Approximating Gradient Flows on Surfaces via MM + CPM
[Ginder, Elliott; Svadlenka, Karel; and Muramatsu, Takuma (2024). Approximation and Application of Minimizing Movements for Surface PDE. arXiv preprint arXiv:2409.03139. See Section 3.2, pp. 7–9. Available at https://arxiv.org/abs/2409.03139.] MM - Minimizing Movements
CPM - Closest Point Method
(e.g. surfaces of sphere and torus are boundary-less surfaces)
bounded domain of Euclidean space
with suitable boundary (e.g. Lipschitz boundary)
u/uS gives each point of the whole domain / surface scalar value in some time t∈[0,T] heat dissipation on flat 2D surface wave propagation through flat 2D surface (red - positive displacement, blue - negative)
on Euclidean domain Ω ΔS - Laplace-Beltrami operator (surface version of Laplacian operator Δ) Dirichlet Boundary Conditions
"all the values on the boundary of our domain are fixed"
we need to define boundary values for bounded domain
extremum of the functional (we are looking for u with minimal evaluation) Dirichlet energy functional
spatial term in gradient flows is always Dirichlet energy
approximating gradient flow by iteratively minimizing functionals
F is functional - accepts function u and returns its scalar evaluation in MM, for next step n+1 we are searching for u that is of lowest such evaluation it would be costly and tricky to numerically approximate field uS across only the surface (we would need to create mesh etc.) therefore for a given n-dimensional arbitrary surface
we create a smooth extension, by extending the values of uS in the direction of normal vectors coming from the surface for each point that belongs to a normal vector, we give same value as the vector's origin which also is its closest point
(if normal vectors intersect with each other, we can always make them shorter such that they do not intersect)
we therefore construct functionals for our band ΩS around the surface S notice that the new u doesn't return the same values for points lying along surface normals in ΩS but with each step CS maps x to its nearest surface point for previous u's now we take Gateaux derivative of the functional at =0 to yield Euler-Lagrange equation = implicit time-step scheme for the time-discrete approximation showing that it works with CS - Closest Point Method infinitely differentiable on ΩS with compact support in ΩS when set to 0, allows us to find such u at which F attains extremum (is stationary) similarly as with classical derivative set to 0, we can find all x in which the f attains extremum total source flow in the volume = net flow through the surface (its boundary)
dV is often abbreviated as dx and both are practically interchangeable (we did projection of rate of change ∇u onto outward normal vector ν) supp(ϕ) is compact subset of ΩS compact ⇒ closed (definite integral ⇒ no C constant) Fundamental Lemma of the Calculus of Variations
Implicit approximations to the surface PDEs via MM + CPM ■