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...
| Autores: | , , , , , , , , , , , , , , , , , , |
|---|---|
| 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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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) |
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Universidad Complutense de Madrid (UCM) |
| reponame_str |
Docta Complutense |
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Docta Complutense |
| repository.name.fl_str_mv |
|
| repository.mail.fl_str_mv |
|
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1869404208517611520 |
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15.811543 |