A test case for the inviscid shallow-water equations on the sphere

被引:11
|
作者
Scott, R. K. [1 ]
Harris, L. M. [2 ]
Polvani, L. M. [3 ,4 ]
机构
[1] Univ St Andrews, Sch Math & Stat, St Andrews KY16 9SS, Fife, Scotland
[2] Princeton Univ, NOAA, Geophys Fluid Dynam Lab, Princeton, NJ 08544 USA
[3] Columbia Univ, Dept Appl Phys & Appl Math, New York, NY USA
[4] Columbia Univ, Dept Earth & Environm Sci, New York, NY USA
基金
美国国家科学基金会;
关键词
shallow-water flow; numerical modelling; potential vorticity; DYNAMICAL CORE;
D O I
10.1002/qj.2667
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
A numerically converged solution to the inviscid global shallow-water equations for a predefined time interval is documented to provide a convenient benchmark for model validation. The solution is based on the same initial conditions as a previously documented solution for the viscous equations. The solution is computed using two independent numerical schemes, one a pseudospectral scheme based on an expansion in spherical harmonics and the other a finite-volume scheme on a cubed-sphere grid. Flow fields and various integral norms are documented to facilitate model comparison and validation. Attention is drawn to the utility of the potential vorticity supremum as a convenient and sensitive test of numerical convergence, in which the exact value is known a priori over the entire time interval.
引用
收藏
页码:488 / 495
页数:8
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