A Hopf–Lax formula for the time evolution of the level-set equation and a new approach to shape sensitivity analysis
Interfaces and free boundaries, Tome 18 (2016) no. 3, pp. 317-353
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The level-set method is used in many different applications to describe the propagation of shapes and domains. When scalar speed fields are used to encode the desired shape evolution, this leads to the classical level-set equation. We present a concise Hopf–Lax representation formula that can be used to characterise the evolved domains at arbitrary times. This result is also applicable for the case of speed fields without a fixed sign, even though the level-set equation has a non-convex Hamiltonian in these situations. The representation formula is based on the same idea that underpins the Fast-Marching Method, and it provides a strong theoretical justification for a generalised Composite Fast-Marching method.
Classification :
49-XX
Mots-clés : Level-set method, shape optimisation, Hopf–Lax formula, viscosity solutions, nonfattening, shape-sensitivity analysis
Mots-clés : Level-set method, shape optimisation, Hopf–Lax formula, viscosity solutions, nonfattening, shape-sensitivity analysis
Affiliations des auteurs :
Daniel Kraft  1
Daniel Kraft. A Hopf–Lax formula for the time evolution of the level-set equation and a new approach to shape sensitivity analysis. Interfaces and free boundaries, Tome 18 (2016) no. 3, pp. 317-353. doi: 10.4171/ifb/366
@article{10_4171_ifb_366,
author = {Daniel Kraft},
title = {A {Hopf{\textendash}Lax} formula for the time evolution of the level-set equation and a new approach to shape sensitivity analysis},
journal = {Interfaces and free boundaries},
pages = {317--353},
year = {2016},
volume = {18},
number = {3},
doi = {10.4171/ifb/366},
url = {http://geodesic.mathdoc.fr/articles/10.4171/ifb/366/}
}
TY - JOUR AU - Daniel Kraft TI - A Hopf–Lax formula for the time evolution of the level-set equation and a new approach to shape sensitivity analysis JO - Interfaces and free boundaries PY - 2016 SP - 317 EP - 353 VL - 18 IS - 3 UR - http://geodesic.mathdoc.fr/articles/10.4171/ifb/366/ DO - 10.4171/ifb/366 ID - 10_4171_ifb_366 ER -
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