TY - JOUR
T1 - Implementation of a high-order combined compact difference scheme in problems of thermally driven convection and dynamo in rotating spherical shells
AU - Takahashi, Futoshi
N1 - Funding Information:
We thank two anonymous referees for helpful comments. Some numerical simulations were carried out on the Earth Simulator at the Earth Simulator Center and TSUBAME-2 at GSIC, Tokyo Institute of Technology. FT is supported by the Japan Society for the Promotion of Science under the grant-in-aid for young scientists (B) No. 22740292.
PY - 2012/6
Y1 - 2012/6
N2 - We present an improved solution method for modeling thermally driven convection and dynamo in a rotating spherical shell. In this method, we introduce a high-order three-point combined compact difference scheme (CCDS) on non-uniform grid points in radius, while spherical harmonic expansion is conventionally performed in the angular direction. The governing equations in the spectral form are time-stepped together with the implicit CCDS up to the second derivative. To improve stability of the scheme, a boundary closure scheme is developed on non-uniform mesh. Numerical comparison with a published benchmark solution at moderate Ekman and Rayleigh numbers demonstrates that accuracy and convergence of the CCDS is fairly good and superior to the existing finite difference scheme using more stencil. With this scheme, we could more accurately solve problems of convection and also dynamo action in planetary core with less grid points.
AB - We present an improved solution method for modeling thermally driven convection and dynamo in a rotating spherical shell. In this method, we introduce a high-order three-point combined compact difference scheme (CCDS) on non-uniform grid points in radius, while spherical harmonic expansion is conventionally performed in the angular direction. The governing equations in the spectral form are time-stepped together with the implicit CCDS up to the second derivative. To improve stability of the scheme, a boundary closure scheme is developed on non-uniform mesh. Numerical comparison with a published benchmark solution at moderate Ekman and Rayleigh numbers demonstrates that accuracy and convergence of the CCDS is fairly good and superior to the existing finite difference scheme using more stencil. With this scheme, we could more accurately solve problems of convection and also dynamo action in planetary core with less grid points.
UR - http://www.scopus.com/inward/record.url?scp=84860892421&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=84860892421&partnerID=8YFLogxK
U2 - 10.1080/03091929.2011.565337
DO - 10.1080/03091929.2011.565337
M3 - Article
AN - SCOPUS:84860892421
SN - 0309-1929
VL - 106
SP - 231
EP - 249
JO - Geophysical and Astrophysical Fluid Dynamics
JF - Geophysical and Astrophysical Fluid Dynamics
IS - 3
ER -