Glacial erosion beneath ice streams and ice‐stream tributaries: constraints on temporal and spatial distribution of erosion from numerical simulations of a West Antarctic ice stream
Аннотация:Geologic evidence such as subglacial troughs and grounding zone wedges indicate that soft‐bedded, West Antarctic ice streams are capable of eroding, transporting and depositing large volumes of debris at high rates (˜100 m 3 yr ‐1 per meter width). In order to understand the dynamics of ice streams and the geologic effects of their activity, it is important to understand the physical mechanisms that control these high rates of sub‐ice‐stream sediment generation and transport. Here, we use a numerical model of Ice Stream C run over c. 8500 model years to quantify the effects of a recently proposed, till‐ploughing mechanism of till formation and redistribution beneath ice streams (Tulaczyk et al. 2001; Clark et al. in press). Our results show that this ‘transport‐limited’ mechanism, in which till transport rates scale with ice velocity and erosion rates with spatial gradients of velocity, is consistent with existing constraints. For instance, our model results predict significantly higher (˜0.6 mm yr ‐1 ) average erosion rates beneath ice‐stream tributaries, which are underlain by deep subglacial troughs, than beneath ice‐stream trunks (˜0.2mm yr ‐1 ), whose subglacial troughs have a significantly smaller relief. We would not obtain this satisfactory result if subglacial erosion was parametrized in the model using the more traditional approach of scaling erosion rates with ice velocity (what we call the ‘production‐limited’ parametrization). Because of the requirement of ice continuity, the magnitude of ice velocity generally increases downstream in polar ice streams, and so do the production‐limited erosion rates. Pending further investigations, we propose that geologic and geomorphic effects of soft‐bedded ice streams should be quantified using some form of a ‘transport‐limited’ parametrization of subglacial erosion rates, e.g. the till‐ploughing mechanism.
