PLASIM–GENIE v1.0: a new intermediate complexity AOGCM

We describe the development, tuning and climate of Planet Simulator (PLASIM)–Grid-ENabled Integrated Earth system model (GENIE), a new intermediate complexity Atmosphere–Ocean General Circulation Model (AOGCM), built by coupling the Planet Simulator to the ocean, sea-ice and land-surface components...

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Published in:Geoscientific Model Development
Main Authors: Holden, Philip B., Edwards, Neil R., Fraedrich, Klaus, Kirk, Edilbert, Lunkeit, Frank, Zhu, Xiuhua
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/gmd-9-3347-2016
https://gmd.copernicus.org/articles/9/3347/2016/
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spelling ftcopernicus:oai:publications.copernicus.org:gmd48373 2023-05-15T18:18:36+02:00 PLASIM–GENIE v1.0: a new intermediate complexity AOGCM Holden, Philip B. Edwards, Neil R. Fraedrich, Klaus Kirk, Edilbert Lunkeit, Frank Zhu, Xiuhua 2018-09-27 application/pdf https://doi.org/10.5194/gmd-9-3347-2016 https://gmd.copernicus.org/articles/9/3347/2016/ eng eng doi:10.5194/gmd-9-3347-2016 https://gmd.copernicus.org/articles/9/3347/2016/ eISSN: 1991-9603 Text 2018 ftcopernicus https://doi.org/10.5194/gmd-9-3347-2016 2020-07-20T16:23:59Z We describe the development, tuning and climate of Planet Simulator (PLASIM)–Grid-ENabled Integrated Earth system model (GENIE), a new intermediate complexity Atmosphere–Ocean General Circulation Model (AOGCM), built by coupling the Planet Simulator to the ocean, sea-ice and land-surface components of the GENIE Earth system model. PLASIM–GENIE supersedes GENIE-2, a coupling of GENIE to the Reading Intermediate General Circulation Model (IGCM). The primitive-equation atmosphere includes chaotic, three-dimensional (3-D) motion and interactive radiation and clouds, and dominates the computational load compared to the relatively simpler frictional-geostrophic ocean, which neglects momentum advection. The model is most appropriate for long-timescale or large ensemble studies where numerical efficiency is prioritised, but lack of data necessitates an internally consistent, coupled calculation of both oceanic and atmospheric fields. A 1000-year simulation with PLASIM–GENIE requires approximately 2 weeks on a single node of a 2.1 GHz AMD 6172 CPU. We demonstrate the tractability of PLASIM–GENIE ensembles by deriving a subjective tuning of the model with a 50-member ensemble of 1000-year simulations. The simulated climate is presented considering (i) global fields of seasonal surface air temperature, precipitation, wind, solar and thermal radiation, with comparisons to reanalysis data; (ii) vegetation carbon, soil moisture and aridity index; and (iii) sea surface temperature, salinity and ocean circulation. Considering its resolution, PLASIM–GENIE reproduces the main features of the climate system well and demonstrates usefulness for a wide range of applications. Text Sea ice Copernicus Publications: E-Journals Geoscientific Model Development 9 9 3347 3361
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collection Copernicus Publications: E-Journals
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language English
description We describe the development, tuning and climate of Planet Simulator (PLASIM)–Grid-ENabled Integrated Earth system model (GENIE), a new intermediate complexity Atmosphere–Ocean General Circulation Model (AOGCM), built by coupling the Planet Simulator to the ocean, sea-ice and land-surface components of the GENIE Earth system model. PLASIM–GENIE supersedes GENIE-2, a coupling of GENIE to the Reading Intermediate General Circulation Model (IGCM). The primitive-equation atmosphere includes chaotic, three-dimensional (3-D) motion and interactive radiation and clouds, and dominates the computational load compared to the relatively simpler frictional-geostrophic ocean, which neglects momentum advection. The model is most appropriate for long-timescale or large ensemble studies where numerical efficiency is prioritised, but lack of data necessitates an internally consistent, coupled calculation of both oceanic and atmospheric fields. A 1000-year simulation with PLASIM–GENIE requires approximately 2 weeks on a single node of a 2.1 GHz AMD 6172 CPU. We demonstrate the tractability of PLASIM–GENIE ensembles by deriving a subjective tuning of the model with a 50-member ensemble of 1000-year simulations. The simulated climate is presented considering (i) global fields of seasonal surface air temperature, precipitation, wind, solar and thermal radiation, with comparisons to reanalysis data; (ii) vegetation carbon, soil moisture and aridity index; and (iii) sea surface temperature, salinity and ocean circulation. Considering its resolution, PLASIM–GENIE reproduces the main features of the climate system well and demonstrates usefulness for a wide range of applications.
format Text
author Holden, Philip B.
Edwards, Neil R.
Fraedrich, Klaus
Kirk, Edilbert
Lunkeit, Frank
Zhu, Xiuhua
spellingShingle Holden, Philip B.
Edwards, Neil R.
Fraedrich, Klaus
Kirk, Edilbert
Lunkeit, Frank
Zhu, Xiuhua
PLASIM–GENIE v1.0: a new intermediate complexity AOGCM
author_facet Holden, Philip B.
Edwards, Neil R.
Fraedrich, Klaus
Kirk, Edilbert
Lunkeit, Frank
Zhu, Xiuhua
author_sort Holden, Philip B.
title PLASIM–GENIE v1.0: a new intermediate complexity AOGCM
title_short PLASIM–GENIE v1.0: a new intermediate complexity AOGCM
title_full PLASIM–GENIE v1.0: a new intermediate complexity AOGCM
title_fullStr PLASIM–GENIE v1.0: a new intermediate complexity AOGCM
title_full_unstemmed PLASIM–GENIE v1.0: a new intermediate complexity AOGCM
title_sort plasim–genie v1.0: a new intermediate complexity aogcm
publishDate 2018
url https://doi.org/10.5194/gmd-9-3347-2016
https://gmd.copernicus.org/articles/9/3347/2016/
genre Sea ice
genre_facet Sea ice
op_source eISSN: 1991-9603
op_relation doi:10.5194/gmd-9-3347-2016
https://gmd.copernicus.org/articles/9/3347/2016/
op_doi https://doi.org/10.5194/gmd-9-3347-2016
container_title Geoscientific Model Development
container_volume 9
container_issue 9
container_start_page 3347
op_container_end_page 3361
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