Determination of a flow center on an ice cap

Abstract A method for identifying the center of ice flow is developed and applied using results from surveys of a strain grid near the summit of Dunde Ice Cap (central China). Strain rates are used to compute stresses. These are used with a consideration of the balance of forces to compute basal fri...

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Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Van Der Veen, C.J., Whillans, I. M.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1992
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000002288
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000002288
Description
Summary:Abstract A method for identifying the center of ice flow is developed and applied using results from surveys of a strain grid near the summit of Dunde Ice Cap (central China). Strain rates are used to compute stresses. These are used with a consideration of the balance of forces to compute basal friction. The flow center at the bed occurs where this friction changes sign. For Dunde Ice Cap, the basal flow center nearly underlies the summit.