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Weichselian permafrost depth in the Netherlands: a comprehensive uncertainty and sensitivity analysis

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Academic year: 2017

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Table 1. Properties of the different components of the subsoil.
Figure 1. Structural elements in the Dutch subsur- subsur-face. LBH = Limburg High, RVG = Ruhr Valley Graben, KempH = Kempisch High, ZH = Zeeland High, OHP = Oosterhout Platform, PMC = Peel-Maasbommel, PMC_zuid =  Peel-Maasbommel High, WNB = West Netherlan
Figure 2. (a) Averaged mid-depth porosity variability of the post-Rupelian overburden, (b) distribution of the average sand content in the post-Rupelian overburden, (c) depth of the top of the Rupel Formation, also representing the thickness of the overbur
Figure 3. Top: best estimate temperature evolution for the We- We-ichselian glaciation, which is taken as an analogue for a future glacial climate in permafrost calculations
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