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A Characteristic Mapping Method with Source Terms: Applications to Ideal Magnetohydrodynamics

Xi-Yuan Yin, Philipp Krah, Jean-Christophe Nave, Kai Schneider

Abstract

This work introduces a generalized characteristic mapping method designed to handle non-linear advection with source terms. The semi-Lagrangian approach advances the flow map, incorporating the source term via the Duhamel integral. We derive a recursive formula for the time decomposition of the map and the source term integral, enhancing computational efficiency. Benchmark computations are presented for a test case with an exact solution and for two-dimensional ideal incompressible magnetohydrodynamics (MHD). Results demonstrate third-order accuracy in both space and time. The submap decomposition method achieves exceptionally high resolution, as illustrated by zooming into fine-scale current sheets. An error estimate is performed and suggests third order convergence in space and time.

A Characteristic Mapping Method with Source Terms: Applications to Ideal Magnetohydrodynamics

Abstract

This work introduces a generalized characteristic mapping method designed to handle non-linear advection with source terms. The semi-Lagrangian approach advances the flow map, incorporating the source term via the Duhamel integral. We derive a recursive formula for the time decomposition of the map and the source term integral, enhancing computational efficiency. Benchmark computations are presented for a test case with an exact solution and for two-dimensional ideal incompressible magnetohydrodynamics (MHD). Results demonstrate third-order accuracy in both space and time. The submap decomposition method achieves exceptionally high resolution, as illustrated by zooming into fine-scale current sheets. An error estimate is performed and suggests third order convergence in space and time.

Paper Structure

This paper contains 13 sections, 1 theorem, 45 equations, 8 figures, 3 tables, 1 algorithm.

Key Result

Proposition 1

The CMM for the ideal MHD equations in two dimensions using Hermite cubic spatial interpolation and $3^{rd}$ order Lagrange time extrapolation and Runge-Kutta 4 integration has a numerical error of order $\mathcal{O}(N^{-3} + {\Delta t}^{3} ) + o(l_1 + l_2)$ where $h$ and ${\Delta t}$ are the spatia

Figures (8)

  • Figure 1: Linear advection swirl test case source term analysis. Shown is the solution $\theta({\bm x}, t)$, subintegrals $F_{[t,\tau_i]}$, source term $f({\bm x}, t)$ and corresponding Fourier spectra (from left to right), for $t=0.4, 1, 1.6$ and 2 (from top to bottom).
  • Figure 2: Convergence in space ($\Delta_x$) and time ($\Delta_t$) for the swirl test case, compared to the analytical reference solution.
  • Figure 3: Time evolution of the vorticity $\omega$ (left) and current density $j$ (right) from top to bottom $t=0.1,0.4,0.9$ for OT.
  • Figure 4: Zoom with center $(x,y)=(L/2,L/2)$ of the current density $j$ at time $t=4.0$ for OT. The zoom factor between each image is 2.
  • Figure 5: Convergence in space (a) and time (b) for OT. Shown is the relative error with respect to the reference solution in the $L^\infty$ norm.
  • ...and 3 more figures

Theorems & Definitions (1)

  • Proposition 1