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To
improve our understanding of controls of
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erosion
rates (sliding power, basal T)
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To
determine erosion rates by dynamic glaciers
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outside
Alaska: Patagonia
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To
improve estimates of glacial erosion rates
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Longer
time scales
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Better
modeling of spatial and temporal
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patterns
of erosion through the large glacial-
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interglacial
climatic oscillations
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