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Dynamic response of surface energy and mass balance of Vest- and Austfonna (Nordaustlandet, Svalbard) on climate change

Fachliche Zuordnung Physische Geographie
Förderung Förderung von 2008 bis 2014
Projektkennung Deutsche Forschungsgemeinschaft (DFG) - Projektnummer 54616321
 
Erstellungsjahr 2014

Zusammenfassung der Projektergebnisse

The DFG-funded work on Vestfonna ice cap during the International Polar Year and beyond has proven that the glaciers and ice caps of Nordaustlandet provide an excellent showcase of region-specific climate-glacier interrelation. While most glaciers on Svalbard have been retreating in recent decades this is not the case for the ice caps of Nordaustlandet. However, as anticipated in the proposal, we were able to show that processes that may eventually lead to a strongly non-linear response of the mass balance under continuing global warming are indeed already underway and can be observed for Vestfonna ice cap. This leads to the conclusion that Nordaustlandet, showing a rather well-balanced climatic mass balance in recent decades and only little variations of the calving fronts, may be subject of increasingly and strongly negative mass balance in the course of the 21st century. We could show that the climatic mass balance of Vestfonna can be adequately modelled by different approaches. When using an enhanced temperature-radiation index model, refreezing must also be taken into account since it contributed between 25% and 30% of the annual accumulation. Also, a reliable method for cloudiness parameterization is crucial in order to obtain resilient results. Snow drift plays a major role in redistributing accumulating snow on and beyond the ice cap as the example of small of De Geerfonna could show both in observations and in the snowdrift modeling. The excellent measurement data and the modelling results provide opportunities for further research. For instance, an adjusted temperature-radiation index model driven by climate projection data from CIMP5 can be run over the entire 21st century in order to provide CMB estimates of Vestfonna for the 21st century. This may also provide an estimate of Vestfonna ice cap’s contribution to future sea level rise. The excellent observational data and the European Arctic Reanalysis (EAR) data will enable to run a fully spatially distributed physically-based surface energy and mass balance model that couples boundary layer atmosphere and snow cover. We hope that this kind of research will result in an even better understanding of the energy fluxes and related processes in the snow cover and at the surface that influence the overall mass balance of glaciers and ice caps.

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