Implications of tde form of the flow law for vertical velocity and age–Depth profiles in polar ice
Wolff, Eric W.; Doake, C.S.M.. 1986 Implications of tde form of the flow law for vertical velocity and age–Depth profiles in polar ice. Journal of Glaciology, 32 (112). 366-370. 10.3189/S0022143000012053
Full text not available from this repository. (Request a copy)Abstract/Summary
Two situations are studied in relation to the flow law of polar ice. In each case, models are used with a flow-law exponent of one, and with the more traditional exponent of three. The horizontal velocity profile at Devon Island, Arctic Canada, is better fitted by n = 1; for the vertical velocity profile, n = 3 gives a better fit, but both model profiles fall well within experimental error. For the Camp Century age–depth profile, only n = 1 gives an acceptable fit when temperature is allowed for. The large discrepancy between isothermal and non-isothermal models for n = 3 shows the importance of allowing for temperature in studies of ice-sheet properties.
Item Type: | Publication - Article |
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Digital Object Identifier (DOI): | 10.3189/S0022143000012053 |
ISSN: | 0022-1430 |
Date made live: | 08 May 2019 08:17 +0 (UTC) |
URI: | https://nora.nerc.ac.uk/id/eprint/523221 |
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