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Modelling of Local Length-Scale Dynamics and Isotropizing Deformations: Formulation in Natural Coordinate System

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Academic year: 2021

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Figure

Figure 1. Stream function used to create the displacement field. The arrows indicate the direction and the intensity of the associated displacement.
Figure 2. For dt = 0.05, deformation of the regular coordinate system by the action of the deformation (a) D, (c) D ◦
Figure 3. Example of one realization of (a) an homogeneous-isotropic error of length-scale L h = 50km, and (b) its deformed version for dt = 0.05.
Figure 4. Anisotropy diagnosis for (a) the analytical metric tensor deduced from Eq. (10) and (b) the ensemble diagnosed tensor, for dt = 0.05
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