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Subglacial sediment distribution from constrained seismic inversion, using MuLTI software: Examples from Midtdalsbreen, Norway

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Figure

Figure 1 illustrates MuLTIschematic differences between the unconstrained (and depth-constrained (’s model geometry and showsFig
Fig. 2. (a) Location of Hardangerjøkulen ice cap, South Norway. (b) Google Earth image of Midtdalsbreen, an outlet glacier of theHardangerjøkulen ice cap
Fig. 5. GPR velocity precision results, using Booth and others (2011) Monte Carlo simulation method, displaying probability density functionsof (a) ice and (b) snow GPR velocities derived from CMP B and C.
Table 1. Elastic parameter boundaries applied in MuLTI for the(glacier feasibility study
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