Abstract:
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Glacial surface velocity is modeled as a sum of a gravitational deformational component and a basal sliding component, which both depend on important physical parameters. Using a shallow ice approximation physics model for glacial surface velocity, we conduct Bayesian inference to infer these parameters at Langjökull, a prominent Icelandic glacier. The posterior estimate for an ice-softness parameter is comparable with recommended values, and spatial patterns in basal sliding also coincide with previous studies of Langjökull. Residual analysis suggests that a normal data distribution for surface velocity is not a good fit, an important finding since many Bayesian statistical models of surface velocity make this assumption. Gibbs sampling is used for Bayesian computation.
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