Huang, P., C. G. Chen, X. L. Li, X. S. Shen, and F. Xiao, 2022: An adaptive nonhydrostatic atmospheric dynamical core using multi-moment constrained finite volume method. Adv. Atmos. Sci., 39(3), 487−501, https://doi.org/10.1007/s00376-021-1185-9.
Citation: Huang, P., C. G. Chen, X. L. Li, X. S. Shen, and F. Xiao, 2022: An adaptive nonhydrostatic atmospheric dynamical core using multi-moment constrained finite volume method. Adv. Atmos. Sci., 39(3), 487−501, https://doi.org/10.1007/s00376-021-1185-9.

An Adaptive Nonhydrostatic Atmospheric Dynamical Core Using a Multi-Moment Constrained Finite Volume Method

  • An adaptive 2D nonhydrostatic dynamical core is proposed by using the multi-moment constrained finite-volume (MCV) scheme and the Berger-Oliger adaptive mesh refinement (AMR) algorithm. The MCV scheme takes several point-wise values within each computational cell as the predicted variables to build high-order schemes based on single-cell reconstruction. Two types of moments, such as the volume-integrated average (VIA) and point value (PV), are defined as constraint conditions to derive the updating formulations of the unknowns, and the constraint condition on VIA guarantees the rigorous conservation of the proposed model. In this study, the MCV scheme is implemented on a height-based, terrain-following grid with variable resolution to solve the nonhydrostatic governing equations of atmospheric dynamics. The AMR grid of Berger-Oliger consists of several groups of blocks with different resolutions, where the MCV model developed on a fixed structured mesh can be used directly. Numerical formulations are designed to implement the coarse-fine interpolation and the flux correction for properly exchanging the solution information among different blocks. Widely used benchmark tests are carried out to evaluate the proposed model. The numerical experiments on uniform and AMR grids indicate that the adaptive model has promising potential for improving computational efficiency without losing accuracy.
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