Combining SAR interferometry and the equation of continuity to estimate the three-dimensional glacier surface-velocity vector

Abstract Until now, an assumption of surface-parallel glacier flow has been used to express the vertical velocity component in terms of the horizontal velocity vector, permitting all three velocity components to be determined from synthetic aperture radar interferometry. We discuss this assumption,...

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Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Reeh, Niels, Madsen, Søren Nørvang, Mohr, Johan Jakob
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1999
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000001398
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000001398