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A Bayesian hierarchical model for glacial dynamics based on the shallow ice approximation and its evaluation using analytical solutions

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dc.contributor Háskóli Íslands
dc.contributor University of Iceland
dc.contributor.author Gopalan, Giridhar Raja
dc.contributor.author Hrafnkelsson, Birgir
dc.contributor.author Adalgeirsdottir, Gudfinna
dc.contributor.author Jarosch, Alexander H.
dc.contributor.author Pálsson, Finnur
dc.date.accessioned 2018-08-29T13:29:13Z
dc.date.available 2018-08-29T13:29:13Z
dc.date.issued 2018-07-11
dc.identifier.citation Gopalan, G., Hrafnkelsson, B., Aðalgeirsdóttir, G., Jarosch, A. H., and Pálsson, F.: A Bayesian hierarchical model for glacial dynamics based on the shallow ice approximation and its evaluation using analytical solutions, The Cryosphere, 12, 2229-2248, https://doi.org/10.5194/tc-12-2229-2018, 2018.
dc.identifier.issn 1994-0416
dc.identifier.issn 1994-0424 (eISSN)
dc.identifier.uri https://hdl.handle.net/20.500.11815/815
dc.description.abstract Bayesian hierarchical modeling can assist the study of glacial dynamics and ice flow properties. This approach will allow glaciologists to make fully probabilistic predictions for the thickness of a glacier at unobserved spatiotemporal coordinates, and it will also allow for the derivation of posterior probability distributions for key physical parameters such as ice viscosity and basal sliding. The goal of this paper is to develop a proof of concept for a Bayesian hierarchical model constructed, which uses exact analytical solutions for the shallow ice approximation (SIA) introduced by Bueler et al. (2005). A suite of test simulations utilizing these exact solutions suggests that this approach is able to adequately model numerical errors and produce useful physical parameter posterior distributions and predictions. A byproduct of the development of the Bayesian hierarchical model is the derivation of a novel finite difference method for solving the SIA partial differential equation (PDE). An additional novelty of this work is the correction of numerical errors induced through a numerical solution using a statistical model. This error-correcting process models numerical errors that accumulate forward in time and spatial variation of numerical errors between the dome, interior, and margin of a glacier.
dc.description.sponsorship The Icelandic Research Fund (RANNIS) is thanked for funding this research.
dc.format.extent 2229-2248
dc.language.iso en
dc.publisher Copernicus GmbH
dc.relation.ispartofseries The Cryosphere;12(7)
dc.rights info:eu-repo/semantics/openAccess
dc.subject Jöklafræði
dc.subject Jöklarannsóknir
dc.subject Íshvel
dc.title A Bayesian hierarchical model for glacial dynamics based on the shallow ice approximation and its evaluation using analytical solutions
dc.type info:eu-repo/semantics/article
dcterms.license © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License.
dc.description.version Peer Reviewed
dc.identifier.journal The Cryosphere
dc.identifier.doi 10.5194/tc-12-2229-2018
dc.relation.url https://www.the-cryosphere.net/12/2229/2018/tc-12-2229-2018.pdf
dc.contributor.department Raunvísindadeild (HÍ)
dc.contributor.department Faculty of Physical Sciences (UI)
dc.contributor.department Jarðvísindastofnun (HÍ)
dc.contributor.department Institute of Earth Sciences (UI)
dc.contributor.school Verkfræði- og náttúruvísindasvið (HÍ)
dc.contributor.school School of Engineering and Natural Sciences (UI)


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