Articles | Volume 4, issue 2
The Cryosphere, 4, 179–190, 2010
https://doi.org/10.5194/tc-4-179-2010
The Cryosphere, 4, 179–190, 2010
https://doi.org/10.5194/tc-4-179-2010

Research article 10 May 2010

Research article | 10 May 2010

Modelling snowdrift sublimation on an Antarctic ice shelf

J. T. M. Lenaerts1, M. R. van den Broeke1, S. J. Déry2, G. König-Langlo3, J. Ettema1, and P. K. Munneke1 J. T. M. Lenaerts et al.
  • 1Institute for Marine and Atmospheric research Utrecht, Utrecht University, Utrecht, The Netherlands
  • 2University of Northern British Columbia, Prince George, Canada
  • 3Alfred Wegener Institüt für Polar- und Meeresforschung, Bremerhaven, Germany

Abstract. In this paper, we estimate the contribution of snowdrift sublimation (SUds) to the surface mass balance at Neumayer, located on the Ekström ice shelf in Eastern Antarctica. A single column version of the RACMO2-ANT model is used as a physical interpolation tool of high-quality radiosonde and surface measurements for a 15-yr period (1993–2007), and combined with a routine to calculate snowdrift sublimation and horizontal snow transport. The site is characterised by a relatively mild, wet and windy climate, so snowdrift is a common phenomenon. The modelled timing and frequency of snowdrift events compares well with observations. This is further illustrated by an additional simulation for Kohnen base, where the timing of snowdrift is realistic, although the modelled horizontal transport is overestimated. Snowdrift sublimation is mainly dependent on wind speed, but also on relative humidity and temperature. During high wind speeds, SUds saturates and cools the air, limiting its own strength. We estimate that SUds removes around 16%±8% of the accumulated snow from the surface. The total sublimation more than triples when snowdrift is considered, although snowdrift sublimation limits sublimation at the surface. SUds shows a strong seasonal cycle, as well as large inter-annual variability. This variability can be related to the variability of the atmospheric conditions in the surface layer.

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