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An improved model for tidally modulated grounding-line migration

Tsai, Victor C. and Gudmundsson, G. Hilmar (2015) An improved model for tidally modulated grounding-line migration. Journal of Glaciology, 61 (226). pp. 216-222. ISSN 0022-1430. doi:10.3189/2015JoG14J152.

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Understanding grounding-line dynamics is necessary for predictions of long-term ice-sheet stability. However, despite growing observations of the tidal influence on grounding-line migration, this short-timescale migration is poorly understood, with most modeling attempts assuming beam theory to calculate displacements. Here we present an improved model of tidal grounding-line migration that treats migration as an elastic fracture problem, forced by the additional ocean water pressure from the tide. This new model predicts that the grounding line cannot be assumed to be in hydrostatic equilibrium and, furthermore, that migration is inherently asymmetric and nonlinear, with migration distances that are not proportional to the tidal load. Specifically, for constant surface slope, the grounding line migrates upstream approximately ten times further as the tide rises from mean sea level to high tide than it migrates downstream as the tide falls from mean sea level to low tide, and migration distances are substantially larger than simple flotation arguments suggest. Numerical tests also show that the dependence of migration distance on elastic moduli and ice-sheet thickness are inconsistent with predictions of beam theory for a range of realistic values. Finally, applying the new model to observations in Antarctica results in new estimates of bed slopes, though these estimates remain uncertain due to imperfect knowledge of the relevant rheological parameters.

Item Type:Article
Related URLs:
URLURL TypeDescription
Tsai, Victor C.0000-0003-1809-6672
Gudmundsson, G. Hilmar0000-0003-4236-5369
Additional Information:© 2015 IGS. MS received 12 August 2014 and accepted in revised form 6 December 2014. We thank Roiy Sayag and two anonymous reviewers for constructive reviews, and the California Institute of Technology for supporting G.H.G.’s visit. This research was carried out at the California Institute of Technology and the Jet Propulsion Laboratory under a contract with the National Aeronautics and Space Administration and partly funded through the President’s and Director’s Fund Program.
Group:Seismological Laboratory
Funding AgencyGrant Number
Caltech President’s FundUNSPECIFIED
JPL Director's Discretionary FundUNSPECIFIED
Subject Keywords:Antarctic glaciology, glacier mechanics, glacier modelling, ice/ocean interactions
Issue or Number:226
Record Number:CaltechAUTHORS:20150312-074943389
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Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:55723
Deposited By: Tony Diaz
Deposited On:12 Mar 2015 22:04
Last Modified:10 Nov 2021 20:49

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