Estimation of parameters in a distributed precipitation-runoff model for Norway

A distributed version of the HBV-model using 1 km<sup>2</sup> grid cells and daily time step was used to simulate runoff from the entire land surface of Norway for the period 1961-1990. The model was sensitive to changes in small scale properties of the land surface and the climati...

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Main Authors: S. Beldring, K. Engeland, L. A. Roald, N. R. Sælthun, A. Voksø
Format: Article
Language:English
Published: Copernicus Publications 2003-01-01
Series:Hydrology and Earth System Sciences
Online Access:http://www.hydrol-earth-syst-sci.net/7/304/2003/hess-7-304-2003.pdf
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spelling doaj-4a37a40345d044d29658c6be7b3c4d932020-11-24T20:57:03ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382003-01-0173304316Estimation of parameters in a distributed precipitation-runoff model for NorwayS. BeldringS. BeldringK. EngelandL. A. RoaldN. R. SælthunA. VoksøA distributed version of the HBV-model using 1 km<sup>2</sup> grid cells and daily time step was used to simulate runoff from the entire land surface of Norway for the period 1961-1990. The model was sensitive to changes in small scale properties of the land surface and the climatic input data, through explicit representation of differences between model elements, and by implicit consideration of sub-grid variations in moisture status. A geographically transferable set of model parameters was determined by a multi-criteria calibration strategy, which simultaneously minimised the residuals between model simulated and observed runoff from 141 Norwegian catchments located in areas with different runoff regimes and landscape characteristics. Model discretisation units with identical landscape classification were assigned similar parameter values. Model performance was evaluated by simulating discharge from 43 independent catchments. Finally, a river routing procedure using a kinematic wave approximation to open channel flow was introduced in the model, and discharges from three additional catchments were calculated and compared with observations. The model was used to produce a map of average annual runoff for Norway for the period 1961-1990.</p> <p style='line-height: 20px;'><b>Keywords: </b>distributed model, multi-criteria calibration, global parameters, ungauged catchments.http://www.hydrol-earth-syst-sci.net/7/304/2003/hess-7-304-2003.pdf
collection DOAJ
language English
format Article
sources DOAJ
author S. Beldring
S. Beldring
K. Engeland
L. A. Roald
N. R. Sælthun
A. Voksø
spellingShingle S. Beldring
S. Beldring
K. Engeland
L. A. Roald
N. R. Sælthun
A. Voksø
Estimation of parameters in a distributed precipitation-runoff model for Norway
Hydrology and Earth System Sciences
author_facet S. Beldring
S. Beldring
K. Engeland
L. A. Roald
N. R. Sælthun
A. Voksø
author_sort S. Beldring
title Estimation of parameters in a distributed precipitation-runoff model for Norway
title_short Estimation of parameters in a distributed precipitation-runoff model for Norway
title_full Estimation of parameters in a distributed precipitation-runoff model for Norway
title_fullStr Estimation of parameters in a distributed precipitation-runoff model for Norway
title_full_unstemmed Estimation of parameters in a distributed precipitation-runoff model for Norway
title_sort estimation of parameters in a distributed precipitation-runoff model for norway
publisher Copernicus Publications
series Hydrology and Earth System Sciences
issn 1027-5606
1607-7938
publishDate 2003-01-01
description A distributed version of the HBV-model using 1 km<sup>2</sup> grid cells and daily time step was used to simulate runoff from the entire land surface of Norway for the period 1961-1990. The model was sensitive to changes in small scale properties of the land surface and the climatic input data, through explicit representation of differences between model elements, and by implicit consideration of sub-grid variations in moisture status. A geographically transferable set of model parameters was determined by a multi-criteria calibration strategy, which simultaneously minimised the residuals between model simulated and observed runoff from 141 Norwegian catchments located in areas with different runoff regimes and landscape characteristics. Model discretisation units with identical landscape classification were assigned similar parameter values. Model performance was evaluated by simulating discharge from 43 independent catchments. Finally, a river routing procedure using a kinematic wave approximation to open channel flow was introduced in the model, and discharges from three additional catchments were calculated and compared with observations. The model was used to produce a map of average annual runoff for Norway for the period 1961-1990.</p> <p style='line-height: 20px;'><b>Keywords: </b>distributed model, multi-criteria calibration, global parameters, ungauged catchments.
url http://www.hydrol-earth-syst-sci.net/7/304/2003/hess-7-304-2003.pdf
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