Spatially extensive estimates of annual accumulation in the dry snow zone of the Greenland Ice Sheet determined from radar altimetry

• Published in: The Cryosphere
• Main Authors: de la Pena, S., Nienow, P., Shepherd, A., Helm, V., Mair, D., Hanna, E., Huybrechts, P., Guo, Q., Cullen, R., Wingham, D.
• Format: Article in Journal/Newspaper
• Language: English
• Published: European Geosciences Union (EGU) / Copernicus Publications 2010
• Subjects: F890 Geographical and Environmental Sciences not elsewhere classified; Greenland; Ice Sheet; The Cryosphere
• Online Access: https://eprints.lincoln.ac.uk/id/eprint/26160/; https://eprints.lincoln.ac.uk/id/eprint/26160/1/26160%20tc-4-467-2010.pdf; https://doi.org/10.5194/tc-4-467-2010

We present estimates of accumulation rate along a 200 km transect ranging in elevation from 2750 to 3150 m in the dry snow zone on the western slope of the Greenland Ice Sheet. An airborne radar altimeter is used to estimate the thickness of annual internal layers and, in conjunction with ground based snow/firn density profiles, annual accumulation rates between 1998 and 2003 are derived. A clear gradient in the thickness of each layer observed by the radar altimeter and in the associated estimates of annual accumulation is seen along the transect, with a 33.6% ± 16% mean decrease in accumulation from west to east. The observed inter-annual variability is high, with the annual mean accumulation rate estimated at 0.359 m.w.e. yr−1 (s.d. ± 0.049 m.w.e. yr−1). Mean accumulation rates modelled using meteorological models overestimate our results by 16% on average, but by 32% and 42% in the years 2001 and 2002. The methodology presented here demonstrates the potential to obtain accurate and spatially extensive accumulation rates from radar altimeters in regions of ice sheets where field observations are sparse, and accumulation rates greater than several tens of cm.