Hydrological response to climate change in the Lesse and the Vesdre catchments: Contribution of a physically based model (Wallonia, Belgium)

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Abstract

The Meuse is an important rain-fed river in North-Western Europe. Nine million people live in its catchment, split over five countries. Projected changes in precipitation and temperature characteristics due to climate change would have a significant impact on the Meuse River and its tributaries. In this study, we focused on the impacts of climate change on the hydrology of two sub-catchments of the Meuse in Belgium, the Lesse and the Vesdre, placing the emphasis on the water-soil-plant continuum in order to highlight the effects of climate change on plant growth, and water uptake on the hydrology of two sub-catchments. These effects were studied using two climate scenarios and a physically based distributed model, which reflects the water-soil-plant continuum. Our results show that the vegetation will evapotranspirate between 10 and 17 % less at the end of the century because of water scarcity in summer, even if the root development is better under climate change conditions. In the low scenario, the mean minimal 7 days discharge value could decrease between 19 and 24 % for a two year return period, and between 20 and 35 % for a fifty year return period. It will lead to rare but severe drought in rivers, with potentially huge consequences on water quality. © 2011 Author(s).

Figures

  • Fig. 1. The Meuse catchment (light grey) in Wallonia (Belgium) and the Vesdre and the Lesse catchments (dark grey).
  • Table 1. Distribution of soil classes (%) for the Lesse and the Vesdre catchments, based upon the Belgian simplified pedological map at 1/50 000.
  • Fig. 2. Simulation structure of the EPICGrid model inside an elementary element.
  • Fig. 3. CCI-HYDR high (blue) and low (green) scenarios for 2020–2050 (light colors) and 2070–2100 (dark colors) vs. PRUDENCE RCM simulation for 2071–2100 (black and grey curves) (de Wit et al., 2007). (a) Precipitation changes in %, (b) temperature changes in ◦C.
  • Table 2. CCI-HYDR impact scenarios and related changes in precipitation, temperature, ET0 and wind (Baguis et al., 2009).
  • Fig. 4. Evolution of monthly flow during a year for the Vesdre at Chaudfontaine (upper panel) and the Lesse at Gendron (lower panel). The shaded areas represent the standard deviation for the reference period. Minimun and maximum represent the minimum and maximum values simulated during the reference period.
  • Fig. 6. Water balance for the Vesdre and the Lesse sub-catchments for the different scenarios and time slices.
  • Table 3. Comparison between observed and simulated MAM7 during reference period and changes in MAM7 values for the Vesdre at Chaudfontaine (left) and the Lesse at Gendron (right) for different return periods (T ).

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APA

Bauwens, A., Sohier, C., & Degré, A. (2011). Hydrological response to climate change in the Lesse and the Vesdre catchments: Contribution of a physically based model (Wallonia, Belgium). Hydrology and Earth System Sciences, 15(6), 1745–1756. https://doi.org/10.5194/hess-15-1745-2011

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