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Establishing a sediment budget in the newly created “Kleine Noordwaard” wetland area in the Rhine–Meuse delta

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Academic year: 2020

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Figure

Figure 1. The study area of the Kleine Noordwaard, which is located within the Biesbosch tidal freshwater wetland, in the lower Rhine–the period beforeMeuse delta in the southwest of the Netherlands (a, b)
Figure 2. Elevation of Transect A (see Fig. 1) with respect to the Dutch Ordnance Datum (m NAP) with subdivision of the area into subtidalareas, flats, low and high marshes, and terrestrial zone relative to mean low water (MLW), mean sea level (MSL), mean high water (MHW),the maximum observed water level (EHW) and the water level for a peak discharge or storm with return period of 1 year, which were usedto divide the study area in.
Figure 3. The difference in channel bed level and the cumulative channel bed volume for each monitoring period
Figure 4. Bed level of channel section 1 (a) and 3 (b) for all moni-toring campaigns (see Fig
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