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Inverse Mean Curvature Flow


Inverse mean curvature flow evolves a hypersurface in its normal direction at speed equal to the reciprocal of the positive sum H of its principal curvatures. Here the sum is used rather than their average as in the mean curvature convention. For an embedding F with outward unit normal nu, its smooth equation is

 partial_tF=nu/H.

A level-set description uses div(del u/||del u||)=||del u|| away from critical points. Weak solutions permit jumps across regions where the smooth evolution breaks down. Huisken and Ilmanen (2001) used such weak solutions to prove the three-dimensional Riemannian Penrose inequality for a connected outermost minimal surface. For an expanding sphere in R^n, its radius satisfies r(t)=r(0)e^(t/(n-1)).


See also

Mean Curvature, Mean Curvature Flow, Minimal Surface, Riemannian Penrose Inequality

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References

Huisken, G. and Ilmanen, T. "The Inverse Mean Curvature Flow and the Riemannian Penrose Inequality." J. Diff. Geom. 59, 353-437, 2001. https://doi.org/10.4310/jdg/1090349447.

Cite this as:

Weisstein, Eric W. "Inverse Mean Curvature Flow." From MathWorld--A Wolfram Resource. https://mathworld.wolfram.com/InverseMeanCurvatureFlow.html

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