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Numerical modelling of climate change impacts on freshwater lenses on the North Sea Island of Borkum using hydrological and geophysical methods

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Figure

Fig. 1. Top panel: location map of study area, bottom panel: North Sea Island of Borkum with its two waterworks (WW): WW I Waterdelle2  and WW II Ostland and the two major rivers.
Fig. 2.Figure 2. Top panel: Annual delivery rates [1000 m³/a] for WW I (Waterdelle), blue bars, and  Top panel: Annual delivery rates [1000 m3 a−1] for WW I (Waterdelle), blue bars, and WW II (Ostland), dark red bars, bottom panel:monthly delivery rates for 2009.
Table 1. Transmissivity (T ) obtained from pumping tests. According to the configuration of the pumping test for all locations of the loggersin the draw down area with 2, 5, 10 m (and so on) distance to the pumping location, transmissivities T (2 m), T (5 m), T (10 m) (and so on)were computed and averaged to one transmissivity T at the pumping location.
Fig. 4.Figure 4. Observation points of electrical water conductivity (ec) and temperature at the  Observation points of electrical water conductivity (ec) and temperature at the surface of the groundwater table during June 2009 andMarch 2010, all 260 locations are represented.
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