Robust winter warming over Eurasia under stratospheric sulfate geoengineering – the role of stratospheric dynamics

It has been suggested that increased stratospheric sulfate aerosol loadings following large, low latitude volcanic eruptions can lead to wintertime warming over Eurasia through dynamical stratosphere-troposphere coupling. We here investigate the proposed connection in the context of hypothetical fut...

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Published in:Atmospheric Chemistry and Physics
Other Authors: Banerjee, Antara (author), Butler, Amy H. (author), Polvani, Lorenzo M. (author), Robock, Alan (author), Simpson, Isla R. (author), Sun, Lantao (author)
Format: Article in Journal/Newspaper
Language:English
Published: 2021
Subjects:
Online Access:https://doi.org/10.5194/acp-21-6985-2021
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spelling ftncar:oai:drupal-site.org:articles_24324 2024-04-14T08:15:33+00:00 Robust winter warming over Eurasia under stratospheric sulfate geoengineering – the role of stratospheric dynamics Banerjee, Antara (author) Butler, Amy H. (author) Polvani, Lorenzo M. (author) Robock, Alan (author) Simpson, Isla R. (author) Sun, Lantao (author) 2021-05-07 https://doi.org/10.5194/acp-21-6985-2021 en eng Atmospheric Chemistry and Physics--Atmos. Chem. Phys.--1680-7324 Stratospheric Aerosol Geoengineering Large Ensemble--10.5065/D6JH3JXX antara-banerjee/GeoengineeringLE_WinterWarming: Publication Code--10.5281/zenodo.4713591 articles:24324 ark:/85065/d7057kb1 doi:10.5194/acp-21-6985-2021 Copyright author(s). This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License. article Text 2021 ftncar https://doi.org/10.5194/acp-21-6985-2021 2024-03-21T18:00:26Z It has been suggested that increased stratospheric sulfate aerosol loadings following large, low latitude volcanic eruptions can lead to wintertime warming over Eurasia through dynamical stratosphere-troposphere coupling. We here investigate the proposed connection in the context of hypothetical future stratospheric sulfate geoengineering in the Geoengineering Large Ensemble simulations. In those geoengineering simulations, we find that stratospheric circulation anomalies that resemble the positive phase of the Northern Annular Mode in winter are a distinguishing climate response which is absent when increasing greenhouse gases alone are prescribed. This stratospheric dynamical response projects onto the positive phase of the North Atlantic Oscillation, leading to associated side effects of this climate intervention strategy, such as continental Eurasian warming and precipitation changes. Seasonality is a key signature of the dynamically driven surface response. We find an opposite response of the North Atlantic Oscillation in summer, when no dynamical role of the stratosphere is expected. The robustness of the wintertime forced response stands in contrast to previously proposed volcanic responses. 1852977 Article in Journal/Newspaper North Atlantic North Atlantic oscillation OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research) Atmospheric Chemistry and Physics 21 9 6985 6997
institution Open Polar
collection OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research)
op_collection_id ftncar
language English
description It has been suggested that increased stratospheric sulfate aerosol loadings following large, low latitude volcanic eruptions can lead to wintertime warming over Eurasia through dynamical stratosphere-troposphere coupling. We here investigate the proposed connection in the context of hypothetical future stratospheric sulfate geoengineering in the Geoengineering Large Ensemble simulations. In those geoengineering simulations, we find that stratospheric circulation anomalies that resemble the positive phase of the Northern Annular Mode in winter are a distinguishing climate response which is absent when increasing greenhouse gases alone are prescribed. This stratospheric dynamical response projects onto the positive phase of the North Atlantic Oscillation, leading to associated side effects of this climate intervention strategy, such as continental Eurasian warming and precipitation changes. Seasonality is a key signature of the dynamically driven surface response. We find an opposite response of the North Atlantic Oscillation in summer, when no dynamical role of the stratosphere is expected. The robustness of the wintertime forced response stands in contrast to previously proposed volcanic responses. 1852977
author2 Banerjee, Antara (author)
Butler, Amy H. (author)
Polvani, Lorenzo M. (author)
Robock, Alan (author)
Simpson, Isla R. (author)
Sun, Lantao (author)
format Article in Journal/Newspaper
title Robust winter warming over Eurasia under stratospheric sulfate geoengineering – the role of stratospheric dynamics
spellingShingle Robust winter warming over Eurasia under stratospheric sulfate geoengineering – the role of stratospheric dynamics
title_short Robust winter warming over Eurasia under stratospheric sulfate geoengineering – the role of stratospheric dynamics
title_full Robust winter warming over Eurasia under stratospheric sulfate geoengineering – the role of stratospheric dynamics
title_fullStr Robust winter warming over Eurasia under stratospheric sulfate geoengineering – the role of stratospheric dynamics
title_full_unstemmed Robust winter warming over Eurasia under stratospheric sulfate geoengineering – the role of stratospheric dynamics
title_sort robust winter warming over eurasia under stratospheric sulfate geoengineering – the role of stratospheric dynamics
publishDate 2021
url https://doi.org/10.5194/acp-21-6985-2021
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_relation Atmospheric Chemistry and Physics--Atmos. Chem. Phys.--1680-7324
Stratospheric Aerosol Geoengineering Large Ensemble--10.5065/D6JH3JXX
antara-banerjee/GeoengineeringLE_WinterWarming: Publication Code--10.5281/zenodo.4713591
articles:24324
ark:/85065/d7057kb1
doi:10.5194/acp-21-6985-2021
op_rights Copyright author(s). This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License.
op_doi https://doi.org/10.5194/acp-21-6985-2021
container_title Atmospheric Chemistry and Physics
container_volume 21
container_issue 9
container_start_page 6985
op_container_end_page 6997
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