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      Lake Toba volcano magma chamber imaged by ambient seismic noise tomography : LAKE TOBA VOLCANO MAGMA CHAMBER

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          Seismic velocity structure and composition of the continental crust: A global view

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            Processing seismic ambient noise data to obtain reliable broad-band surface wave dispersion measurements

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              A fast marching level set method for monotonically advancing fronts.

              A fast marching level set method is presented for monotonically advancing fronts, which leads to an extremely fast scheme for solving the Eikonal equation. Level set methods are numerical techniques for computing the position of propagating fronts. They rely on an initial value partial differential equation for a propagating level set function and use techniques borrowed from hyperbolic conservation laws. Topological changes, corner and cusp development, and accurate determination of geometric properties such as curvature and normal direction are naturally obtained in this setting. This paper describes a particular case of such methods for interfaces whose speed depends only on local position. The technique works by coupling work on entropy conditions for interface motion, the theory of viscosity solutions for Hamilton-Jacobi equations, and fast adaptive narrow band level set methods. The technique is applicable to a variety of problems, including shape-from-shading problems, lithographic development calculations in microchip manufacturing, and arrival time problems in control theory.
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                Author and article information

                Journal
                Geophysical Research Letters
                Geophys. Res. Lett.
                American Geophysical Union (AGU)
                00948276
                September 2010
                September 2010
                September 11 2010
                : 37
                : 17
                : n/a
                Affiliations
                [1 ]Section 2.2, Deutsches GeoForschungsZentrum GFZ; Potsdam; Germany
                [2 ]Meteorological, Climatological and Geophysical Agency; Jakarta; Indonesia
                [3 ]Indonesian Institute of Sciences; Bandung; Indonesia
                Article
                10.1029/2010GL044211
                48550ba1-3e16-4667-8308-0ebaf8ea53ce
                © 2010

                http://doi.wiley.com/10.1002/tdm_license_1.1

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