Articles | Volume 25, issue 8
https://doi.org/10.5194/hess-25-4275-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/hess-25-4275-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
03 Aug 2021
Research article |
| 03 Aug 2021
| 03 Aug 2021
Mass balance and hydrological modeling of the Hardangerjøkulen ice cap in south-central Norway
Trude Eidhammer
CORRESPONDING AUTHOR
National Center for Atmospheric Research, P.O. Box 3000, Boulder, CO 80307, USA
Adam Booth
School of Earth and Environment, University of Leeds, Leeds, UK
Sven Decker
Department of Geosciences, University of Oslo, Oslo, Norway
NORCE Norwegian Research Centre, Bjerknes Centre for Climate Research, Bergen, Norway
Michael Barlage
National Center for Atmospheric Research, P.O. Box 3000, Boulder, CO 80307, USA
now at: National Centers for Environmental Prediction, NOAA, College Park, MD 20740, USA
David Gochis
National Center for Atmospheric Research, P.O. Box 3000, Boulder, CO 80307, USA
Roy Rasmussen
National Center for Atmospheric Research, P.O. Box 3000, Boulder, CO 80307, USA
Kjetil Melvold
Norwegian Water Resource and Energy Directorate, Oslo, Norway
Atle Nesje
Department of Earth Science, University of Bergen, Bergen, Norway
Stefan Sobolowski
NORCE Norwegian Research Centre, Bjerknes Centre for Climate Research, Bergen, Norway
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Short summary
We coupled a detailed snow–ice model (Crocus) to represent glaciers in the Weather Research and Forecasting (WRF)-Hydro model and tested it on a well-studied glacier. Several observational systems were used to evaluate the system, i.e., satellites, ground-penetrating radar (used over the glacier for snow depth) and stake observations for glacier mass balance and discharge measurements in rivers from the glacier. Results showed improvements in the streamflow projections when including the model.
We coupled a detailed snow–ice model (Crocus) to represent glaciers in the Weather Research and...
