Abstract
This study evaluates the water balance of the island of Sjælland (7330 km2) in Denmark using two different types of physically-based model approaches. The DaisyGIS model is an advanced 1-D land surface model
which is parameterized at the plot-scale and upscaled using remote sensing and GIS (Geographical Information System) data to represent land cover and
soil characteristics. In comparison, the DK-model constitutes a 3-D integrated hydrological model setup (based on the MIKE SHE code) which uses a
comprehensive geological data set and is calibrated to obtain global model parameters representing all catchments at Sjælland. A good agreement was
found between annual net precipitation (precipitation minus evapotranspiration) estimated by the two model systems, but seasonal differences in
evapotranspiration occurred which could be related to the use of the remote sensing for evapotranspiration calculation in Daisy or caused by dissimilar soil
properties. Despite these differences, the DK-model simulated streamflows efficiently for both agricultural and forest catchments. In contrast, Daisy simulations suggest that a more advanced distributed land surface parameterization can contribute to improving water balance simulations of urbanized surface-water dominated catchments. The integrated annual water balance of Sjælland was found to be nearly in balance but large spatial variations occurred among the 30 studied catchments. Overall, the results indicate a need for further studies on model sensitivity and uncertainties related to net precipitation quantification in spatially distributed hydrological modelling.
which is parameterized at the plot-scale and upscaled using remote sensing and GIS (Geographical Information System) data to represent land cover and
soil characteristics. In comparison, the DK-model constitutes a 3-D integrated hydrological model setup (based on the MIKE SHE code) which uses a
comprehensive geological data set and is calibrated to obtain global model parameters representing all catchments at Sjælland. A good agreement was
found between annual net precipitation (precipitation minus evapotranspiration) estimated by the two model systems, but seasonal differences in
evapotranspiration occurred which could be related to the use of the remote sensing for evapotranspiration calculation in Daisy or caused by dissimilar soil
properties. Despite these differences, the DK-model simulated streamflows efficiently for both agricultural and forest catchments. In contrast, Daisy simulations suggest that a more advanced distributed land surface parameterization can contribute to improving water balance simulations of urbanized surface-water dominated catchments. The integrated annual water balance of Sjælland was found to be nearly in balance but large spatial variations occurred among the 30 studied catchments. Overall, the results indicate a need for further studies on model sensitivity and uncertainties related to net precipitation quantification in spatially distributed hydrological modelling.
Original language | English |
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Title of host publication | Quantification and reduction of predictive uncertainty for sustainable water resources management. Proceedings of Symposium HS2004 at IUGG2007, Perugia, July 2007 |
Editors | Eva Boegh, Harald Kunstmann, Thorsten Wagener, Alan Hall, Luis Bastidas, Stewart Franks, Hoshin Gupta, Dan Rosbjerg, John Schaake |
Publisher | IAHS |
Pages | 267-277 |
Number of pages | 12 |
ISBN (Print) | 9781901502091 |
Publication status | Published - 2007 |
Event | International Union of Geodesy and Geophysics XXIV General Assembly - Perugia, Italy Duration: 2 Jul 2007 → 13 Jul 2007 Conference number: 24 |
Publication series
Series | IAHS Publication |
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Volume | 313 |
ISSN | 0144-7815 |
Conference
Conference | International Union of Geodesy and Geophysics XXIV General Assembly |
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Abbreviated title | IUAG XXIV |
Country/Territory | Italy |
City | Perugia |
Period | 2/07/07 → 13/07/07 |
Keywords
- 3-D Hydrological model
- Denmark
- Land surface model
- Large-scale
- Water balance modelling
Programme Area
- Programme Area 2: Water Resources