Skip to content
DraconiticResearch
Search Sources API
203,234 studies31 sourcesUpdated 32 min ago
PreprintarXiv licencearXiv

A Second-Order Semi-Implicit Projection Time-Stepping Scheme for the Shallow-Water Equations on the Sphere Using Compatible Finite Elements

Abstract

We propose a second-order, semi-implicit time-stepping scheme for the shallow-water equations on the sphere discretised with compatible finite elements. The scheme splits the advection operator from the wave operator, applying a DG-upwind SSPRK3 method to the advection part and an H(div)-conforming implicit discretisation to the wave part, solved efficiently via hybridisation. The scheme follows a three-step symmetric splitting: an explicit half-step, a full advection step, and an implicit half-step that simultaneously projects the velocity back into the H(div) space. This symmetry guarantees global second-order accuracy and confines the stability restriction to the CFL condition of the advection step alone. The time-step can therefore be extended beyond this limit by subcycling the advection step without additional implicit solves. The method is implemented in Firedrake and validated against a standard suite of spherical shallow-water benchmarks, demonstrating stable results for Courant numbers up to 1 (with two advection subcycles) with second-order finite elements, second-order convergence, and good parallel scaling.

Related

  1. A thermodynamically compatible semi-implicit finite volume scheme for the compressible Euler equations
    Michael Dumbser, Gabriella Puppo, Sara Rinaldi +1
    HALPreprintCC BY-NC-SA 4.0Full textNumerical analysis & scientific computingHALarXiv
  2. Are implicit schemes needed in adaptive time stepping for PDEs?
    Mikhail A. Botchev
    arXivPreprintarXiv licenceFull textNumerical analysis & scientific computingComputational physicsarXiv
  3. Preconditioning for the time-dependent Stokes equations: stage-weighted Radau IIA and weighted discontinuous Galerkin time-stepping
    Esteban Henríquez, Jeonghun J. Lee, Sander Rhebergen
    arXivPreprintCC BY 4.0Full textNumerical analysis & scientific computingarXiv
  4. Structure-preserving operator splitting for 2.5D ideal MHD with an entropy-stable DGSEM and exactly divergence-free compatible finite elements
    Siyuan Fan, Guosheng Fu
    arXivPreprintarXiv licenceFull textNumerical analysis & scientific computingarXiv
  5. Domain splitting with localized implicit prediction for wave equations
    Tim Buchholz, Roland Maier
    arXivPreprintarXiv licenceFull textNumerical analysis & scientific computingarXiv
BibTeX
@misc{kowalczyk2026secondorder,
  title = {{A Second-Order Semi-Implicit Projection Time-Stepping Scheme for the Shallow-Water Equations on the Sphere Using Compatible Finite Elements}},
  author = {Karina Kowalczyk and Colin Cotter},
  howpublished = {arXiv},
  year = {2026},
  month = nov,
  doi = {10.48550/arxiv.2611.08169},
  eprint = {2611.08169},
  archivePrefix = {arXiv},
  url = {https://arxiv.org/abs/2611.08169},
}
RIS
TY  - UNPB
TI  - A Second-Order Semi-Implicit Projection Time-Stepping Scheme for the Shallow-Water Equations on the Sphere Using Compatible Finite Elements
AU  - Karina Kowalczyk
AU  - Colin Cotter
PY  - 2026
DA  - 2026/11/05
PB  - arXiv
DO  - 10.48550/arxiv.2611.08169
UR  - https://arxiv.org/abs/2611.08169
AB  - We propose a second-order, semi-implicit time-stepping scheme for the shallow-water equations on the sphere discretised with compatible finite elements. The scheme splits the advection operator from the wave operator, applying a DG-upwind SSPRK3 method to the advection part and an H(div)-conforming implicit discretisation to the wave part, solved efficiently via hybridisation. The scheme follows a three-step symmetric splitting: an explicit half-step, a full advection step, and an implicit half-step that simultaneously projects the velocity back into the H(div) space. This symmetry guarantees global second-order accuracy and confines the stability restriction to the CFL condition of the advection step alone. The time-step can therefore be extended beyond this limit by subcycling the advection step without additional implicit solves. The method is implemented in Firedrake and validated against a standard suite of spherical shallow-water benchmarks, demonstrating stable results for Courant numbers up to 1 (with two advection subcycles) with second-order finite elements, second-order convergence, and good parallel scaling.
ER  -