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In‐situ quantification of ice rheology and direct measurement of the Raymond Effect at Summit, Greenland using a phase‐sensitive radar
Author(s) -
GilletChaulet Fabien,
Hindmarsh Richard C. A.,
Corr Hugh F. J.,
King Edward C.,
Jenkins Adrian
Publication year - 2011
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2011gl049843
Subject(s) - geology , rheometry , rheology , greenland ice sheet , ice stream , ice sheet , glaciology , groenlandia , strain rate , forcing (mathematics) , phase (matter) , summit , climatology , sea ice , geomorphology , physical geography , cryosphere , materials science , physics , geotechnical engineering , hydrogeology , geography , quantum mechanics , composite material , metamorphic petrology , metallurgy
The Glen exponent n characterizes the stress‐dependence of ice deformation, directly influencing the rate at which ice masses respond to external forcing. The slow deformation in large ice‐sheets makes laboratory rheometry at representative strain‐rates difficult. We develop a new technique to estimate n in‐situ , deploying a phase‐sensitive radar to measure vertical strain rates of around 10 −4 yr −1 within the top 1000 m of ice across ice divides at Summit and NEEM, Greenland. A fluid‐dynamical feature, the Raymond Effect, predicts strong vertical strain‐rate variation across divides over distances of a few ice‐thicknesses. We achieve sufficient resolution to show this pattern, enabling us to estimate n = 4.5 by inverting our observations with flow modelling. This is higher than values previously used but consistent with other indirect measurements, implying laboratory measurements do not explore the full range of ice rheology and the consequent possibility of a greater sensitivity and responsiveness in ice‐sheet dynamics.