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Volume 10, issue 1
The Cryosphere, 10, 271-285, 2016
https://doi.org/10.5194/tc-10-271-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
The Cryosphere, 10, 271-285, 2016
https://doi.org/10.5194/tc-10-271-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 03 Feb 2016

Research article | 03 Feb 2016

The modelled surface mass balance of the Antarctic Peninsula at 5.5 km horizontal resolution

J. M. van Wessem1, S. R. M. Ligtenberg1, C. H. Reijmer1, W. J. van de Berg1, M. R. van den Broeke1, N. E. Barrand2, E. R. Thomas3, J. Turner3, J. Wuite4, T. A. Scambos5, and E. van Meijgaard6 J. M. van Wessem et al.
  • 1Institute for Marine and Atmospheric Research Utrecht, Utrecht University, Utrecht, the Netherlands
  • 2School of Geography, Earth and Environmental Sciences, University of Birmingham, Birmingham, UK
  • 3British Antarctic Survey, Cambridge, UK
  • 4ENVEO IT GmbH, Innsbruck, Austria
  • 5National Snow and Ice Data Center, University of Colorado, Boulder, CO, USA
  • 6Royal Netherlands Meteorological Institute, De Bilt, the Netherlands

Abstract. This study presents a high-resolution (∼ 5.5km) estimate of surface mass balance (SMB) over the period 1979–2014 for the Antarctic Peninsula (AP), generated by the regional atmospheric climate model RACMO2.3 and a firn densification model (FDM). RACMO2.3 is used to force the FDM, which calculates processes in the snowpack, such as meltwater percolation, refreezing and runoff. We evaluate model output with 132 in situ SMB observations and discharge rates from six glacier drainage basins, and find that the model realistically simulates the strong spatial variability in precipitation, but that significant biases remain as a result of the highly complex topography of the AP. It is also clear that the observations significantly underrepresent the high-accumulation regimes, complicating a full model evaluation.

The SMB map reveals large accumulation gradients, with precipitation values above 3000mmweyr−1 in the western AP (WAP) and below 500mmweyr−1 in the eastern AP (EAP), not resolved by coarser data sets such as ERA-Interim. The average AP ice-sheet-integrated SMB, including ice shelves (an area of 4.1 × 105km2), is estimated at 351Gtyr−1 with an interannual variability of 58Gtyr−1, which is dominated by precipitation (PR) (365±57Gtyr−1). The WAP (2.4 × 105km2) SMB (276±47Gtyr−1), where PR is large (276±47Gtyr−1), dominates over the EAP (1.7 × 105km2) SMB (75±11Gtyr−1) and PR (84±11Gtyr−1). Total sublimation is 11±2Gtyr−1 and meltwater runoff into the ocean is 4±4Gtyr−1. There are no significant trends in any of the modelled AP SMB components, except for snowmelt that shows a significant decrease over the last 36 years (−0.36Gtyr−2).

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This study presents the first high-resolution (5.5 km) modelled estimate of surface mass balance (SMB) over the period 1979–2014 for the Antarctic Peninsula (AP). Precipitation (snowfall and rain) largely determines the SMB, and is exceptionally high over the western mountain slopes, with annual values > 4 m water equivalent. Snowmelt is widespread over the AP, but only runs off into the ocean at some locations: the Larsen B,C, and Wilkins ice shelves, and along the north-western mountains.
This study presents the first high-resolution (5.5 km) modelled estimate of surface mass balance...
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