“…This region has gained significant interest for deep geothermal exploration due to its increased geothermal gradient, for example around Soultz-sous-Forêts, Landau, and Bruchsal (Agemar et al, 2013(Agemar et al, , 2014Illies, 1972;Pauwels et al, 1993;Geothermie, 2007;Vidal et al, 2015). However, obtaining reliable spatial temperature distributions is a major challenge as seen in the ongoing discussion in literature (Agemar et al, 2013(Agemar et al, , 2014Freymark et al, 2017Freymark et al, , 2019GeORG-Projektteam, 2013;Stober & Bucher, 2015), also because of the unclear influence of advection on the temperature distribution within the Upper Rhine Graben. So far, only "trial-and-error" model calibrations have been performed in basin-scale models of this region (Freymark et al, 2017).…”