Thermodynamics of the interaction between ice shelves and the sea

An ice shelf is a floating ice sheet, attached to land where ice is grounded along the coastline. Nourished both by surface snow accumulation and by glaciers and ice sheets flowing off the land, ice shelves can reach a considerable thickness, varying from up to 1 300 m when the ice starts to float t...

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Bibliographic Details
Published in:Polar Record
Main Author: Doake, C. S. M.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1976
Subjects:
Online Access:http://dx.doi.org/10.1017/s0032247400028692
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0032247400028692