Stratospheric water vapor affecting atmospheric circulation

Water vapor plays an important role in many aspects of the climate system, by affecting radiation, cloud formation, atmospheric chemistry and dynamics. Even the low stratospheric water vapor content provides an important climate feedback, but current climate models show a substantial moist bias in t...

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Autores: Charlesworth, Edward, Plöger, Felix, Birner, Thomas, Baikhadzhaev, Rasul, Ábalos Álvarez, Marta, Abraham, Nathan Luke, Akiyoshi, Hideharu, Slimane Bekki, Slimane, Dennison, Fraser, Jöckel, Patrick, Keeble, James, Kinnison, Doug, Morgenstern, Olaf, Plummer, David, Rozanov, Eugene, Strode, Sarah, Zeng, Guang, Egorova, Tatiana, Riese, Martin
Tipo de recurso: artículo
Fecha de publicación:2023
País:España
Institución:Universidad Complutense de Madrid (UCM)
Repositorio:Docta Complutense
Idioma:inglés
OAI Identifier:oai:docta.ucm.es:20.500.14352/108149
Acceso en línea:https://hdl.handle.net/20.500.14352/108149
Access Level:acceso abierto
Palabra clave:550.3
Geofísica
2507 Geofísica
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spelling Stratospheric water vapor affecting atmospheric circulationCharlesworth, EdwardPlöger, FelixBirner, ThomasBaikhadzhaev, RasulÁbalos Álvarez, MartaAbraham, Nathan LukeAkiyoshi, HideharuSlimane Bekki, SlimaneDennison, FraserJöckel, PatrickKeeble, JamesKinnison, DougMorgenstern, OlafPlummer, DavidRozanov, EugeneStrode, SarahZeng, GuangEgorova, TatianaRiese, Martin550.3Geofísica2507 GeofísicaWater vapor plays an important role in many aspects of the climate system, by affecting radiation, cloud formation, atmospheric chemistry and dynamics. Even the low stratospheric water vapor content provides an important climate feedback, but current climate models show a substantial moist bias in the lowermost stratosphere. Here we report crucial sensitivity of the atmospheric circulation in the stratosphere and troposphere to the abundance of water vapor in the lowermost stratosphere. We show from a mechanistic climate model experiment and inter-model variability that lowermost stratospheric water vapor decreases local temperatures, and thereby causes an upward and poleward shift of subtropical jets, a strengthening of the stratospheric circulation, a poleward shift of the tropospheric eddy-driven jet and regional climate impacts. The mechanistic model experiment in combination with atmospheric observations further shows that the prevailing moist bias in current models is likely caused by the transport scheme, and can be alleviated by employing a less diffusive Lagrangian scheme. The related effects on atmospheric circulation are of similar magnitude as climate change effects. Hence, lowermost stratospheric water vapor exerts a first order effect on atmospheric circulation and improving its representation in models offers promising prospects for future research.Nature ResearchUniversidad Complutense de Madrid20232023-07-0320232023-07-03journal articlehttp://purl.org/coar/resource_type/c_6501VoRhttp://purl.org/coar/version/c_970fb48d4fbd8a85info:eu-repo/semantics/articleapplication/pdfhttps://hdl.handle.net/20.500.14352/108149reponame:Docta Complutenseinstname:Universidad Complutense de Madrid (UCM)Inglésengopen accesshttp://purl.org/coar/access_right/c_abf2Attribution 4.0 Internationalhttp://creativecommons.org/licenses/by/4.0/info:eu-repo/semantics/openAccessoai:docta.ucm.es:20.500.14352/1081492026-06-02T12:44:21Z
dc.title.none.fl_str_mv Stratospheric water vapor affecting atmospheric circulation
title Stratospheric water vapor affecting atmospheric circulation
spellingShingle Stratospheric water vapor affecting atmospheric circulation
Charlesworth, Edward
550.3
Geofísica
2507 Geofísica
title_short Stratospheric water vapor affecting atmospheric circulation
title_full Stratospheric water vapor affecting atmospheric circulation
title_fullStr Stratospheric water vapor affecting atmospheric circulation
title_full_unstemmed Stratospheric water vapor affecting atmospheric circulation
