EGU2020-4005
https://doi.org/10.5194/egusphere-egu2020-4005
EGU General Assembly 2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

MPDATA method for non–uniform mesh

Xinpeng Yuan
Xinpeng Yuan
  • China Meteorological Administration, Chinese Academy of Meteorological Sciences, China (yuanxp@cma.gov.cn)

 

MPDATA method for non–uniform mesh

 

Xinpeng Yuan

State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences,China 

Meteorological Administration, Beijing 100081, China 

 

Keyword: Atmospheric dynamics, MPDATA, non–uniform mesh, precision

Abstract: MPDATA[1,2](multidimensional positive definite advection transport algorithm) is proposed by Piotr K. Smolarkiewicz in 1983. This method is used to efficiently solve the advection transport problem of non-negative thermodynamic variables (such as liquid water or water vapor) in the atmospheric dynamics model. This method has been proved to be an effective numerical solution to the advection transport problem for uniform meshes. However, since there is no uniform mesh division on the sphere, the traditional MPDATA method is faced with the incompatibility problem for the non-uniform and quasi-uniform meshing of the sphere, resulting in the numerical algorithm failing to reach the designed second-order accuracy. Firstly, this paper analyzes the insufficiency of traditional MPDATA methods for non-uniform grids. That is, the incompatibility of the first-order numerical scheme and the approximation of boundary derivative.Then the MPDATA method suitable for non-uniform grid is proposed. According to the characteristics of non-uniform grid and the characteristics of well-balance[3] central grid point algorithm, the MPDATA method suitable for 1-d and 2-d complex grid structure is designed. The consistency and positivity of the algorithm are proved by mathematical analysis. Finally, the theoretical proof is verified by numerical simulation.

 

Reference

[1] Smolarkiewicz P. A Simple Positive Definite Advection Scheme with Small Implicit Diffusion[J]. Monthly Weather Review. 1983.

[2] Smolarkiewicz P K, Szmelter J. MPDATA: An edge-based unstructured-grid formulation[J]. Journal of Computational Physics. 2005, 206(2): 624-649.

[3] Kurganov A, Levy D. Central-Upwind Schemes for the Saint-Venant System[J]. ESAIM: Mathematical Modelling and Numerical Analysis. 2002, 36(3): 397-425.

 

How to cite: Yuan, X.: MPDATA method for non–uniform mesh, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-4005, https://doi.org/10.5194/egusphere-egu2020-4005, 2020

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