2021
DOI: 10.48550/arxiv.2108.01244
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Level-set forced mean curvature flow with the Neumann boundary condition

Abstract: Here, we study a level-set forced mean curvature flow with the homogeneous Neumann boundary condition. We first show that the solution is Lipschitz in time and locally Lipschitz in space. Then, under an additional condition on the forcing term, we prove that the solution is globally Lipschitz. We obtain the large time behavior of the solution in this setting and study the large time profile in some specific situations. Finally, we give two examples demonstrating that the additional condition on the forcing ter… Show more

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Cited by 1 publication
(11 citation statements)
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“…Note that the illustration justifies the necessity of a nonzero force term in order to have a global gradient estimate on a nonconvex domain. In this context, the results on the forced mean curvature flow with the right angle condition have been obtained [23] recently, which explains the effect of the constraints by the forcing term and by the geometry of the boundary. However, there are no results on the forced mean curvature flow and the forced mean curvature equation with more general boundary conditions on a general bounded domain, for neither the graph case nor the level-set case.…”
Section: Introductionmentioning
confidence: 79%
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“…Note that the illustration justifies the necessity of a nonzero force term in order to have a global gradient estimate on a nonconvex domain. In this context, the results on the forced mean curvature flow with the right angle condition have been obtained [23] recently, which explains the effect of the constraints by the forcing term and by the geometry of the boundary. However, there are no results on the forced mean curvature flow and the forced mean curvature equation with more general boundary conditions on a general bounded domain, for neither the graph case nor the level-set case.…”
Section: Introductionmentioning
confidence: 79%
“…The novelty of this paper is threefold; first of all, the multiplier method in [23] can be combined with the method in [40] in order to get a priori gradient estimates of (1.7) uniform in η > 0. The combination of the methods allows us to handle the difficulties coming from the nonconvexity of Ω, a forcing term c, a transport term f , a nonzero boundary condition with φ ≡ 0 at the same time.…”
Section: Introductionmentioning
confidence: 99%
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