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Critical investigation of calculation methods for the elastic velocities in anisotropic ice polycrystals

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Figure

Figure 1. Spherical angles (ϕ, θ) used for the orientation of thec axis, (cˆ is an unitary vector).
Figure 2. First configuration of a VTI girdle with a single zenith angle θ0. (a) shows a typical c axis ˆc = (sinθ0 cosϕ, sinθ0 sinϕ, cosθ0)within one grain, with a constant θ0, and ϕ varies randomly from grain to grain
Figure 4. Illustration of the inconsistency of the velocity averaging method for the two VTI textures shown in Fig
Figure 5. (a) System of angles used in Bennett’s calculations.given by ( ˆc isϕ, θ) and k is given by σ, being otherwise in the (e1,e3) plane

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