Conservative explicit local time-stepping schemes for the shallow water equations

Thi Thao Phuong Hoang, Wei Leng, Lili Ju, Zhu Wang, Konstantin Pieper

Research output: Contribution to journalArticlepeer-review

22 Scopus citations

Abstract

In this paper we develop explicit local time-stepping (LTS) schemes with second and third order accuracy for the shallow water equations. The system is discretized in space by a C-grid staggering method, namely the TRiSK scheme adopted in MPAS-Ocean, a global ocean model with the capability of resolving multiple resolutions within a single simulation. The time integration is designed based on the strong stability preserving Runge–Kutta (SSP-RK) methods, but different time step sizes can be used in different regions of the domain through the coupling of coarse-fine time discretizations on the interface, and are only restricted by respective local CFL conditions. The proposed LTS schemes are of predictor–corrector type in which the predictors are constructed based on Taylor series expansions and SSP-RK stepping algorithms. The schemes preserve some important physical quantities in the discrete sense, such as exact conservation of the mass and potential vorticity and conservation of the total energy within time truncation errors. Moreover, they inherit the natural parallelism of the original explicit global time-stepping schemes. Extensive numerical tests are presented to illustrate the performance of the proposed algorithms.

Original languageEnglish
Pages (from-to)152-176
Number of pages25
JournalJournal of Computational Physics
Volume382
DOIs
StatePublished - Apr 1 2019
Externally publishedYes

Funding

This work is partially supported by US Department of Energy Office of Science under grants DE-SC0016540 and DE-SC0016591 and National Natural Science Foundation of China under grant 11501553.

FundersFunder number
U.S. Department of EnergyDE-SC0016591, DE-SC0016540
National Natural Science Foundation of China11501553

    Keywords

    • Finite volume
    • Local time-stepping
    • Mass conservation
    • Potential vorticity
    • Shallow water equations
    • Strong stability preserving Runge–Kutta

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