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...
Main Authors: | , , , , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
American Meteorological Society
2015
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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 |
id | ftunivcmadrid:oai:docta.ucm.es:20.500.14352/91800 |
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 |
op_rights | restricted access |
publishDate | 2015 |
publisher | American Meteorological Society |
record_format | openpolar |
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 |