Articles | Volume 7, issue 3
The Cryosphere, 7, 779–795, 2013
The Cryosphere, 7, 779–795, 2013

Research article 06 May 2013

Research article | 06 May 2013

High-resolution interactive modelling of the mountain glacier–atmosphere interface: an application over the Karakoram

E. Collier1,2, T. Mölg2, F. Maussion2, D. Scherer2, C. Mayer3, and A. B. G. Bush1 E. Collier et al.
  • 1Department of Earth & Atmospheric Sciences, University of Alberta, Edmonton, Canada
  • 2Chair of Climatology, Technische Universität Berlin, Berlin, Germany
  • 3Commission for Geodesy and Glaciology, Bavarian Academy of Sciences and Humanities, Munich, Germany

Abstract. The traditional approach to simulations of alpine glacier mass balance (MB) has been one-way, or offline, thus precluding feedbacks from changing glacier surface conditions on the atmospheric forcing. In addition, alpine glaciers have been only simply, if at all, represented in atmospheric models to date. Here, we extend a recently presented, novel technique for simulating glacier–atmosphere interactions without the need for statistical downscaling, through the use of a coupled high-resolution mesoscale atmospheric and physically-based climatic mass balance (CMB) modelling system that includes glacier CMB feedbacks to the atmosphere. We compare the model results over the Karakoram region of the northwestern Himalaya with remote sensing data for the ablation season of 2004 as well as with in situ glaciological and meteorological measurements from the Baltoro glacier. We find that interactive coupling has a localized but appreciable impact on the near-surface meteorological forcing data and that incorporation of CMB processes improves the simulation of variables such as land surface temperature and snow albedo. Furthermore, including feedbacks from the glacier model has a non-negligible effect on simulated CMB, reducing modelled ablation, on average, by 0.1 m w.e. (−6.0%) to a total of −1.5 m w.e. between 25 June–31 August 2004. The interactively coupled model shows promise as a new, multi-scale tool for explicitly resolving atmospheric-CMB processes of mountain glaciers at the basin scale.