中国物理B ›› 2001, Vol. 10 ›› Issue (12): 1103-1105.doi: 10.1088/1009-1963/10/12/303

• GENERAL • 上一篇    下一篇

LATTICE BOLTZMANN EQUATION MODEL IN THE CORIOLIS FIELD

冯士德, 毛江玉, 张琼   

  1. State Key Laboratory of Numerical Modelling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
  • 收稿日期:2001-06-23 修回日期:2001-09-05 出版日期:2005-06-12 发布日期:2005-06-12
  • 基金资助:
    Project supported by the National Natural Science Foundation of China (Grant Nos. 49823002, 40005005, 7-200053, 4-200060), and by the State Key Development Programme for Basic Research of China (Grant No. G1998040904).

LATTICE BOLTZMANN EQUATION MODEL IN THE CORIOLIS FIELD

Feng Shi-de (冯士德), Mao Jiang-yu (毛江玉), Zhang Qiong (张琼)   

  1. State Key Laboratory of Numerical Modelling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
  • Received:2001-06-23 Revised:2001-09-05 Online:2005-06-12 Published:2005-06-12
  • Supported by:
    Project supported by the National Natural Science Foundation of China (Grant Nos. 49823002, 40005005, 7-200053, 4-200060), and by the State Key Development Programme for Basic Research of China (Grant No. G1998040904).

PDF (PC)

514

赞

摘要： In a large-scale field of rotational fluid, various unintelligible and surprising dynamic phenomena are produced due to the effect of the Coriolis force. The lattice Boltzmann equation (LBE) model in the Coriolis field is developed based on previous works.[1-4] Geophysical fluid dynamics equations are derived from the model. Numerical simulations have been made on an ideal atmospheric circulation of the Northern Hemisphere by using the model and they reproduce the Rossby wave motion well. Hence the applicability of the model is verified in both theory and experiment.

Abstract: In a large-scale field of rotational fluid, various unintelligible and surprising dynamic phenomena are produced due to the effect of the Coriolis force. The lattice Boltzmann equation (LBE) model in the Coriolis field is developed based on previous works.[1-4] Geophysical fluid dynamics equations are derived from the model. Numerical simulations have been made on an ideal atmospheric circulation of the Northern Hemisphere by using the model and they reproduce the Rossby wave motion well. Hence the applicability of the model is verified in both theory and experiment.

Key words: distribution function, Coriolis force, geophysical hydrodynamic equations

中图分类号:  (Transport processes)

  • 05.60.-k
47.85.Dh (Hydrodynamics, hydraulics, hydrostatics)