Imaging of firn isochrones across an Antarctic ice rise and implications for patterns of snow accumulation rate

Vaughan, D.G. ORCID: https://orcid.org/0000-0002-9065-0570; Anderson, P.S.; King, J.C. ORCID: https://orcid.org/0000-0003-3315-7568; Mann, G.W.; Mobbs, S.D.; Ladkin, R.S.. 2004 Imaging of firn isochrones across an Antarctic ice rise and implications for patterns of snow accumulation rate. Journal of Glaciology, 50 (170). 413-418. https://doi.org/10.3189/172756504781829882

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Abstract/Summary

It has been an underlying assumption in many studies that near-surface layers imaged by ground-penetrating radar (GPR) can be interpreted as depositional markers or isochrones. It has been shown that GPR layers can be approximately reproduced from the measured electrical properties of ice, but these material layers are generally narrower and more closely spaced than can be resolved by typical GPR systems operating in the range 50-400 MHz. Thus GPR layers should be interpreted as interference patterns produced from closely spaced and potentially discontinuous material layers, and should not be assumed to be interpretable as precise markers of isochrones. We present 100 MHz GPR data from Lyddan Ice Rise, Antarctica, in which near-surface (< 50 m deep) layers are clearly imaged. The growth of the undulations in these layers with depth is approximately linear, implying that, rather than resulting from a pattern of vertical strain rate, they do correspond to some pattern of snowfall variation. Furthermore, comparison of the GPR layers with snow-stake measurements suggests that around 80% of the rms variability in mean annual accumulation is present in the GPR layers. The observations suggest that, at least in this case, the GPR layers do approximate isochrones, and that patterns of snow accumulation over Lyddan Ice Rise are dominated by extremely persistent spatial variations with only a small residual spatial variability. If this condition is shown to be widely applicable it may reduce the period required for measurements of surface elevation change to be taken as significant indications of mass imbalance.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	https://doi.org/10.3189/172756504781829882
Programmes:	BAS Programmes > Antarctic Science in the Global Context (2000-2005) > Antarctic Climate Processes BAS Programmes > Antarctic Science in the Global Context (2000-2005) > Global Interactions of the Antarctic Ice Sheet
ISSN:	00221430
Additional Keywords:	Snow; Accumulation; Ground penetrating radar;
NORA Subject Terms:	Glaciology Data and Information
Date made live:	12 Aug 2010 14:55 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/10145

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