Constraints on ice volume changes of the West Antarctic Ice Sheet and Ross

the Last Glacial Maximum (~20 ka), marine evidence indicates that the grounding line of the West Antarctic Ice Sheet (WAIS) advanced northwards into the Ross Ice Shelf (RIS), blocking drainage of outlet glaciers through the Transantarctic Mountains (TM) resulting in significant downstream thickening...

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Bibliographic Details
Main Authors: Fink, D, Storey, B, Joy, K, Shulmeister, J
Format: Conference Object
Language:English
Published: 12th International Conference on Accelerator Mass Spectrometry (AMS-12) 2011
Subjects:
Ices program
Cosmology
Antarcticia
Glaciers
Altitude
Greenhouse effect
Antarctic
Darwin Glacier
Diamond Hill
Dubris Valley
Ross Ice Shelf
The Antarctic
Transantarctic Mountains
Wellman
West Antarctic Ice Sheet
Antarc*
Ice Sheet
Ice Shelf
Online Access:http://apo.ansto.gov.au/dspace/handle/10238/4144
http://www.gns.cri.nz/ams12/

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