Coastal regions belong to the most densely populated areas worldwide. According to the UN, ∼40% of the world's population lives within 100 km of the coast (UNEP, 2021). Coastal aquifers serve as a major water resource in these regions and are often characterized by low ground levels as well as anthropogenic activities impacting the local water cycle, for example, dense drainage networks and high water demands related to agriculture, industries and domestic use (Michael et al., 2017).At the same time, the projected climate change leads to a general increase in mean sea level and the possibility for enhanced storminess (IPCC, 2019). Combined, these circumstances put coastal groundwater systems at high risk with regard to saltwater intrusion (Werner et al., 2013). A natural rise of groundwater tables would accompany a rising sea level and antagonize saltwater intrusion. However, this will not occur in most low-lying coastal regions, because ∼70% of the global coasts are characterized as head/topography-controlled (Michael et al., 2013), either by low ground levels, artificial drainage measures, groundwater abstraction or a combination of these factors. Consequently, the landward head gradient increases, resulting in even more pronounced groundwater salinization (abbreviated as "salinization" in the following) (