Ocean interactions with the base of Amery Ice Shelf, Antarctica
Using a two-dimensional ocean themohaline circulation model, we varied the cavity shape beneath Amery Ice Shelf in an attempt to reproduce the 150-m-thick marine ice layer observed at the 'G1' ice core site. Most simulations caused melting rates which decrease the ice thickness by as much...
Main Authors: | , |
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Format: | Other/Unknown Material |
Language: | unknown |
Published: |
1992
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Online Access: | http://ntrs.nasa.gov/search.jsp?R=19930037350 |