title_sort Stratospheric water vapor affecting atmospheric circulation
dc.creator.none.fl_str_mv Charlesworth, Edward
Plöger, Felix
Birner, Thomas
Baikhadzhaev, Rasul
Ábalos Álvarez, Marta
Abraham, Nathan Luke
Akiyoshi, Hideharu
Slimane Bekki, Slimane
Dennison, Fraser
Jöckel, Patrick
Keeble, James
Kinnison, Doug
Morgenstern, Olaf
Plummer, David
Rozanov, Eugene
Strode, Sarah
Zeng, Guang
Egorova, Tatiana
Riese, Martin
author Charlesworth, Edward
author_facet Charlesworth, Edward
Plöger, Felix
Birner, Thomas
Baikhadzhaev, Rasul
Ábalos Álvarez, Marta
Abraham, Nathan Luke
Akiyoshi, Hideharu
Slimane Bekki, Slimane
Dennison, Fraser
Jöckel, Patrick
Keeble, James
Kinnison, Doug
Morgenstern, Olaf
Plummer, David
Rozanov, Eugene
Strode, Sarah
Zeng, Guang
Egorova, Tatiana
Riese, Martin
author_role author
author2 Plöger, Felix
Birner, Thomas
Baikhadzhaev, Rasul
Ábalos Álvarez, Marta
Abraham, Nathan Luke
Akiyoshi, Hideharu
Slimane Bekki, Slimane
Dennison, Fraser
Jöckel, Patrick
Keeble, James
Kinnison, Doug
Morgenstern, Olaf
Plummer, David
Rozanov, Eugene
Strode, Sarah
Zeng, Guang
Egorova, Tatiana
Riese, Martin
author2_role author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
author
dc.contributor.none.fl_str_mv Universidad Complutense de Madrid
dc.subject.none.fl_str_mv 550.3
Geofísica
2507 Geofísica
topic 550.3
Geofísica
2507 Geofísica
description Water vapor plays an important role in many aspects of the climate system, by affecting radiation, cloud formation, atmospheric chemistry and dynamics. Even the low stratospheric water vapor content provides an important climate feedback, but current climate models show a substantial moist bias in the lowermost stratosphere. Here we report crucial sensitivity of the atmospheric circulation in the stratosphere and troposphere to the abundance of water vapor in the lowermost stratosphere. We show from a mechanistic climate model experiment and inter-model variability that lowermost stratospheric water vapor decreases local temperatures, and thereby causes an upward and poleward shift of subtropical jets, a strengthening of the stratospheric circulation, a poleward shift of the tropospheric eddy-driven jet and regional climate impacts. The mechanistic model experiment in combination with atmospheric observations further shows that the prevailing moist bias in current models is likely caused by the transport scheme, and can be alleviated by employing a less diffusive Lagrangian scheme. The related effects on atmospheric circulation are of similar magnitude as climate change effects. Hence, lowermost stratospheric water vapor exerts a first order effect on atmospheric circulation and improving its representation in models offers promising prospects for future research.
publishDate 2023
dc.date.none.fl_str_mv 2023
2023-07-03
2023
2023-07-03
dc.type.none.fl_str_mv journal article
http://purl.org/coar/resource_type/c_6501
VoR
http://purl.org/coar/version/c_970fb48d4fbd8a85
dc.type.openaire.fl_str_mv info:eu-repo/semantics/article
format article
dc.identifier.none.fl_str_mv https://hdl.handle.net/20.500.14352/108149
url https://hdl.handle.net/20.500.14352/108149
dc.language.none.fl_str_mv Inglés
eng
language_invalid_str_mv Inglés
language eng
dc.rights.none.fl_str_mv open access
http://purl.org/coar/access_right/c_abf2
Attribution 4.0 International
http://creativecommons.org/licenses/by/4.0/
dc.rights.openaire.fl_str_mv info:eu-repo/semantics/openAccess
rights_invalid_str_mv open access
http://purl.org/coar/access_right/c_abf2
Attribution 4.0 International
http://creativecommons.org/licenses/by/4.0/
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv Nature Research
publisher.none.fl_str_mv Nature Research
dc.source.none.fl_str_mv reponame:Docta Complutense
instname:Universidad Complutense de Madrid (UCM)
instname_str Universidad Complutense de Madrid (UCM)
reponame_str Docta Complutense
collection Docta Complutense
repository.name.fl_str_mv
repository.mail.fl_str_mv
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