Thermal Convection in Ice Sheets: We look but do not see

Abstract Thermal convection in the Antarctic and Greenland ice sheets has been dismissed on the grounds that radio-echo stratigraphy is undisturbed for long distances. However, the undisturbed stratigraphy lies, for the most part, above the density inversion in polar ice sheets and therefore does no...

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Bibliographic Details
Published in:Journal of Glaciology
Main Author: Hughes, T.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1985
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000004974
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000004974