de Madrid - UCM)
description Previous research shows that blocking highs (BHs) influence wintertime polar stratospheric variability through the modulation of the climatological planetary waves (PWs) depending on the BH location. BHs over the Euro-Atlantic sector tend to enhance the upward PW propagation, and those over the northwestern Pacific Ocean tend to reduce it. Future changes are examined in the response of the wave activity flux to the BH location and their relationship with wintertime stratospheric variability in transient simulations of ECHAM/Modular Earth Submodel System (MESSy) Atmospheric Chemistry (EMAC). After it is verified that EMAC can reproduce qualitatively well the geographical dependence of the BH influence on PW activity injection, it is shown that this dependence does not change in the future. However, an eastward shift of the pattern of the BH influence on PW propagation over the Pacific, a farther eastward extension of the pattern over the Atlantic Ocean, and an intensification of the wavenumber-1 component of the interaction between climatological and anomalous waves are detected. Changes in the upper-tropospheric jet and an intensification of the wavenumber-1 climatological wave due to a strengthening of the Aleutian low agree with these variations. The spatial distribution of future BHs preceding extreme polar vortex events is also affected by the slight modifications in the wave activity pattern. Hence, future BHs preceding strong vortex events tend to be more concentrated over the Pacific than in the past, where BHs interfere negatively with wavenumber-1 climatological waves. Future BHs prior to major stratospheric warmings are located in a broader area than in the past, predominantly over an extended Euro-Atlantic sector. Deutscher Akademischer Austauschdienst Deutsche Forschungsgemeinschaft Research Council of Norway Depto. de Física de la Tierra y Astrofísica Fac. de Ciencias Físicas TRUE pub
format Article in Journal/Newspaper
genre aleutian low
genre_facet aleutian low
geographic Norway
Pacific
geographic_facet Norway
Pacific
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institution Open Polar
language English
op_collection_id ftunivcmadrid
op_doi https://doi.org/20.500.14352/9180010.1175/jcli-d-14-00210.110.1175/JCLI-D-14-00210.1
op_relation info:eu-repo/grantAgreement/DFG/SHARP/LA 1025/13-1
info:eu-repo/grantAgreement/DFG/ISOLAA /LA 1025/17-1
info:eu-repo/grantAgreement/DFG/PROSECCO/LA 1025/5-3
Ayarzagüena, B., Y. J. Orsolini, U. Langematz, J. Abalichin, and A. Kubin, 2015: The Relevance of the Location of Blocking Highs for Stratospheric Variability in a Changing Climate. J. Climate, 28, 531–549, https://doi.org/10.1175/JCLI-D-14-00210.1.
https://hdl.handle.net/20.500.14352/91800
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publisher American Meteorological Society
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spelling ftunivcmadrid:oai:docta.ucm.es:20.500.14352/91800 2025-05-04T14:06:59+00:00 The relevance of the location of blocking highs for stratospheric variability in a changing climate Ayarzagüena Porras, Blanca Orsolini, Yvan J. Langematz, Ulrike Abalichin, Janna Kubin, Anne 2015 application/pdf https://hdl.handle.net/20.500.14352/91800 https://doi.org/10.1175/jcli-d-14-00210.1 eng eng American Meteorological Society info:eu-repo/grantAgreement/DFG/SHARP/LA 1025/13-1 info:eu-repo/grantAgreement/DFG/ISOLAA /LA 1025/17-1 info:eu-repo/grantAgreement/DFG/PROSECCO/LA 1025/5-3 Ayarzagüena, B., Y. J. Orsolini, U. Langematz, J. Abalichin, and A. Kubin, 2015: The Relevance of the Location of Blocking Highs for Stratospheric Variability in a Changing Climate. J. Climate, 28, 531–549, https://doi.org/10.1175/JCLI-D-14-00210.1. https://hdl.handle.net/20.500.14352/91800 restricted access 551.51 Blocking Planetary waves Stratospheric circulation Stratosphere-troposphere coupling Climate change Climate models Física atmosférica 2501.06 Dinámica Atmosférica 2501.21 Simulación Numérica journal article VoR 2015 ftunivcmadrid https://doi.org/20.500.14352/9180010.1175/jcli-d-14-00210.110.1175/JCLI-D-14-00210.1 2025-04-09T14:16:29Z Previous research shows that blocking highs (BHs) influence wintertime polar stratospheric variability through the modulation of the climatological planetary waves (PWs) depending on the BH location. BHs over the Euro-Atlantic sector tend to enhance the upward PW propagation, and those over the northwestern Pacific Ocean tend to reduce it. Future changes are examined in the response of the wave activity flux to the BH location and their relationship with wintertime stratospheric variability in transient simulations of ECHAM/Modular Earth Submodel System (MESSy) Atmospheric Chemistry (EMAC). After it is verified that EMAC can reproduce qualitatively well the geographical dependence of the BH influence on PW activity injection, it is shown that this dependence does not change in the future. However, an eastward shift of the pattern of the BH influence on PW propagation over the Pacific, a farther eastward extension of the pattern over the Atlantic Ocean, and an intensification of the wavenumber-1 component of the interaction between climatological and anomalous waves are detected. Changes in the upper-tropospheric jet and an intensification of the wavenumber-1 climatological wave due to a strengthening of the Aleutian low agree with these variations. The spatial distribution of future BHs preceding extreme polar vortex events is also affected by the slight modifications in the wave activity pattern. Hence, future BHs preceding strong vortex events tend to be more concentrated over the Pacific than in the past, where BHs interfere negatively with wavenumber-1 climatological waves. Future BHs prior to major stratospheric warmings are located in a broader area than in the past, predominantly over an extended Euro-Atlantic sector. Deutscher Akademischer Austauschdienst Deutsche Forschungsgemeinschaft Research Council of Norway Depto. de Física de la Tierra y Astrofísica Fac. de Ciencias Físicas TRUE pub Article in Journal/Newspaper aleutian low Docta Complutense (Universidad Complutense de Madrid - UCM) Norway Pacific
spellingShingle 551.51
Blocking
Planetary waves
Stratospheric circulation
Stratosphere-troposphere coupling
Climate change
Climate models
Física atmosférica
2501.06 Dinámica Atmosférica
2501.21 Simulación Numérica
Ayarzagüena Porras, Blanca
Orsolini, Yvan J.
Langematz, Ulrike
Abalichin, Janna
Kubin, Anne
The relevance of the location of blocking highs for stratospheric variability in a changing climate
title The relevance of the location of blocking highs for stratospheric variability in a changing climate
title_full The relevance of the location of blocking highs for stratospheric variability in a changing climate
title_fullStr The relevance of the location of blocking highs for stratospheric variability in a changing climate
title_full_unstemmed The relevance of the location of blocking highs for stratospheric variability in a changing climate
title_short The relevance of the location of blocking highs for stratospheric variability in a changing climate
title_sort relevance of the location of blocking highs for stratospheric variability in a changing climate
topic 551.51
Blocking
Planetary waves
Stratospheric circulation
Stratosphere-troposphere coupling
Climate change
Climate models
Física atmosférica
2501.06 Dinámica Atmosférica
2501.21 Simulación Numérica
topic_facet 551.51
Blocking
Planetary waves
Stratospheric circulation
Stratosphere-troposphere coupling
Climate change
Climate models
Física atmosférica
2501.06 Dinámica Atmosférica
2501.21 Simulación Numérica
url https://hdl.handle.net/20.500.14352/91800
https://doi.org/10.1175/jcli-d-14-00210.1