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| Titel |
Hydrological modelling of glacierized catchments focussing on the validation of simulated snow patterns – applications within the flood forecasting system of the Tyrolean river Inn |
| VerfasserIn |
J. Schöber, S. Achleitner, R. Kirnbauer, F. Schöberl, H. Schönlaub |
| Medientyp |
Artikel
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| Sprache |
Englisch
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| ISSN |
1680-7340
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| Digitales Dokument |
URL |
| Erschienen |
In: Hydrologic Modelling for the Assessment of Ecosystem Services and Landscape Functions ; Nr. 27 (2010-09-28), S.99-109 |
| Datensatznummer |
250016346
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| Publikation (Nr.) |
 copernicus.org/adgeo-27-99-2010.pdf |
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| Zusammenfassung |
| The catchment of the river Inn is located in the Swiss and Austrian Alps. In
the frame of the flood forecasting system "HoPI"
(Hochwasserprognose für den Tiroler Inn), the
Austrian part of the river Inn and its tributaries are covered within a
hybrid numerical model. The runoff from the glacierized headwaters of the
south-western Inn tributaries is calculated using the Snow- and Icemelt Model
"SES" which utilizes a spatially-distributed energy balance approach;
within SES, the accumulation and melting processes for snow, firn, and ice
are considered. It is of great importance that such a type of model is used
in the simulation of alpine areas since in these regions stream flow is
influenced by the accumulation and melt of snow and ice and snow-free
glaciers have also the potential to increase or even induce flood flow. For a
prototype of the forecast system, SES was calibrated using the snow depletion
of a glacier, but later, following the first results during the operational
mode, the model was recalibrated and validated using remotely-sensed data
covering all 13 glacierized catchments. Using the final snow-parameter
setting, a simulation run of 15 hydrological years without any state
corrections achieved overall agreements between observed and simulated snow
cover ranging from 68% to 88% for all individual catchments. Runoff was
calibrated and validated using the data from three different gauges. A
parameter set, including both validated snow and runoff parameters, was
applied for the modelling of a fourth gauged catchment and also achieved
accurate results. This final unique parameterization was transferred to the
remaining, ungauged watersheds. |
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