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dc.contributor.authorWhillans, I. M.
dc.contributor.authorvan der Veen, Cornelis J.
dc.date.accessioned2015-04-08T20:07:36Z
dc.date.available2015-04-08T20:07:36Z
dc.date.issued1997-11-05
dc.identifier.citationWhillans, I. M. & Van Der Veen, C. J. "The role of lateral drag in the dynamics of Ice Stream B, Antarctica." Journal of Glaciology (1997) 43, 144. pp 231 - 327. http://www.igsoc.org:8080/journal/43/144/igs_journal_vol43_issue144_pg231-237.pdfen_US
dc.identifier.urihttp://hdl.handle.net/1808/17342
dc.description.abstractThe partitioning of resistive force between the bed and sides of Ice Stream B, Antarctica , is obtained for three large areas that have bee n measured using repeat aerial photogrammetry. Problems associated with data errors and local variations in ice strength and velocity are reduced by considering the a really ave raged budget of forces for each photo block. Results indicate that the bed under Ice Stream B must be very weak and unable to provide much res instance. Mechanical l control on this ice stream emanates almost entirely from the lateral margins.en_US
dc.publisherInternational Glaciological Societyen_US
dc.relation.isversionofhttp://www.igsoc.org:8080/journal/43/144/igs_journal_vol43_issue144_pg231-237.pdf
dc.titleThe role of lateral drag in the dynamics of Ice Stream B, Antarcticaen_US
dc.typeArticle
kusw.kuauthorvan der Veen, Cornelis J.
kusw.kudepartmentGeographyen_US
kusw.oaversionScholarly/refereed, publisher version
kusw.oapolicyThis item does not meet KU Open Access policy criteria.
dc.rights.accessrightsopenAccess


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