Changing the Climate Sensitivity of an Atmospheric General Circulation Model through Cloud Radiative Adjustment
Conducting probabilistic climate projections with a particular climate model requires the ability to vary the model’s characteristics, such as its climate sensitivity. In this study, the authors implement and validate a method to change the climate sensitivity of the National Center for Atmospheric...
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American Meteorological Society
2013
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Online Access: | http://hdl.handle.net/1721.1/78856 https://orcid.org/0000-0001-5533-6570 |
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author | Sokolov, Andrei P. Monier, Erwan |
author2 | Massachusetts Institute of Technology. Center for Global Change Science |
author_facet | Massachusetts Institute of Technology. Center for Global Change Science Sokolov, Andrei P. Monier, Erwan |
author_sort | Sokolov, Andrei P. |
collection | MIT |
description | Conducting probabilistic climate projections with a particular climate model requires the ability to vary the model’s characteristics, such as its climate sensitivity. In this study, the authors implement and validate a method to change the climate sensitivity of the National Center for Atmospheric Research (NCAR) Community Atmosphere Model, version 3 (CAM3), through cloud radiative adjustment. Results show that the cloud radiative adjustment method does not lead to physically unrealistic changes in the model’s response to an external forcing, such as doubling CO2 concentrations or increasing sulfate aerosol concentrations. Furthermore, this method has some advantages compared to the traditional perturbed physics approach. In particular, the cloud radiative adjustment method can produce any value of climate sensitivity within the wide range of uncertainty based on the observed twentieth century climate change. As a consequence, this method allows Monte Carlo–type probabilistic climate forecasts to be conducted where values of uncertain parameters not only cover the whole uncertainty range, but cover it homogeneously. Unlike the perturbed physics approach that can produce several versions of a model with the same climate sensitivity but with very different regional patterns of change, the cloud radiative adjustment method can only produce one version of the model with a specific climate sensitivity. As such, a limitation of this method is that it cannot cover the full uncertainty in regional patterns of climate change. |
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institution | Massachusetts Institute of Technology |
language | en_US |
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publishDate | 2013 |
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spelling | mit-1721.1/788562022-09-28T17:11:35Z Changing the Climate Sensitivity of an Atmospheric General Circulation Model through Cloud Radiative Adjustment Sokolov, Andrei P. Monier, Erwan Massachusetts Institute of Technology. Center for Global Change Science Massachusetts Institute of Technology. Joint Program on the Science & Policy of Global Change Sokolov, Andrei P. Monier, Erwan Conducting probabilistic climate projections with a particular climate model requires the ability to vary the model’s characteristics, such as its climate sensitivity. In this study, the authors implement and validate a method to change the climate sensitivity of the National Center for Atmospheric Research (NCAR) Community Atmosphere Model, version 3 (CAM3), through cloud radiative adjustment. Results show that the cloud radiative adjustment method does not lead to physically unrealistic changes in the model’s response to an external forcing, such as doubling CO2 concentrations or increasing sulfate aerosol concentrations. Furthermore, this method has some advantages compared to the traditional perturbed physics approach. In particular, the cloud radiative adjustment method can produce any value of climate sensitivity within the wide range of uncertainty based on the observed twentieth century climate change. As a consequence, this method allows Monte Carlo–type probabilistic climate forecasts to be conducted where values of uncertain parameters not only cover the whole uncertainty range, but cover it homogeneously. Unlike the perturbed physics approach that can produce several versions of a model with the same climate sensitivity but with very different regional patterns of change, the cloud radiative adjustment method can only produce one version of the model with a specific climate sensitivity. As such, a limitation of this method is that it cannot cover the full uncertainty in regional patterns of climate change. 2013-05-09T21:02:01Z 2013-05-09T21:02:01Z 2012-10 2011-10 Article http://purl.org/eprint/type/JournalArticle 0894-8755 1520-0442 http://hdl.handle.net/1721.1/78856 Sokolov, Andrei P., and Erwan Monier. “Changing the Climate Sensitivity of an Atmospheric General Circulation Model through Cloud Radiative Adjustment.” Journal of Climate 25.19 (2012): 6567–6584. ©2013 American Meteorological Society https://orcid.org/0000-0001-5533-6570 en_US http://dx.doi.org/10.1175/jcli-d-11-00590.1 Journal of Climate Article is made available in accordance with the publisher's policy and may be subject to US copyright law. Please refer to the publisher's site for terms of use. application/pdf American Meteorological Society American Meteorological Society |
spellingShingle | Sokolov, Andrei P. Monier, Erwan Changing the Climate Sensitivity of an Atmospheric General Circulation Model through Cloud Radiative Adjustment |
title | Changing the Climate Sensitivity of an Atmospheric General Circulation Model through Cloud Radiative Adjustment |
title_full | Changing the Climate Sensitivity of an Atmospheric General Circulation Model through Cloud Radiative Adjustment |
title_fullStr | Changing the Climate Sensitivity of an Atmospheric General Circulation Model through Cloud Radiative Adjustment |
title_full_unstemmed | Changing the Climate Sensitivity of an Atmospheric General Circulation Model through Cloud Radiative Adjustment |
title_short | Changing the Climate Sensitivity of an Atmospheric General Circulation Model through Cloud Radiative Adjustment |
title_sort | changing the climate sensitivity of an atmospheric general circulation model through cloud radiative adjustment |
url | http://hdl.handle.net/1721.1/78856 https://orcid.org/0000-0001-5533-6570 |
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