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University of Cambridge > Talks.cam > British Antarctic Survey > Applying adjoint methods to the glacial isostatic adjustment inverse problem
Applying adjoint methods to the glacial isostatic adjustment inverse problemAdd to your list(s) Download to your calendar using vCal
If you have a question about this talk, please contact Rosie Williams. If external to BAS, please email the organiser in advance to gain access to the building In this talk I will start with a brief introduction to the physics of glacial isostatic adjustment (GIA), focusing on the deformation of the solid Earth and how it can be modelled numerically. I will then describe the associated inverse problem whose aim is to infer the past evolution of ice sheets from observations of GIA . One approach to solving the inverse GIA problem is to use gradient-based optimization. Calculation of the required gradients can be computationally demanding, but I will show how this can be done very efficiently through an application of the so-called adjoint method. Finally, I will outline some future research plans which aim to incorporate ice-dynamics more fully into the GIA forward and inverse problems. This talk is part of the British Antarctic Survey series. This talk is included in these lists:
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