An Intermediate Complexity Climate Model (ICCMp1) based on the GFDL flexible modelling system

An intermediate complexity coupled ocean-atmosphere-land-ice model, based on the Geophysical Fluid Dynamics Laboratory (GFDL) Flexible Modelling System (FMS), has been developed to study mechanisms of ocean-atmosphere interactions and natural climate variability at interannual to interdecadal and lo...

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Main Authors: R. Farneti, G. K. Vallis
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2009
Subjects:
Online Access:https://doaj.org/article/a202dc297667498e883489d5c2f1e079
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spelling ftdoajarticles:oai:doaj.org/article:a202dc297667498e883489d5c2f1e079 2023-05-15T18:18:40+02:00 An Intermediate Complexity Climate Model (ICCMp1) based on the GFDL flexible modelling system R. Farneti G. K. Vallis 2009-07-01T00:00:00Z https://doaj.org/article/a202dc297667498e883489d5c2f1e079 EN eng Copernicus Publications http://www.geosci-model-dev.net/2/73/2009/gmd-2-73-2009.pdf https://doaj.org/toc/1991-959X https://doaj.org/toc/1991-9603 1991-959X 1991-9603 https://doaj.org/article/a202dc297667498e883489d5c2f1e079 Geoscientific Model Development, Vol 2, Iss 2, Pp 73-88 (2009) Geology QE1-996.5 article 2009 ftdoajarticles 2022-12-31T01:53:57Z An intermediate complexity coupled ocean-atmosphere-land-ice model, based on the Geophysical Fluid Dynamics Laboratory (GFDL) Flexible Modelling System (FMS), has been developed to study mechanisms of ocean-atmosphere interactions and natural climate variability at interannual to interdecadal and longer time scales. The model uses the three-dimensional primitive equations for both ocean and atmosphere but is simplified from a "state of the art" coupled model by using simplified atmospheric physics and parameterisation schemes. These simplifications provide considerable savings in computational expense and, perhaps more importantly, allow mechanisms to be investigated more cleanly and thoroughly than with a more elaborate model. For example, the model allows integrations of several millennia as well as broad parameter studies. For the ocean, the model uses the free surface primitive equations Modular Ocean Model (MOM) and the GFDL/FMS sea-ice model (SIS) is coupled to the oceanic grid. The atmospheric component consists of the FMS B-grid moist primitive equations atmospheric dynamical core with highly simplified physical parameterisations. A simple bucket model is implemented for our idealised land following the GFDL/FMS Land model. The model is supported within the standard MOM releases as one of its many test cases and the source code is thus freely available. Here we describe the model components and present a climatology of coupled simulations achieved with two different geometrical configurations. Throughout the paper, we give a flavour of the potential for this model to be a powerful tool for the climate modelling community by mentioning a wide range of studies that are currently being explored. Article in Journal/Newspaper Sea ice Directory of Open Access Journals: DOAJ Articles
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Geology
QE1-996.5
spellingShingle Geology
QE1-996.5
R. Farneti
G. K. Vallis
An Intermediate Complexity Climate Model (ICCMp1) based on the GFDL flexible modelling system
topic_facet Geology
QE1-996.5
description An intermediate complexity coupled ocean-atmosphere-land-ice model, based on the Geophysical Fluid Dynamics Laboratory (GFDL) Flexible Modelling System (FMS), has been developed to study mechanisms of ocean-atmosphere interactions and natural climate variability at interannual to interdecadal and longer time scales. The model uses the three-dimensional primitive equations for both ocean and atmosphere but is simplified from a "state of the art" coupled model by using simplified atmospheric physics and parameterisation schemes. These simplifications provide considerable savings in computational expense and, perhaps more importantly, allow mechanisms to be investigated more cleanly and thoroughly than with a more elaborate model. For example, the model allows integrations of several millennia as well as broad parameter studies. For the ocean, the model uses the free surface primitive equations Modular Ocean Model (MOM) and the GFDL/FMS sea-ice model (SIS) is coupled to the oceanic grid. The atmospheric component consists of the FMS B-grid moist primitive equations atmospheric dynamical core with highly simplified physical parameterisations. A simple bucket model is implemented for our idealised land following the GFDL/FMS Land model. The model is supported within the standard MOM releases as one of its many test cases and the source code is thus freely available. Here we describe the model components and present a climatology of coupled simulations achieved with two different geometrical configurations. Throughout the paper, we give a flavour of the potential for this model to be a powerful tool for the climate modelling community by mentioning a wide range of studies that are currently being explored.
format Article in Journal/Newspaper
author R. Farneti
G. K. Vallis
author_facet R. Farneti
G. K. Vallis
author_sort R. Farneti
title An Intermediate Complexity Climate Model (ICCMp1) based on the GFDL flexible modelling system
title_short An Intermediate Complexity Climate Model (ICCMp1) based on the GFDL flexible modelling system
title_full An Intermediate Complexity Climate Model (ICCMp1) based on the GFDL flexible modelling system
title_fullStr An Intermediate Complexity Climate Model (ICCMp1) based on the GFDL flexible modelling system
title_full_unstemmed An Intermediate Complexity Climate Model (ICCMp1) based on the GFDL flexible modelling system
title_sort intermediate complexity climate model (iccmp1) based on the gfdl flexible modelling system
publisher Copernicus Publications
publishDate 2009
url https://doaj.org/article/a202dc297667498e883489d5c2f1e079
genre Sea ice
genre_facet Sea ice
op_source Geoscientific Model Development, Vol 2, Iss 2, Pp 73-88 (2009)
op_relation http://www.geosci-model-dev.net/2/73/2009/gmd-2-73-2009.pdf
https://doaj.org/toc/1991-959X
https://doaj.org/toc/1991-9603
1991-959X
1991-9603
https://doaj.org/article/a202dc297667498e883489d5c2f1e079
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