ICESat’s new perspective on ice shelf rifts: the vertical dimension. Geophys

[1] The small footprint ($70 m) and $172 m alongtrack spacing of the Geoscience Laser Altimeter System (GLAS) on the Ice, Cloud and land Elevation Satellite (ICESat) provides unprecedented horizontal resolution for a satellite altimeter. This enables ICESat to map many previously unresolved features...

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Bibliographic Details
Main Authors: H A Fricker, J N Bassis, B Minster, D R Macayeal
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2005
Subjects:
Amery
Ross Ice Shelf
Ice Shelf
Ice Shelves
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1084.1851
http://geosci.uchicago.edu/pdfs/macayeal/Fricker_macayeal_rift.pdf
Description
Summary:[1] The small footprint ($70 m) and $172 m alongtrack spacing of the Geoscience Laser Altimeter System (GLAS) on the Ice, Cloud and land Elevation Satellite (ICESat) provides unprecedented horizontal resolution for a satellite altimeter. This enables ICESat to map many previously unresolved features on ice shelves, such as crevasses, rifts, grounding zones and ice fronts. We present examples of ICESat-derived elevation data showing topography over rifts on the Amery and Ross ice shelves, widths of rifts and as estimates of the thickness of mélange (a collection of ice and snow trapped inside the rifts). We show that mélange thickness remains constant over the ICESat data period and tends to be thicker in older rifts. We validate the ICESat-derived mélange depth estimate with an in situ measurement on the Ross Ice Shelf.

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