Climate model response from the Geoengineering Model Intercomparison Project (GeoMIP)
Solar geoengineering - deliberate reduction in the amount of solar radiation retained by the Earth - has been proposed as a means of counteracting some of the climatic effects of anthropogenic greenhouse gas emissions. We present results from Experiment G1 of the Geoengineering Model Intercomparison...
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ftpubman:oai:pure.mpg.de:item_1838004 2023-08-27T04:08:08+02:00 Climate model response from the Geoengineering Model Intercomparison Project (GeoMIP) Kravitz, B. Caldeira, K. Boucher, O. Robock, A. Rasch, P. Alterskjær, K. Karam, D. Cole, J. Curry, C. Haywood, J. Irvine, P. Ji, D. Jones, A. Kristjánsson, J. Lunt, D. Moore, J. Niemeier, U. Schmidt, H. Schulz, M. Singh, B. Tilmes, S. Watanabe, S. Yang, S. Yoon, J. 2013-08-09 application/pdf http://hdl.handle.net/11858/00-001M-0000-0014-5E36-8 http://hdl.handle.net/11858/00-001M-0000-0014-6063-5 eng eng info:eu-repo/semantics/altIdentifier/doi/10.1002/jgrd.50646 http://hdl.handle.net/11858/00-001M-0000-0014-5E36-8 http://hdl.handle.net/11858/00-001M-0000-0014-6063-5 info:eu-repo/semantics/openAccess Journal of Geophysical Research-Atmospheres info:eu-repo/semantics/article 2013 ftpubman https://doi.org/10.1002/jgrd.50646 2023-08-02T01:33:57Z Solar geoengineering - deliberate reduction in the amount of solar radiation retained by the Earth - has been proposed as a means of counteracting some of the climatic effects of anthropogenic greenhouse gas emissions. We present results from Experiment G1 of the Geoengineering Model Intercomparison Project, in which 12 climate models have simulated the climate response to an abrupt quadrupling of CO2 from preindustrial concentrations brought into radiative balance via a globally uniform reduction in insolation. Models show this reduction largely offsets global mean surface temperature increases due to quadrupled CO2 concentrations and prevents 97% of the Arctic sea ice loss that would otherwise occur under high CO2 levels but, compared to the preindustrial climate, leaves the tropics cooler (-0.3 K) and the poles warmer (+0.8 K). Annual mean precipitation minus evaporation anomalies for G1 are less than 0.2 mm day-1 in magnitude over 92% of the globe, but some tropical regions receive less precipitation, in part due to increased moist static stability and suppression of convection. Global average net primary productivity increases by 120% in G1 over simulated preindustrial levels, primarily from CO2 fertilization, but also in part due to reduced plant heat stress compared to a high CO2 world with no geoengineering. All models show that uniform solar geoengineering in G1 cannot simultaneously return regional and global temperature and hydrologic cycle intensity to preindustrial levels. Key Points Temperature reduction from uniform geoengineering is not uniform Geoengineering cannot offset both temperature and hydrology changes NPP increases mostly due to CO2 fertilization ©2013. American Geophysical Union. All Rights Reserved. Article in Journal/Newspaper Arctic Sea ice Max Planck Society: MPG.PuRe Arctic Journal of Geophysical Research: Atmospheres 118 15 8320 8332 |
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Max Planck Society: MPG.PuRe |
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ftpubman |
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English |
description |
Solar geoengineering - deliberate reduction in the amount of solar radiation retained by the Earth - has been proposed as a means of counteracting some of the climatic effects of anthropogenic greenhouse gas emissions. We present results from Experiment G1 of the Geoengineering Model Intercomparison Project, in which 12 climate models have simulated the climate response to an abrupt quadrupling of CO2 from preindustrial concentrations brought into radiative balance via a globally uniform reduction in insolation. Models show this reduction largely offsets global mean surface temperature increases due to quadrupled CO2 concentrations and prevents 97% of the Arctic sea ice loss that would otherwise occur under high CO2 levels but, compared to the preindustrial climate, leaves the tropics cooler (-0.3 K) and the poles warmer (+0.8 K). Annual mean precipitation minus evaporation anomalies for G1 are less than 0.2 mm day-1 in magnitude over 92% of the globe, but some tropical regions receive less precipitation, in part due to increased moist static stability and suppression of convection. Global average net primary productivity increases by 120% in G1 over simulated preindustrial levels, primarily from CO2 fertilization, but also in part due to reduced plant heat stress compared to a high CO2 world with no geoengineering. All models show that uniform solar geoengineering in G1 cannot simultaneously return regional and global temperature and hydrologic cycle intensity to preindustrial levels. Key Points Temperature reduction from uniform geoengineering is not uniform Geoengineering cannot offset both temperature and hydrology changes NPP increases mostly due to CO2 fertilization ©2013. American Geophysical Union. All Rights Reserved. |
format |
Article in Journal/Newspaper |
author |
Kravitz, B. Caldeira, K. Boucher, O. Robock, A. Rasch, P. Alterskjær, K. Karam, D. Cole, J. Curry, C. Haywood, J. Irvine, P. Ji, D. Jones, A. Kristjánsson, J. Lunt, D. Moore, J. Niemeier, U. Schmidt, H. Schulz, M. Singh, B. Tilmes, S. Watanabe, S. Yang, S. Yoon, J. |
spellingShingle |
Kravitz, B. Caldeira, K. Boucher, O. Robock, A. Rasch, P. Alterskjær, K. Karam, D. Cole, J. Curry, C. Haywood, J. Irvine, P. Ji, D. Jones, A. Kristjánsson, J. Lunt, D. Moore, J. Niemeier, U. Schmidt, H. Schulz, M. Singh, B. Tilmes, S. Watanabe, S. Yang, S. Yoon, J. Climate model response from the Geoengineering Model Intercomparison Project (GeoMIP) |
author_facet |
Kravitz, B. Caldeira, K. Boucher, O. Robock, A. Rasch, P. Alterskjær, K. Karam, D. Cole, J. Curry, C. Haywood, J. Irvine, P. Ji, D. Jones, A. Kristjánsson, J. Lunt, D. Moore, J. Niemeier, U. Schmidt, H. Schulz, M. Singh, B. Tilmes, S. Watanabe, S. Yang, S. Yoon, J. |
author_sort |
Kravitz, B. |
title |
Climate model response from the Geoengineering Model Intercomparison Project (GeoMIP) |
title_short |
Climate model response from the Geoengineering Model Intercomparison Project (GeoMIP) |
title_full |
Climate model response from the Geoengineering Model Intercomparison Project (GeoMIP) |
title_fullStr |
Climate model response from the Geoengineering Model Intercomparison Project (GeoMIP) |
title_full_unstemmed |
Climate model response from the Geoengineering Model Intercomparison Project (GeoMIP) |
title_sort |
climate model response from the geoengineering model intercomparison project (geomip) |
publishDate |
2013 |
url |
http://hdl.handle.net/11858/00-001M-0000-0014-5E36-8 http://hdl.handle.net/11858/00-001M-0000-0014-6063-5 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Sea ice |
genre_facet |
Arctic Sea ice |
op_source |
Journal of Geophysical Research-Atmospheres |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1002/jgrd.50646 http://hdl.handle.net/11858/00-001M-0000-0014-5E36-8 http://hdl.handle.net/11858/00-001M-0000-0014-6063-5 |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1002/jgrd.50646 |
container_title |
Journal of Geophysical Research: Atmospheres |
container_volume |
118 |
container_issue |
15 |
container_start_page |
8320 |
op_container_end_page |
8332 |
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1775348832575422464 |