Development and evaluation of an Earth-System model-HadGEM2

被引:1120
作者
Collins, W. J. [1 ]
Bellouin, N. [1 ]
Doutriaux-Boucher, M. [1 ]
Gedney, N. [1 ]
Halloran, P. [1 ]
Hinton, T. [1 ]
Hughes, J. [1 ]
Jones, C. D. [1 ]
Joshi, M. [2 ]
Liddicoat, S. [1 ]
Martin, G. [1 ]
O'Connor, F. [1 ]
Rae, J. [1 ]
Senior, C. [1 ]
Sitch, S. [3 ]
Totterdell, I. [1 ]
Wiltshire, A. [1 ]
Woodward, S. [1 ]
机构
[1] Met Off Hadley Ctr, Exeter, Devon, England
[2] Univ Reading, Dept Meteorol, Climate Directorate, Natl Ctr Atmospher Sci, Reading, Berks, England
[3] Univ Leeds, Sch Geog, Leeds LS2 9JT, W Yorkshire, England
关键词
ENVIRONMENT SIMULATOR JULES; NET PRIMARY PRODUCTIVITY; CARBON-CYCLE FEEDBACKS; FRESH-WATER DISCHARGE; CLIMATE MODEL; METHANE EMISSIONS; DIMETHYL SULFIDE; PLANT GEOGRAPHY; SOIL-MOISTURE; OCEAN;
D O I
10.5194/gmd-4-1051-2011
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
We describe here the development and evaluation of an Earth system model suitable for centennial-scale climate prediction. The principal new components added to the physical climate model are the terrestrial and ocean ecosystems and gas-phase tropospheric chemistry, along with their coupled interactions. The individual Earth system components are described briefly and the relevant interactions between the components are explained. Because the multiple interactions could lead to unstable feedbacks, we go through a careful process of model spin up to ensure that all components are stable and the interactions balanced. This spun-up configuration is evaluated against observed data for the Earth system components and is generally found to perform very satisfactorily. The reason for the evaluation phase is that the model is to be used for the core climate simulations carried out by the Met Office Hadley Centre for the Coupled Model Intercomparison Project (CMIP5), so it is essential that addition of the extra complexity does not detract substantially from its climate performance. Localised changes in some specific meteorological variables can be identified, but the impacts on the overall simulation of present day climate are slight. This model is proving valuable both for climate predictions, and for investigating the strengths of biogeochemical feedbacks.
引用
收藏
页码:1051 / 1075
页数:25
相关论文
共 98 条
  • [1] [Anonymous], THESIS U DURHAM DURH
  • [2] [Anonymous], 73 HADL CTR
  • [3] [Anonymous], 2001, DESCRIPTION TRIFFID
  • [4] [Anonymous], GEOSCI MODEL D UNPUB
  • [5] [Anonymous], NDP018 CARB DIOX INF
  • [6] COHERENCE BETWEEN SEASONAL CYCLES OF DIMETHYL SULFIDE, METHANESULFONATE AND SULFATE IN MARINE AIR
    AYERS, GP
    IVEY, JP
    GILLETT, RW
    [J]. NATURE, 1991, 349 (6308) : 404 - 406
  • [7] Bagnold R., 1941, PHYS BLOWN SAND DESE
  • [8] Reevaluation of Mineral aerosol radiative forcings suggests a better agreement with satellite and AERONET data
    Balkanski, Y.
    Schulz, M.
    Claquin, T.
    Guibert, S.
    [J]. ATMOSPHERIC CHEMISTRY AND PHYSICS, 2007, 7 : 81 - 95
  • [9] Aerosol forcing in the Climate Model Intercomparison Project (CMIP5) simulations by HadGEM2-ES and the role of ammonium nitrate
    Bellouin, Nicolas
    Rae, Jamie
    Jones, Andy
    Johnson, Colin
    Haywood, Jim
    Boucher, Olivier
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2011, 116
  • [10] The Joint UK Land Environment Simulator (JULES), model description - Part 1: Energy and water fluxes
    Best, M. J.
    Pryor, M.
    Clark, D. B.
    Rooney, G. G.
    Essery, R. L. H.
    Menard, C. B.
    Edwards, J. M.
    Hendry, M. A.
    Porson, A.
    Gedney, N.
    Mercado, L. M.
    Sitch, S.
    Blyth, E.
    Boucher, O.
    Cox, P. M.
    Grimmond, C. S. B.
    Harding, R. J.
    [J]. GEOSCIENTIFIC MODEL DEVELOPMENT, 2011, 4 (03) : 677 - 699