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The ACCESS coupled model: description, control climate and evaluation

Daohua BiCollaboration for Australian Weather and Climate ResearchMartin DixHealth Sciences and NutritionSimon MarslandCommonwealth Scientific and Industrial Research OrganisationSiobhan O’FarrellCollaboration for Australian Weather and Climate ResearchHarun RashidCollaboration for Australian Weather and Climate ResearchPetteri UotilaCollaboration for Australian Weather and Climate ResearchAndrew G. HirstCommonwealth Scientific and Industrial Research OrganisationEva KowalczykHealth Sciences and NutritionMaciej GolebiewskiCSIRO High Performance Computing and Communications Centre, Melbourne, AustraliaArnold SullivanCollaboration for Australian Weather and Climate ResearchHailin YanCAWCR/CSIRO Marine and Atmospheric Research, Aspendale, AustraliaNicholas HannahHealth Sciences and NutritionCharmaine FranklinCollaboration for Australian Weather and Climate ResearchZhaobin SunCollaboration for Australian Weather and Climate ResearchPeter VohralikCSIRO Materials Science and Engineering, Lindfield, AustraliaI. G. WattersonCAWCR/CSIRO Marine and Atmospheric Research, Aspendale, AustraliaXiaobing ZhouCollaboration for Australian Weather and Climate ResearchR. FiedlerCentre Europen de Recherche et de Formation Avance en Calcul Scientifique, Toulouse, FranceMark CollierCommonwealth Scientific and Industrial Research OrganisationYamin MaNOAA Geophysical Fluid Dynamics LaboratoryJulie NoonanCAWCR/CSIRO Marine and Atmospheric Research, Aspendale, AustraliaLauren StevensCommonwealth Scientific and Industrial Research OrganisationPeter UheCollaboration for Australian Weather and Climate ResearchHongyan ZhuNOAA Geophysical Fluid Dynamics LaboratoryStephen M. GriffiesNOAA/Geophysical Fluid Dynamics Laboratory, Princeton, NJ, USARichard S. HillMet Office Hadley Centre, Exeter, UKChris HarrisMet Office Hadley Centre, Exeter, UKKamal PuriNational Oceanic and Atmospheric Administration/Geophysical Fluid Dynamics Laboratory, Princeton, NJ, USA
2013en
ABI

Annotatsiya

The Australian Community Climate and Earth System Simulator coupled model (ACCESS-CM) has been developed at the Centre for Australian Weather and Climate Research (CAWCR), a partnership between CSIRO 1 and the Bureau of Meteorology. It is built by coupling the UK Met Office atmospheric unified model (UM), and other sub-models as required, to the ACCESS ocean model, which consists of the NOAA/GFDL 2 ocean model MOM4p1 and the LANL 3 sea-ice model CICE4.1, under the CERFACS 4 OASIS3.2-5 coupling framework. The primary goal of the ACCESS-CM development is to provide the Australian climate community with a new generation fully coupled climate model for climate research, and to participate in phase five of the Coupled Model Inter-comparison Project (CMIP5). This paper describes the ACCESS-CM framework and components, and presents the control climates from two versions of the ACCESS-CM, ACCESS1.0 and AC-CESS1.3, together with some fields from the 20 th century historical experiments, as part of model evaluation. While sharing the same ocean sea-ice model (except different setups for a few parameters), ACCESS1.0 and ACCESS1.3 differ from each other in their atmospheric and land surface components: the former is configured with the UK Met Office HadGEM2 (r1.1) atmospheric physics and the Met Office Surface Exchange Scheme land surface model version 2, and the latter with atmospheric physics similar to the UK Met Office Global Atmosphere 1.0 including modifications performed at CAWCR and the CSIRO Community Atmosphere Biosphere Land Exchange land surface model version 1.8. The global average annual mean surface air temperature across the 500-year preindustrial control integrations show a warming drift of 0.35 C in ACCESS1.0 and 0.04 C in AC-CESS1.3. The overall skills of ACCESS-CM in simulating a set of key climatic fields both globally and over Australia significantly surpass those from the preceding CSIRO Mk3.5 model delivered to the previous coupled model inter-comparison. However, ACCESS-CM, like other CMIP5 models, has deficiencies in various aspects, and these are also discussed.

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