tidal bending of ice shelves as a mechanism for large-scale temporal variations in ice flow
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ID: 238431
2018
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Abstract
GPS measurements reveal strong modulation of horizontal
ice shelf and ice stream flow at a variety of tidal frequencies, most notably
a fortnightly (Msf) frequency not present in the vertical tides
themselves. Current theories largely fail to explain the strength and
prevalence of this signal over floating ice shelves. We show how well-known
non-linear aspects of ice rheology can give rise to widespread, long-periodic
tidal modulation in ice shelf flow, generated within ice shelves themselves
through tidal flexure acting at diurnal and semidiurnal frequencies. Using
full-Stokes viscoelastic modelling, we show that inclusion of tidal bending
within the model accounts for much of the observed tidal modulation of
ice shelf flow. Furthermore, our model shows that, in the absence of vertical
tidal forcing, the mean flow of the ice shelf is reduced by almost 30 % for
the geometry that we consider.
| Reference Key |
rosier2018thetidal
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|---|---|
| Authors | ;S. H. R. Rosier;G. H. Gudmundsson |
| Journal | journal of applied polymer science |
| Year | 2018 |
| DOI |
10.5194/tc-12-1699-2018
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| URL | |
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