Historical trends in precipitation and stream discharge at the Skjern River catchment, Denmark

A 133 yr data set from the 1055 km<sup>2 </sup>Skjern River catchment in western Denmark has been analysed with respect to precipitation, temperature, evapotranspiration and discharge. The precipitation series have been tested and corrected using the standard normal homogeneity test and...

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Main Authors: I. B. Karlsson, T. O. Sonnenborg, K. H. Jensen, J. C. Refsgaard
Format: Article
Language:English
Published: Copernicus Publications 2014-02-01
Series:Hydrology and Earth System Sciences
Online Access:http://www.hydrol-earth-syst-sci.net/18/595/2014/hess-18-595-2014.pdf
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spelling doaj-d234424d139247808ebbcbc5d437f4952020-11-24T21:07:22ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382014-02-0118259561010.5194/hess-18-595-2014Historical trends in precipitation and stream discharge at the Skjern River catchment, DenmarkI. B. Karlsson0T. O. Sonnenborg1K. H. Jensen2J. C. Refsgaard3Geological Survey of Denmark and Greenland (GEUS), Copenhagen, DenmarkGeological Survey of Denmark and Greenland (GEUS), Copenhagen, DenmarkCopenhagen University – Department of Geosciences and Natural Resource Management, Copenhagen, DenmarkGeological Survey of Denmark and Greenland (GEUS), Copenhagen, DenmarkA 133 yr data set from the 1055 km<sup>2 </sup>Skjern River catchment in western Denmark has been analysed with respect to precipitation, temperature, evapotranspiration and discharge. The precipitation series have been tested and corrected using the standard normal homogeneity test and subsequently corrected for undercatch. The degree of change in the climatic variables is examined using the non-parametric Mann–Kendall test. During the last 133 yr the area has experienced a significant change in precipitation of 26% and a temperature change of 1.4&deg;C, leading to increases in river discharge of 52% and groundwater recharge of 86%. A lumped conceptual hydrological model, NAM, was calibrated on the period 1951–1980 and showed generally an excellent match between simulated and observed discharge. The capability of the hydrological model to predict climate change impact was investigated by looking at performances outside the calibration period. The results showed a reduced model fit, especially for recent time periods (after the 1980s), and not all hydrological changes could be explained. This might indicate that hydrological models cannot be expected to predict climate change impacts on discharge as accurately in the future, compared to the performance under present conditions, where they can be calibrated. The (simulated) stream discharge was subsequently analysed using high flow and drought indices based on the threshold method. The extreme signal was found to depend highly on the period chosen as reference to normal. The analysis indicated that no significant amplitude increase of the hydrograph for both wet and dry extremes could be found superimposed on the overall discharge increase.http://www.hydrol-earth-syst-sci.net/18/595/2014/hess-18-595-2014.pdf
collection DOAJ
language English
format Article
sources DOAJ
author I. B. Karlsson
T. O. Sonnenborg
K. H. Jensen
J. C. Refsgaard
spellingShingle I. B. Karlsson
T. O. Sonnenborg
K. H. Jensen
J. C. Refsgaard
Historical trends in precipitation and stream discharge at the Skjern River catchment, Denmark
Hydrology and Earth System Sciences
author_facet I. B. Karlsson
T. O. Sonnenborg
K. H. Jensen
J. C. Refsgaard
author_sort I. B. Karlsson
title Historical trends in precipitation and stream discharge at the Skjern River catchment, Denmark
title_short Historical trends in precipitation and stream discharge at the Skjern River catchment, Denmark
title_full Historical trends in precipitation and stream discharge at the Skjern River catchment, Denmark
title_fullStr Historical trends in precipitation and stream discharge at the Skjern River catchment, Denmark
title_full_unstemmed Historical trends in precipitation and stream discharge at the Skjern River catchment, Denmark
title_sort historical trends in precipitation and stream discharge at the skjern river catchment, denmark
publisher Copernicus Publications
series Hydrology and Earth System Sciences
issn 1027-5606
1607-7938
publishDate 2014-02-01
description A 133 yr data set from the 1055 km<sup>2 </sup>Skjern River catchment in western Denmark has been analysed with respect to precipitation, temperature, evapotranspiration and discharge. The precipitation series have been tested and corrected using the standard normal homogeneity test and subsequently corrected for undercatch. The degree of change in the climatic variables is examined using the non-parametric Mann–Kendall test. During the last 133 yr the area has experienced a significant change in precipitation of 26% and a temperature change of 1.4&deg;C, leading to increases in river discharge of 52% and groundwater recharge of 86%. A lumped conceptual hydrological model, NAM, was calibrated on the period 1951–1980 and showed generally an excellent match between simulated and observed discharge. The capability of the hydrological model to predict climate change impact was investigated by looking at performances outside the calibration period. The results showed a reduced model fit, especially for recent time periods (after the 1980s), and not all hydrological changes could be explained. This might indicate that hydrological models cannot be expected to predict climate change impacts on discharge as accurately in the future, compared to the performance under present conditions, where they can be calibrated. The (simulated) stream discharge was subsequently analysed using high flow and drought indices based on the threshold method. The extreme signal was found to depend highly on the period chosen as reference to normal. The analysis indicated that no significant amplitude increase of the hydrograph for both wet and dry extremes could be found superimposed on the overall discharge increase.
url http://www.hydrol-earth-syst-sci.net/18/595/2014/hess-18-595-2014.pdf
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