Katabatic wind influence on meltwater supply to fuel glacier-substrate interactions at grounding line, Terra Nova Bay, Antarctica

The co-isotopic composition, both in δD and in δ18O, of interbedded debris-rich and clear ice layers, thought to have been formed at the grounding line of Hells Gate Ice Shelf, indicates freezing by a double-diffusion effect between continental meltwater and sea water within a subglacial sediment. A...

Full description

Bibliographic Details
Main Authors: Bouzette, Ariane, Souchez, Roland
Format: Article in Journal/Newspaper
Language:English
Published: 1999
Subjects:
Glaciologie
Hells Gate
Marginal Lake
Terra Nova Bay
Annals of Glaciology
Antarc*
Antarctica
Ice Shelf
Online Access:http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/173121
https://dipot.ulb.ac.be/dspace/bitstream/2013/173121/3/doi_156751.pdf

Similar Items