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Title: Fluctuations of the terminus of the Moltke Glacier
Authors: Mock, S. J.
Keywords: Glaciers
Moltke Glacier, Greenland
Glacier flow
Glacier oscillation
Glacier movement
Publisher: Cold Regions Research and Engineering Laboratory (U.S.)
Engineer Research and Development Center (U.S.)
Series/Report no.: Technical report (Cold Regions Research and Engineering Laboratory (U.S.)) ; 179.
Description: Technical Report
Abstract: The terminus position of the Moltke Glacier (one of 3 glaciers which reach tidewater in Wolstenholme Fjord, Greenland) has been mapped from existing maps and from aerial and terrestrial photographs for the years 1946-47, 1954, 1956, 1962, and 1965. With earlier work by J. W. Wright (1939), a fairly detailed record of terminus position exists for the period 1916 to 1965. The glacier has been in nearly continuous retreat during this period, interrupted by a slight advance from 1926 to 1932. Loss of area has been accelerating since 1946-47. Ice flow velocity near the terminus has fluctuated through a known range from 30 m/yr to over 1000 m/yr. The observed changes in velocity may be connected with the arrival of broad kinematic waves near the terminus. The waves could lead to an increase in sliding velocity if the bed of the glacier, at least in the extreme lower reaches, is near or at the pressure melting point.
Rights: Approved for public release; distribution is unlimited.
Appears in Collections:Technical Report

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