Abstract
The classical one-phase Stefan problem describes the temperature distribution in a homogeneous medium undergoing a phase transition, such as ice melting to water. This is accomplished by solving the heat equation on a time-dependent domain whose boundary is transported by the normal derivative of the temperature along the evolving and a priori unknown free-boundary. We establish a global-in-time stability result for nearly spherical geometries and small temperatures, using a novel hybrid methodology, which combines energy estimates, decay estimates, and Hopf-type inequalities.
Original language | English |
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Publisher | arXiv |
Pages | N/A |
Number of pages | 50 |
Volume | N/A |
Publication status | Published - 6 Dec 2012 |
Keywords
- math.AP
- 35R35, 35B65, 35K05, 80A22