Greenland Ice Sheet Response to Stratospheric Aerosol Injection Geoengineering
Abstract The Greenland ice sheet is expected lose at least 90% of its current volume if ice sheet summer temperatures warm by around 1.8 °C above pre‐industrial. Geoengineering by stratospheric sulfate aerosol injection might slow Greenland ice sheet melting and sea level rise by reducing summer tem...
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Online Access: | https://doi.org/10.1029/2019EF001393 https://doaj.org/article/9cfce3433f7e44c1b7ba0c8359e2e48a |
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fttriple:oai:gotriple.eu:oai:doaj.org/article:9cfce3433f7e44c1b7ba0c8359e2e48a 2023-05-15T15:09:21+02:00 Greenland Ice Sheet Response to Stratospheric Aerosol Injection Geoengineering John C. Moore Chao Yue Liyun Zhao Xiaoran Guo Shingo Watanabe Duoying Ji 2019-12-01 https://doi.org/10.1029/2019EF001393 https://doaj.org/article/9cfce3433f7e44c1b7ba0c8359e2e48a en eng Wiley 2328-4277 doi:10.1029/2019EF001393 https://doaj.org/article/9cfce3433f7e44c1b7ba0c8359e2e48a undefined Earth's Future, Vol 7, Iss 12, Pp 1451-1463 (2019) sea level rise mass balance glacier dynamics geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2019 fttriple https://doi.org/10.1029/2019EF001393 2023-01-22T19:32:38Z Abstract The Greenland ice sheet is expected lose at least 90% of its current volume if ice sheet summer temperatures warm by around 1.8 °C above pre‐industrial. Geoengineering by stratospheric sulfate aerosol injection might slow Greenland ice sheet melting and sea level rise by reducing summer temperature and insolation; however, such schemes could also reduce precipitation and affect large‐scale climate drivers such as the Atlantic Meridional Over‐turning Circulation (AMOC). Earlier work found that AMOC increased under geoengineering and that might lead to greater mass loss from Greenland than under greenhouse gas forcing alone. We simulated Greenland ice sheet climates using four Earth system models running the stratospheric sulfate aerosol injection experiment GeoMIP G4 and the CMIP RCP4.5 and RCP8.5 greenhouse gas scenarios that were then used to drive the surface energy and mass balance model, SEMIC. Simulated runoff is 20% lower under G4 than RCP4.5, while under RCP8.5 it is 17% higher. The mechanism is through increased Arctic sea ice concentration and reduced humidity leading to surface cooling of the ablation zone. Reduced absorption of outgoing longwave radiation caused by hydrological cycle weakening dominates associated decreases in precipitation under geoengineering and stronger AMOC than under RCP4.5. An ice dynamics model simulates 15% lower ice losses under G4 than RCP4.5. Thus, total sea level rise by 2070 from the Greenland ice sheet under G4 geoengineering is about 15–20% lower than under the RCP4.5 scenario. Article in Journal/Newspaper Arctic glacier Greenland Ice Sheet Sea ice Unknown Arctic Greenland Earth's Future 7 12 1451 1463 |
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language |
English |
topic |
sea level rise mass balance glacier dynamics geo envir |
spellingShingle |
sea level rise mass balance glacier dynamics geo envir John C. Moore Chao Yue Liyun Zhao Xiaoran Guo Shingo Watanabe Duoying Ji Greenland Ice Sheet Response to Stratospheric Aerosol Injection Geoengineering |
topic_facet |
sea level rise mass balance glacier dynamics geo envir |
description |
Abstract The Greenland ice sheet is expected lose at least 90% of its current volume if ice sheet summer temperatures warm by around 1.8 °C above pre‐industrial. Geoengineering by stratospheric sulfate aerosol injection might slow Greenland ice sheet melting and sea level rise by reducing summer temperature and insolation; however, such schemes could also reduce precipitation and affect large‐scale climate drivers such as the Atlantic Meridional Over‐turning Circulation (AMOC). Earlier work found that AMOC increased under geoengineering and that might lead to greater mass loss from Greenland than under greenhouse gas forcing alone. We simulated Greenland ice sheet climates using four Earth system models running the stratospheric sulfate aerosol injection experiment GeoMIP G4 and the CMIP RCP4.5 and RCP8.5 greenhouse gas scenarios that were then used to drive the surface energy and mass balance model, SEMIC. Simulated runoff is 20% lower under G4 than RCP4.5, while under RCP8.5 it is 17% higher. The mechanism is through increased Arctic sea ice concentration and reduced humidity leading to surface cooling of the ablation zone. Reduced absorption of outgoing longwave radiation caused by hydrological cycle weakening dominates associated decreases in precipitation under geoengineering and stronger AMOC than under RCP4.5. An ice dynamics model simulates 15% lower ice losses under G4 than RCP4.5. Thus, total sea level rise by 2070 from the Greenland ice sheet under G4 geoengineering is about 15–20% lower than under the RCP4.5 scenario. |
format |
Article in Journal/Newspaper |
author |
John C. Moore Chao Yue Liyun Zhao Xiaoran Guo Shingo Watanabe Duoying Ji |
author_facet |
John C. Moore Chao Yue Liyun Zhao Xiaoran Guo Shingo Watanabe Duoying Ji |
author_sort |
John C. Moore |
title |
Greenland Ice Sheet Response to Stratospheric Aerosol Injection Geoengineering |
title_short |
Greenland Ice Sheet Response to Stratospheric Aerosol Injection Geoengineering |
title_full |
Greenland Ice Sheet Response to Stratospheric Aerosol Injection Geoengineering |
title_fullStr |
Greenland Ice Sheet Response to Stratospheric Aerosol Injection Geoengineering |
title_full_unstemmed |
Greenland Ice Sheet Response to Stratospheric Aerosol Injection Geoengineering |
title_sort |
greenland ice sheet response to stratospheric aerosol injection geoengineering |
publisher |
Wiley |
publishDate |
2019 |
url |
https://doi.org/10.1029/2019EF001393 https://doaj.org/article/9cfce3433f7e44c1b7ba0c8359e2e48a |
geographic |
Arctic Greenland |
geographic_facet |
Arctic Greenland |
genre |
Arctic glacier Greenland Ice Sheet Sea ice |
genre_facet |
Arctic glacier Greenland Ice Sheet Sea ice |
op_source |
Earth's Future, Vol 7, Iss 12, Pp 1451-1463 (2019) |
op_relation |
2328-4277 doi:10.1029/2019EF001393 https://doaj.org/article/9cfce3433f7e44c1b7ba0c8359e2e48a |
op_rights |
undefined |
op_doi |
https://doi.org/10.1029/2019EF001393 |
container_title |
Earth's Future |
container_volume |
7 |
container_issue |
12 |
container_start_page |
1451 |
op_container_end_page |
1463 |
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1766340569956614144 |