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Strong increases in flood frequency and discharge of the River Meuse over the late Holocene: impacts of long-term anthropogenic land use change and climate variability

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Academic year: 2021

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Table 3. Percentage change in mean annual (Q ann ), summer (Q sum ), and winter (Q win ) dis- dis-charge and various high-flow percentiles (Q k , k = 75, 90, 95, 99) between 4000–3000 BP and the 20th Century AD (above), and between the 19th and 20th Centur
Fig. 1. Map showing the location of the Meuse Basin and discharge measuring stations used in this study (after RWS Limburg/IWACO, 2000)
Fig. 2. Flowchart showing the main compartments and flows of the STREAM palaeodischarge model (Ward et al., 2007)
Fig. 3. Downscaled ECBilt-CLIO-VECODE climate data for the time-periods 4000–3000 BP and 1000–2000 AD
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