Please use this identifier to cite or link to this item: https://hdl.handle.net/11681/5724
Title: Glacier sliding
Authors: Northwestern University (Evanston, Ill.). Technological Institute.
Weertman, Johannes.
Keywords: Glaciers
Glacier movement
Glacier sliding
Glacier ice
Ice
Ice cap
Ice sheet
Publisher: Cold Regions Research and Engineering Laboratory (U.S.)
Engineer Research and Development Center (U.S.)
Series/Report no.: Research report (Cold Regions Research and Engineering Laboratory (U.S.)) ; 162.
Description: Research Report
Summary: The theory of the sliding of glaciers presented in earlier papers has been generalized (1) by taking into account the resistance to sliding offered by obstacles both smaller and larger than the controlling obstacles and (2) by relaxing the assumption that ice is always in intimate contact with the bed at the downstream side of an obstacle. The sliding velocities and controlling obstacle sizes which are found from the generalized theory are approximately the same as those found from the earlier theory. A new result obtained from the present theory is the fact that a water layer an order of magnitude smaller in thickness than the height of the controlling obstacles can cause an appreciable increase in the sliding velocity. The generalized theory contains Lliboutry's sliding theory as an extreme limiting case. For certain thicknesses of a glacier the sliding velocity is a double-valued function of the shear stress exerted at the bed.
URI: http://hdl.handle.net/11681/5724
Appears in Collections:CRREL Research Report

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