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Deep Time Reconstructions of Internal Earth Structure with the Adjoint Method
作者姓名:BUNGE Hans-Peter  COLLI Lorenzo  GHELICHKHAN Siavash  OESER Jens
摘    要:正The adjoint method is a powerful tool to obtain gradient information in a computational model relative to unknown model parameters,allowing one to solve inverse problems where analytical solutions are not available or the cost to determine prohibitive.In geodynamics its most prominent application relates to the restoration problem of mantle convection(i.e.,to reconstruct past mantle flow states with dynamic earth models back in time by finding optimal flow histories relative to


Deep Time Reconstructions of Internal Earth Structure with the Adjoint Method
Authors:BUNGE Hans-Peter  COLLI Lorenzo  GHELICHKHAN Siavash and OESER Jens
Institution:1 Department of Geosciences, Ludwig-Maximilians University, D-80333 Munich, Theresienstrasse 41,2 Department of Earth and Atmospheric Sciences, University of Houston,1 Department of Geosciences, Ludwig-Maximilians University, D-80333 Munich, Theresienstrasse 41 and 1 Department of Geosciences, Ludwig-Maximilians University, D-80333 Munich, Theresienstrasse 41
Abstract:
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