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dc.contributor.authorÅström, Jan
dc.contributor.authorRiikilä, Timo
dc.contributor.authorTallinen, Tuomas
dc.contributor.authorZwinger, Thomas
dc.contributor.authorBenn, D.
dc.contributor.authorMoore, J.C.
dc.contributor.authorTimonen, Jussi
dc.date.accessioned2016-01-28T11:28:48Z
dc.date.available2016-01-28T11:28:48Z
dc.date.issued2013
dc.identifier.citationÅström, J., Riikilä, T., Tallinen, T., Zwinger, T., Benn, D., Moore, J. C., & Timonen, J. (2013). A particle based simulation model for glacier dynamics. <em>Cryosphere</em>, 7 (5), 1591-1602. <a href="http://dx.doi.org/10.5194/tc-7-1591-2013">doi:10.5194/tc-7-1591-2013</a> Retrieved from <a href="http://www.the-cryosphere.net/7/1591/2013/tc-7-1591-2013.pdf">http://www.the-cryosphere.net/7/1591/2013/tc-7-1591-2013.pdf</a>
dc.identifier.otherTUTKAID_60759
dc.identifier.urihttps://jyx.jyu.fi/handle/123456789/48502
dc.description.abstractA particle-based computer simulation model was developed for investigating the dynamics of glaciers. In the model, large ice bodies are made of discrete elastic particles which are bound together by massless elastic beams. These beams can break, which induces brittle behaviour. At loads below fracture, beams may also break and reform with small probabilities to incorporate slowly deforming viscous behaviour in the model. This model has the advantage that it can simulate important physical processes such as ice calving and fracturing in a more realistic way than traditional continuum models. For benchmarking purposes the deformation of an ice block on a slip-free surface was compared to that of a similar block simulated with a Finite Element fullStokes continuum model. Two simulations were performed: (1) calving of an ice block partially supported in water, similar to a grounded marine glacier terminus, and (2) fracturing of an ice block on an inclined plane of varying basal friction, which could represent transition to fast flow or surging. Despite several approximations, including restriction to twodimensions and simplified water-ice interaction, the model was able to reproduce the size distributions of the debris observed in calving, which may be approximated by universal scaling laws. On a moderate slope, a large ice block was stable and quiescent as long as there was enough of friction against the substrate. For a critical length of frictional contact, global sliding began, and the model block disintegrated in a manner suggestive of a surging glacier. In this case the fragment size distribution produced was typical of a grinding process.
dc.language.isoeng
dc.publisherCopernicus Publications
dc.relation.ispartofseriesCryosphere
dc.relation.urihttp://www.the-cryosphere.net/7/1591/2013/tc-7-1591-2013.pdf
dc.subject.otherLaskennallinen materiaalifysiikka
dc.subject.otherjään tutkimus
dc.subject.otherPhysics
dc.subject.otherMechanics
dc.subject.otherComputational material physics
dc.subject.otherice behaviour
dc.titleA particle based simulation model for glacier dynamics
dc.typearticle
dc.identifier.urnURN:NBN:fi:jyu-201601271299
dc.contributor.laitosFysiikan laitosfi
dc.contributor.laitosDepartment of Physicsen
dc.contributor.oppiaineFysiikka
dc.type.urihttp://purl.org/eprint/type/JournalArticle
dc.date.updated2016-01-27T13:15:08Z
dc.type.coarjournal article
dc.description.reviewstatuspeerReviewed
dc.format.pagerange1591-1602
dc.relation.issn1994-0416
dc.relation.volume7
dc.type.versionpublishedVersion
dc.rights.copyright© Author(s) 2013. This is an open access article distributed under the terms of Creative Commons Attribution 3.0 License
dc.rights.accesslevelopenAccessfi
dc.rights.urlhttps://creativecommons.org/licenses/by/3.0/
dc.relation.doi10.5194/tc-7-1591-2013


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© Author(s) 2013. This is an open access article distributed under the terms of Creative Commons Attribution 3.0 License
Except where otherwise noted, this item's license is described as © Author(s) 2013. This is an open access article distributed under the terms of Creative Commons Attribution 3.0 License