The Radiative Forcing Model Intercomparison Project (RFMIP): experimental protocol for CMIP6

The phrasing of the first of three questions motivating CMIP6 – “How does the Earth system respond to forcing?” – suggests that forcing is always well-known, yet the radiative forcing to which this question refers has historically been uncertain in coordinated experiments even as understanding of ho...

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Main Authors: R. Pincus, P. M. Forster, B. Stevens
Format: Article
Language:English
Published: Copernicus Publications 2016-09-01
Series:Geoscientific Model Development
Online Access:http://www.geosci-model-dev.net/9/3447/2016/gmd-9-3447-2016.pdf
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author R. Pincus
P. M. Forster
B. Stevens
author_facet R. Pincus
P. M. Forster
B. Stevens
author_sort R. Pincus
collection DOAJ
description The phrasing of the first of three questions motivating CMIP6 – “How does the Earth system respond to forcing?” – suggests that forcing is always well-known, yet the radiative forcing to which this question refers has historically been uncertain in coordinated experiments even as understanding of how best to infer radiative forcing has evolved. The Radiative Forcing Model Intercomparison Project (RFMIP) endorsed by CMIP6 seeks to provide a foundation for answering the question through three related activities: (i) accurate characterization of the effective radiative forcing relative to a near-preindustrial baseline and careful diagnosis of the components of this forcing; (ii) assessment of the absolute accuracy of clear-sky radiative transfer parameterizations against reference models on the global scales relevant for climate modeling; and (iii) identification of robust model responses to tightly specified aerosol radiative forcing from 1850 to present. <br><br> Complete characterization of effective radiative forcing can be accomplished with 180 years (Tier 1) of atmosphere-only simulation using a sea-surface temperature and sea ice concentration climatology derived from the host model's preindustrial control simulation. Assessment of parameterization error requires trivial amounts of computation but the development of small amounts of infrastructure: new, spectrally detailed diagnostic output requested as two snapshots at present-day and preindustrial conditions, and results from the model's radiation code applied to specified atmospheric conditions. The search for robust responses to aerosol changes relies on the CMIP6 specification of anthropogenic aerosol properties; models using this specification can contribute to RFMIP with no additional simulation, while those using a full aerosol model are requested to perform at least one and up to four 165-year coupled ocean–atmosphere simulations at Tier 1.
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spelling doaj.art-8df966fd5b944bdc9547de2f56550d282022-12-22T00:58:06ZengCopernicus PublicationsGeoscientific Model Development1991-959X1991-96032016-09-01993447346010.5194/gmd-9-3447-2016The Radiative Forcing Model Intercomparison Project (RFMIP): experimental protocol for CMIP6R. Pincus0P. M. Forster1B. Stevens2Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO 80309, USAInstitute for Climate and Atmospheric Science, School of Earth and Environment, University of Leeds, Leeds, UKMax Planck Institute for Meteorology, Hamburg 20146, GermanyThe phrasing of the first of three questions motivating CMIP6 – “How does the Earth system respond to forcing?” – suggests that forcing is always well-known, yet the radiative forcing to which this question refers has historically been uncertain in coordinated experiments even as understanding of how best to infer radiative forcing has evolved. The Radiative Forcing Model Intercomparison Project (RFMIP) endorsed by CMIP6 seeks to provide a foundation for answering the question through three related activities: (i) accurate characterization of the effective radiative forcing relative to a near-preindustrial baseline and careful diagnosis of the components of this forcing; (ii) assessment of the absolute accuracy of clear-sky radiative transfer parameterizations against reference models on the global scales relevant for climate modeling; and (iii) identification of robust model responses to tightly specified aerosol radiative forcing from 1850 to present. <br><br> Complete characterization of effective radiative forcing can be accomplished with 180 years (Tier 1) of atmosphere-only simulation using a sea-surface temperature and sea ice concentration climatology derived from the host model's preindustrial control simulation. Assessment of parameterization error requires trivial amounts of computation but the development of small amounts of infrastructure: new, spectrally detailed diagnostic output requested as two snapshots at present-day and preindustrial conditions, and results from the model's radiation code applied to specified atmospheric conditions. The search for robust responses to aerosol changes relies on the CMIP6 specification of anthropogenic aerosol properties; models using this specification can contribute to RFMIP with no additional simulation, while those using a full aerosol model are requested to perform at least one and up to four 165-year coupled ocean–atmosphere simulations at Tier 1.http://www.geosci-model-dev.net/9/3447/2016/gmd-9-3447-2016.pdf
spellingShingle R. Pincus
P. M. Forster
B. Stevens
The Radiative Forcing Model Intercomparison Project (RFMIP): experimental protocol for CMIP6
Geoscientific Model Development
title The Radiative Forcing Model Intercomparison Project (RFMIP): experimental protocol for CMIP6
title_full The Radiative Forcing Model Intercomparison Project (RFMIP): experimental protocol for CMIP6
title_fullStr The Radiative Forcing Model Intercomparison Project (RFMIP): experimental protocol for CMIP6
title_full_unstemmed The Radiative Forcing Model Intercomparison Project (RFMIP): experimental protocol for CMIP6
title_short The Radiative Forcing Model Intercomparison Project (RFMIP): experimental protocol for CMIP6
title_sort radiative forcing model intercomparison project rfmip experimental protocol for cmip6
url http://www.geosci-model-dev.net/9/3447/2016/gmd-9-3447-2016.pdf
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