A new dynamical core for the Met Office's global and regional modelling of the atmosphere

被引:855
作者
Davies, T [1 ]
Cullen, MJP [1 ]
Malcolm, AJ [1 ]
Mawson, MH [1 ]
Staniforth, A [1 ]
White, AA [1 ]
Wood, N [1 ]
机构
[1] Met Off, Exeter, Devon, England
关键词
climate modelling; deep atmosphere; fully compressible; non-hydrostatic; NWP; predictor-corrector; semi-implicit; semi-Lagrangian;
D O I
10.1256/qj.04.101
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
A computational scheme suitable for numerical weather prediction and climate modelling over a wide range of length scales is described. Its formulation is non-hydrostatic and fully compressible, and shallow atmosphere approximations are not made. Semi-implicit, semi-Lagrangian time-integration methods are used. The scheme forms the dynamical core of the unified model used at the Met Office for all its operational numerical weather prediction and in its climate studies.
引用
收藏
页码:1759 / 1782
页数:24
相关论文
共 80 条
[1]  
Arakawa A, 1996, MON WEATHER REV, V124, P511, DOI 10.1175/1520-0493(1996)124<0511:VDOTPE>2.0.CO
[2]  
2
[3]  
Arakawa A., 1977, Methods of Computational Physics, V17, P173, DOI [10.1016/B978-0-12-460817-7.50009-4, DOI 10.1016/B978-0-12-460817-7.50009-4]
[4]  
BARKSTROM B, 1989, B AM METEOROL SOC, V70, P1254, DOI 10.1175/1520-0477(1989)070<1254:ERBEAA>2.0.CO
[5]  
2
[6]  
BATES JR, 1993, MON WEATHER REV, V121, P244, DOI 10.1175/1520-0493(1993)121<0244:AGMAMU>2.0.CO
[7]  
2
[8]  
BERMEJO R, 1992, MON WEATHER REV, V120, P2622, DOI 10.1175/1520-0493(1992)120<2622:TCOSLA>2.0.CO
[9]  
2
[10]  
CLARK PA, 2002, IN PRESS Q J R METEO