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

dc.contributorHáskóli Íslandsen_US
dc.contributorUniversity of Icelanden_US
dc.contributor.authorGopalan, Giridhar Raja
dc.contributor.authorHrafnkelsson, Birgir
dc.contributor.authorAdalgeirsdottir, Gudfinna
dc.contributor.authorJarosch, Alexander H.
dc.contributor.authorPálsson, Finnur
dc.contributor.departmentRaunvísindadeild (HÍ)en_US
dc.contributor.departmentFaculty of Physical Sciences (UI)en_US
dc.contributor.departmentJarðvísindastofnun (HÍ)en_US
dc.contributor.departmentInstitute of Earth Sciences (UI)en_US
dc.contributor.schoolVerkfræði- og náttúruvísindasvið (HÍ)en_US
dc.contributor.schoolSchool of Engineering and Natural Sciences (UI)en_US
dc.date.accessioned2018-08-29T13:29:13Z
dc.date.available2018-08-29T13:29:13Z
dc.date.issued2018-07-11
dc.description.abstractBayesian 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.en_US
dc.description.sponsorshipThe Icelandic Research Fund (RANNIS) is thanked for funding this research.en_US
dc.description.versionPeer Revieweden_US
dc.format.extent2229-2248en_US
dc.identifier.citationGopalan, 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.en_US
dc.identifier.doi10.5194/tc-12-2229-2018
dc.identifier.issn1994-0416
dc.identifier.issn1994-0424 (eISSN)
dc.identifier.journalThe Cryosphereen_US
dc.identifier.urihttps://hdl.handle.net/20.500.11815/815
dc.language.isoenen_US
dc.publisherCopernicus GmbHen_US
dc.relation.ispartofseriesThe Cryosphere;12(7)
dc.relation.urlhttps://www.the-cryosphere.net/12/2229/2018/tc-12-2229-2018.pdfen_US
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.subjectJöklafræðien_US
dc.subjectJöklarannsókniren_US
dc.subjectÍshvelen_US
dc.titleA Bayesian hierarchical model for glacial dynamics based on the shallow ice approximation and its evaluation using analytical solutionsen_US
dc.typeinfo:eu-repo/semantics/articleen_US
dcterms.license© Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License.en_US

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