Studies of the Grounding Line Location on Ice Streams D and E, Antarctica

Landsat Thematic Mapper (TM) images were used prior to the 1991-92 field season to infer the position of the grounding line at the mouths of ice streams D and E, West Antarctica. Our field plan for mass balance studies was based on this determination, and thus the imagery played a central role in bo...

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Bibliographic Details
Main Authors: Robert W. Jacobel, Audrey E. Robinson, Robert A. Bindschadler
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.548.3584
http://www.stolaf.edu/people/jacobel/Papers/VISAG Annals 20 (w figs).pdf
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Summary:Landsat Thematic Mapper (TM) images were used prior to the 1991-92 field season to infer the position of the grounding line at the mouths of ice streams D and E, West Antarctica. Our field plan for mass balance studies was based on this determination, and thus the imagery played a central role in both the scientific and logistics planning. A radar profile along the flow direction was made across the inferred grounding line at one location, and ice thickness measurements together with surface surveying enable us to compare the hydrostatic surface and the actual topography to determine the point at which the ice becomes grounded. The profile transits from floating to grounded ice at the same location as the grounding line inferred from the imagery. Changes in the radar echo strength also occur at this location giving further support to this interpretation. Tilt studies of the ice flexure caused by tidal variations at locations on either side of this grounding