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...

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Bibliographic Details
Main Authors: Hellmer, Hartmut H., Jacobs, Stanley S.
Format: Other/Unknown Material
Language:unknown
Published: 1992
Subjects:
48
Online Access:http://ntrs.nasa.gov/search.jsp?R=19930037350