Journal cover Journal topic
Geoscientific Model Development An interactive open-access journal of the European Geosciences Union
Geosci. Model Dev., 6, 141-160, 2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
Development and technical paper
31 Jan 2013
Optimising the FAMOUS climate model: inclusion of global carbon cycling
J. H. T. Williams1, R. S. Smith2, P. J. Valdes1, B. B. B. Booth3, and A. Osprey2 1BRIDGE, School of Geographical Sciences, University of Bristol, Bristol, BS8 1SS, UK
2Department of Meteorology, University of Reading, Reading, RG6 6BB, UK
3Met Office Hadley Centre, FitzRoy Road, Exeter, EX1 3PB, UK
Abstract. FAMOUS fills an important role in the hierarchy of climate models, both explicitly resolving atmospheric and oceanic dynamics yet being sufficiently computationally efficient that either very long simulations or large ensembles are possible. An improved set of carbon cycle parameters for this model has been found using a perturbed physics ensemble technique. This is an important step towards building the "Earth System" modelling capability of FAMOUS, which is a reduced resolution, and hence faster running, version of the Hadley Centre Climate model, HadCM3. Two separate 100 member perturbed parameter ensembles were performed; one for the land surface and one for the ocean. The land surface scheme was tested against present-day and past representations of vegetation and the ocean ensemble was tested against observations of nitrate. An advantage of using a relatively fast climate model is that a large number of simulations can be run and hence the model parameter space (a large source of climate model uncertainty) can be more thoroughly sampled. This has the associated benefit of being able to assess the sensitivity of model results to changes in each parameter. The climatologies of surface and tropospheric air temperature and precipitation are improved relative to previous versions of FAMOUS. The improved representation of upper atmosphere temperatures is driven by improved ozone concentrations near the tropopause and better upper level winds.

Citation: Williams, J. H. T., Smith, R. S., Valdes, P. J., Booth, B. B. B., and Osprey, A.: Optimising the FAMOUS climate model: inclusion of global carbon cycling, Geosci. Model Dev., 6, 141-160,, 2013.
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