Sea-salt injections into the low-latitude marine boundary layer: The transient response in three earth system models

Among proposed mechanisms for counteracting global warming through solar radiation management is the deliberate injection of sea salt acting via marine cloud brightening and the direct effect of sea-salt aerosols. In this study, we show results from multidecadal simulations of such sea-salt climate...

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Published in:Journal of Geophysical Research: Atmospheres
Main Authors: Alterskjær, K., Kristjánsson, J., Boucher, O., Muri, H., Niemeier, U., Schmidt, H., Schulz, M., Timmreck, C.
Format: Article in Journal/Newspaper
Language:English
Published: 2013
Subjects:
Online Access:http://hdl.handle.net/11858/00-001M-0000-0014-CF1B-6
http://hdl.handle.net/11858/00-001M-0000-0014-CF1D-2
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spelling ftpubman:oai:pure.mpg.de:item_1878108 2023-08-27T04:07:38+02:00 Sea-salt injections into the low-latitude marine boundary layer: The transient response in three earth system models Alterskjær, K. Kristjánsson, J. Boucher, O. Muri, H. Niemeier, U. Schmidt, H. Schulz, M. Timmreck, C. 2013-11-16 application/pdf http://hdl.handle.net/11858/00-001M-0000-0014-CF1B-6 http://hdl.handle.net/11858/00-001M-0000-0014-CF1D-2 eng eng info:eu-repo/semantics/altIdentifier/doi/10.1002/2013JD020432 http://hdl.handle.net/11858/00-001M-0000-0014-CF1B-6 http://hdl.handle.net/11858/00-001M-0000-0014-CF1D-2 info:eu-repo/semantics/openAccess Journal of Geophysical Research-Atmospheres info:eu-repo/semantics/article 2013 ftpubman https://doi.org/10.1002/2013JD020432 2023-08-02T01:33:57Z Among proposed mechanisms for counteracting global warming through solar radiation management is the deliberate injection of sea salt acting via marine cloud brightening and the direct effect of sea-salt aerosols. In this study, we show results from multidecadal simulations of such sea-salt climate engineering (SSCE) on top of the RCP4.5 emission scenario using three Earth system models. As in the proposed "G3" experiment of the Geoengineering Model Intercomparison Project, SSCE is designed to keep the top-of-atmosphere radiative forcing at the 2020 level for 50 years. SSCE is then turned off and the models run for another 20 years, enabling an investigation of the abrupt warming associated with a termination of climate engineering ("termination effect"). As in former idealized studies, the climate engineering in all three models leads to a significant suppression of evaporation from low-latitude oceans and reduced precipitation over low-latitude oceans as well as in the storm-track regions. Unlike those studies, however, we find in all models enhanced evaporation, cloud formation, and precipitation over low-latitude land regions. This is a response to the localized cooling over the low-latitude oceans imposed by the SSCE design. As a result, the models obtain reduced aridity in many low-latitude land regions as well as in southern Europe. Terminating the SSCE leads to a rapid near-surface temperature increase, which, in the Arctic, exceeds 2 K in all three models within 20 years after SSCE has ceased. In the same period September Arctic sea ice cover shrinks by over 25%. Key Points This is the first multi-ESM study of sea salt climate engineering Over the low-latitude continents all models find a reduction in aridity Terminating climate engineering leads to Arctic warming exceeding 1 K / decade ©2013 The Authors. Journal of Geophysical Research: Atmospheres published by Wiley on behalf of the American Geophysical Union. Article in Journal/Newspaper Arctic Global warming Sea ice Max Planck Society: MPG.PuRe Arctic Journal of Geophysical Research: Atmospheres 118 21
institution Open Polar
collection Max Planck Society: MPG.PuRe
op_collection_id ftpubman
language English
description Among proposed mechanisms for counteracting global warming through solar radiation management is the deliberate injection of sea salt acting via marine cloud brightening and the direct effect of sea-salt aerosols. In this study, we show results from multidecadal simulations of such sea-salt climate engineering (SSCE) on top of the RCP4.5 emission scenario using three Earth system models. As in the proposed "G3" experiment of the Geoengineering Model Intercomparison Project, SSCE is designed to keep the top-of-atmosphere radiative forcing at the 2020 level for 50 years. SSCE is then turned off and the models run for another 20 years, enabling an investigation of the abrupt warming associated with a termination of climate engineering ("termination effect"). As in former idealized studies, the climate engineering in all three models leads to a significant suppression of evaporation from low-latitude oceans and reduced precipitation over low-latitude oceans as well as in the storm-track regions. Unlike those studies, however, we find in all models enhanced evaporation, cloud formation, and precipitation over low-latitude land regions. This is a response to the localized cooling over the low-latitude oceans imposed by the SSCE design. As a result, the models obtain reduced aridity in many low-latitude land regions as well as in southern Europe. Terminating the SSCE leads to a rapid near-surface temperature increase, which, in the Arctic, exceeds 2 K in all three models within 20 years after SSCE has ceased. In the same period September Arctic sea ice cover shrinks by over 25%. Key Points This is the first multi-ESM study of sea salt climate engineering Over the low-latitude continents all models find a reduction in aridity Terminating climate engineering leads to Arctic warming exceeding 1 K / decade ©2013 The Authors. Journal of Geophysical Research: Atmospheres published by Wiley on behalf of the American Geophysical Union.
format Article in Journal/Newspaper
author Alterskjær, K.
Kristjánsson, J.
Boucher, O.
Muri, H.
Niemeier, U.
Schmidt, H.
Schulz, M.
Timmreck, C.
spellingShingle Alterskjær, K.
Kristjánsson, J.
Boucher, O.
Muri, H.
Niemeier, U.
Schmidt, H.
Schulz, M.
Timmreck, C.
Sea-salt injections into the low-latitude marine boundary layer: The transient response in three earth system models
author_facet Alterskjær, K.
Kristjánsson, J.
Boucher, O.
Muri, H.
Niemeier, U.
Schmidt, H.
Schulz, M.
Timmreck, C.
author_sort Alterskjær, K.
title Sea-salt injections into the low-latitude marine boundary layer: The transient response in three earth system models
title_short Sea-salt injections into the low-latitude marine boundary layer: The transient response in three earth system models
title_full Sea-salt injections into the low-latitude marine boundary layer: The transient response in three earth system models
title_fullStr Sea-salt injections into the low-latitude marine boundary layer: The transient response in three earth system models
title_full_unstemmed Sea-salt injections into the low-latitude marine boundary layer: The transient response in three earth system models
title_sort sea-salt injections into the low-latitude marine boundary layer: the transient response in three earth system models
publishDate 2013
url http://hdl.handle.net/11858/00-001M-0000-0014-CF1B-6
http://hdl.handle.net/11858/00-001M-0000-0014-CF1D-2
geographic Arctic
geographic_facet Arctic
genre Arctic
Global warming
Sea ice
genre_facet Arctic
Global warming
Sea ice
op_source Journal of Geophysical Research-Atmospheres
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1002/2013JD020432
http://hdl.handle.net/11858/00-001M-0000-0014-CF1B-6
http://hdl.handle.net/11858/00-001M-0000-0014-CF1D-2
op_rights info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1002/2013JD020432
container_title Journal of Geophysical Research: Atmospheres
container_volume 118
container_issue 21
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