Dynamic climate emulators for solar geoengineering

Climate emulators trained on existing simulations can be used to project project the climate effects that result from different possible future pathways of anthropogenic forcing, without further relying on general circulation model (GCM) simulations. We extend this idea to include different amounts...

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Published in:Atmospheric Chemistry and Physics
Main Authors: MacMartin, Douglas G., Kravitz, Ben
Format: Article in Journal/Newspaper
Language:unknown
Published: European Geosciences Union 2016
Subjects:
Online Access:https://doi.org/10.5194/acp-16-15789-2016
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spelling ftcaltechauth:oai:authors.library.caltech.edu:rdezs-p4d81 2024-09-15T18:35:21+00:00 Dynamic climate emulators for solar geoengineering MacMartin, Douglas G. Kravitz, Ben 2016-12-22 https://doi.org/10.5194/acp-16-15789-2016 unknown European Geosciences Union https://doi.org/10.5194/acp-16-15789-2016 oai:authors.library.caltech.edu:rdezs-p4d81 eprintid:73979 resolverid:CaltechAUTHORS:20170202-082033858 info:eu-repo/semantics/openAccess Other Atmospheric Chemistry and Physics, 16(24), 15789-15799, (2016-12-22) info:eu-repo/semantics/article 2016 ftcaltechauth https://doi.org/10.5194/acp-16-15789-2016 2024-08-06T15:34:58Z Climate emulators trained on existing simulations can be used to project project the climate effects that result from different possible future pathways of anthropogenic forcing, without further relying on general circulation model (GCM) simulations. We extend this idea to include different amounts of solar geoengineering in addition to different pathways of greenhouse gas concentrations, by training emulators from a multi-model ensemble of simulations from the Geoengineering Model Intercomparison Project (GeoMIP). The emulator is trained on the abrupt 4 × CO_2 and a compensating solar reduction simulation (G1), and evaluated by comparing predictions against a simulated 1 % per year CO_2 increase and a similarly smaller solar reduction (G2). We find reasonable agreement in most models for predicting changes in temperature and precipitation (including regional effects), and annual-mean Northern Hemisphere sea ice extent, with the difference between simulation and prediction typically being smaller than natural variability. This verifies that the linearity assumption used in constructing the emulator is sufficient for these variables over the range of forcing considered. Annual-minimum Northern Hemisphere sea ice extent is less well predicted, indicating a limit to the linearity assumption. © 2016 Author(s). This work is distributed under the Creative Commons Attribution 3.0 License. Published by Copernicus Publications on behalf of the European Geosciences Union. Received: 17 June 2016 – Published in Atmos. Chem. Phys. Discuss.: 24 June 2016; Revised: 18 November 2016 – Accepted: 22 November 2016 – Published: 22 December 2016. We thank all participants of the Geoengineering Model Intercomparison Project and their model development teams, CLIVAR/WCRP Working Group on Coupled Modeling for endorsing GeoMIP, and the scientists managing the Earth System Grid data nodes, who assisted with making GeoMIP output available. The Pacific Northwest National Laboratory is operated for the U.S. Department of ... Article in Journal/Newspaper Sea ice Caltech Authors (California Institute of Technology) Atmospheric Chemistry and Physics 16 24 15789 15799
institution Open Polar
collection Caltech Authors (California Institute of Technology)
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language unknown
description Climate emulators trained on existing simulations can be used to project project the climate effects that result from different possible future pathways of anthropogenic forcing, without further relying on general circulation model (GCM) simulations. We extend this idea to include different amounts of solar geoengineering in addition to different pathways of greenhouse gas concentrations, by training emulators from a multi-model ensemble of simulations from the Geoengineering Model Intercomparison Project (GeoMIP). The emulator is trained on the abrupt 4 × CO_2 and a compensating solar reduction simulation (G1), and evaluated by comparing predictions against a simulated 1 % per year CO_2 increase and a similarly smaller solar reduction (G2). We find reasonable agreement in most models for predicting changes in temperature and precipitation (including regional effects), and annual-mean Northern Hemisphere sea ice extent, with the difference between simulation and prediction typically being smaller than natural variability. This verifies that the linearity assumption used in constructing the emulator is sufficient for these variables over the range of forcing considered. Annual-minimum Northern Hemisphere sea ice extent is less well predicted, indicating a limit to the linearity assumption. © 2016 Author(s). This work is distributed under the Creative Commons Attribution 3.0 License. Published by Copernicus Publications on behalf of the European Geosciences Union. Received: 17 June 2016 – Published in Atmos. Chem. Phys. Discuss.: 24 June 2016; Revised: 18 November 2016 – Accepted: 22 November 2016 – Published: 22 December 2016. We thank all participants of the Geoengineering Model Intercomparison Project and their model development teams, CLIVAR/WCRP Working Group on Coupled Modeling for endorsing GeoMIP, and the scientists managing the Earth System Grid data nodes, who assisted with making GeoMIP output available. The Pacific Northwest National Laboratory is operated for the U.S. Department of ...
format Article in Journal/Newspaper
author MacMartin, Douglas G.
Kravitz, Ben
spellingShingle MacMartin, Douglas G.
Kravitz, Ben
Dynamic climate emulators for solar geoengineering
author_facet MacMartin, Douglas G.
Kravitz, Ben
author_sort MacMartin, Douglas G.
title Dynamic climate emulators for solar geoengineering
title_short Dynamic climate emulators for solar geoengineering
title_full Dynamic climate emulators for solar geoengineering
title_fullStr Dynamic climate emulators for solar geoengineering
title_full_unstemmed Dynamic climate emulators for solar geoengineering
title_sort dynamic climate emulators for solar geoengineering
publisher European Geosciences Union
publishDate 2016
url https://doi.org/10.5194/acp-16-15789-2016
genre Sea ice
genre_facet Sea ice
op_source Atmospheric Chemistry and Physics, 16(24), 15789-15799, (2016-12-22)
op_relation https://doi.org/10.5194/acp-16-15789-2016
oai:authors.library.caltech.edu:rdezs-p4d81
eprintid:73979
resolverid:CaltechAUTHORS:20170202-082033858
op_rights info:eu-repo/semantics/openAccess
Other
op_doi https://doi.org/10.5194/acp-16-15789-2016
container_title Atmospheric Chemistry and Physics
container_volume 16
container_issue 24
container_start_page 15789
op_container_end_page 15799
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