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Acknowledgement of Professor Lliboutry's reply to “Comments by J. Nye on “Temperate ice permeability, stability of water veins and percolation of internal meltwater” by L. Lliboutry”

Published online by Cambridge University Press:  20 January 2017

John Nye
John Nye*
Affiliation:
H. H. Wills Physics Laboratory, University of Bristol, Bristol BS8 1TL, England
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Type
Correspondence
Information
Journal of Glaciology , Volume 43 , Issue 144 , 1997 , pp. 373
Copyright
Copyright © International Glaciological Society 1997

Sir,

I am grateful to Professor 1.1 iboutry for his response. On the second point, he is perfectly right in pointing out that my Reference Nye(Nye, 1976) paper omitted the heat flow between lenses and veins; this had indeed been treated quantitatively bv Reference Nye and MaeNye and Mae (1972), but ignoring any effect of the different salinities and without considering in detail the effect oil permeability. I amglad to sec that Professor Lliboutry has now given attention to the effect this heat flux may have on the permeability ofglaciers to water.

26 March 1997

References

Nye, J.F. 1976. Water flow in glaciers: jökulhlaups, tunned and veins. J. Glaciol., 17(76), 181–207.CrossRefGoogle Scholar
Nye, J. F. and Mae, S. 1972. The effect οf non-hydrostatic stress on intergranular water grains and lenses in ice. J. Glaciol., 11(61), 81–101.Google Scholar