The CSIRO Mk3L climate system model version 1.0-Part 1: Description and evaluation

被引:93
作者
Phipps, S. J. [1 ,2 ,3 ,4 ]
Rotstayn, L. D. [5 ]
Gordon, H. B. [5 ]
Roberts, J. L. [2 ,3 ,6 ]
Hirst, A. C. [5 ]
Budd, W. F. [1 ,2 ,3 ]
机构
[1] Univ Tasmania, Inst Antarctic & So Ocean Studies, Hobart, Tas 7001, Australia
[2] Antarctic Climate & Ecosyst CRC, Hobart, Tas, Australia
[3] Tasmanian Partnership Adv Comp, Hobart, Tas, Australia
[4] Univ New S Wales, Climate Change Res Ctr, Sydney, NSW 2052, Australia
[5] Ctr Australian Weather & Climate Res, Aspendale, Vic, Australia
[6] Australian Antarctic Div, Kingston, Tas, Australia
关键词
GENERAL-CIRCULATION MODEL; ANTARCTIC CIRCUMPOLAR CURRENT; NINO-SOUTHERN-OSCILLATION; PHYSICALLY-BASED SCHEME; LARGE-SCALE MODELS; EL-NINO; STRATIFORM CLOUDS; COUPLED MODEL; SEA-ICE; ATMOSPHERE MODELS;
D O I
10.5194/gmd-4-483-2011
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The CSIRO Mk3L climate system model is a coupled general circulation model, designed primarily for millennial-scale climate simulations and palaeoclimate research. Mk3L includes components which describe the atmosphere, ocean, sea ice and land surface, and combines computational efficiency with a stable and realistic control climatology. This paper describes the model physics and software, analyses the control climatology, and evaluates the ability of the model to simulate the modern climate. Mk3L incorporates a spectral atmospheric general circulation model, a z-coordinate ocean general circulation model, a dynamic-thermodynamic sea ice model and a land surface scheme with static vegetation. The source code is highly portable, and has no dependence upon proprietary software. The model distribution is freely available to the research community. A 1000-yr climate simulation can be completed in around one-and-a-half months on a typical desktop computer, with greater throughput being possible on high-performance computing facilities. Mk3L produces realistic simulations of the larger-scale features of the modern climate, although with some biases on the regional scale. The model also produces reasonable representations of the leading modes of internal climate variability in both the tropics and extratropics. The control state of the model exhibits a high degree of stability, with only a weak cooling trend on millennial timescales. Ongoing development work aims to improve the model climatology and transform Mk3L into a comprehensive earth system model.
引用
收藏
页码:483 / 509
页数:27
相关论文
共 145 条
[1]   Simulation of the El Nino Southern Oscillation: Results from the Coupled Model Intercomparison Project [J].
AchutaRao, K ;
Sperber, KR .
CLIMATE DYNAMICS, 2002, 19 (3-4) :191-209
[2]  
[Anonymous], R12771ARPA RAND CORP
[3]  
[Anonymous], 2002, 60 CSIRO ATM RES
[4]  
[Anonymous], 23 CSIRO DIV ATM RES
[5]  
[Anonymous], 013 CSIRO MAR ATM RE
[6]  
[Anonymous], R12761ARPA RAND CORP
[7]  
[Anonymous], 3 ANT CLIM EC COOP R
[8]  
Arakawa A., 1977, Methods in Computational Physics: Advances in Research and Applications, P173, DOI [10.1016/B978-0-12-460817-7.50009-4, DOI 10.1016/B978-0-12-460817-7.50009-4]
[9]  
BARKSTROM BR, 1984, B AM METEOROL SOC, V65, P1170, DOI 10.1175/1520-0477(1984)065<1170:TERBE>2.0.CO
[10]  
2