A MULTIGRID SOLVER FOR SEMIIMPLICIT GLOBAL SHALLOW-WATER MODELS

被引:9
|
作者
BARROS, SRM
DEE, DP
DICKSTEIN, F
机构
[1] NYU,COURANT INST MATH SCI,NEW YORK,NY 10012
[2] PONTIFICIA UNIV CATOLICA RIO DE JANEIRO,DEPT MATH,BR-20000 RIO DE JANEIRO,RJ,BRAZIL
[3] UNIV FED RIO DE JANEIRO,CTR CIENCIAS SAUDE,INST MATEMAT,DEPT APPL MATH,RIO DE JANEIRO,RJ,BRAZIL
关键词
D O I
10.1080/07055900.1990.9649366
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The multigrid principle produces fast solversfor systems of algebraic equations, particularly those that arise from discretizing elliptic boundary‐value problems. A multigrid solver is developed for the discretized two‐dimensional elliptic equation on the sphere that arises from a semi‐implicit time discretization of the global shallow‐water equations. We experiment with different formulations of the semi‐implicit scheme that result in variable‐coefficient Helmholtz‐type equations for which no fast direct solversare available. The efficiency of the multigrid solver is optimal, in the sense that the total operation count is proportional to the number of unknowns. Numerical experiments using initial data derived from actual 300‐mb height and wind velocity fields indicate that our semi‐implicit global shallow‐water model has very good accuracy and stability properties. © Taylor & Francis Group, LLC.
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页码:24 / 47
页数:24
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