Globally, floods are the most common natural hazard and have major economic, social, and ecological impacts on communities (CRED & UNISDR, 2015). Coastal river areas concentrate population, infrastructure, and economic activity, all of these highly vulnerable to floods (Koks et al., 2015). The effects of global warming in such already flood-prone areas raise concerns about future flood conditions, making imperative the need for reliable methods for their analysis (Seneviratne et al., 2012) and innovative approaches to their planning and management. These challenges, however, have been insufficiently addressed by regulations and policies. In the European Union (EU), the EU Floods Directive (2007/60/CE) and the Water Framework Directive (2000/60/ EC) establish the framework for assessing and managing flood risks. It defines a cycle that includes a preliminary assessment to identify areas at risk of flooding, the creation of flood hazard and risk maps, and the establishment of flood risk management plans focused on prevention, protection, and preparedness. It also establishes that these steps need to be reviewed every 6 years, and acknowledges the need to take into account the likely impact of climate change on the magnitude and frequency of floods. The European Water Framework Directive does not go beyond these procedural obligations, leaving open the question as to which methodological approaches are most appropriate for such flood risk assessments.The prediction of flooding in coastal river areas is not an easy task due to the complexity and interaction of the underlying physical processes. Elevated water levels in coastal reaches originate from the interaction of several coastal and inland drivers, such as storm surge and river discharge. These flood drivers are often not independent since they share a common meteorological forcing. For example, the combined effects of low atmospheric pressure and strong winds associated with synoptic-scale storms can induce storm surges along the coast. Concurrently, or in close succession, heavy precipitation increases freshwater runoff, and as a result leads to high river discharge. Elevated sea levels can block or slow down river drainage into the sea, leading to increased upstream water levels. Compared to flood events caused by a single driver, compound floods can usually be expected to yield higher impacts, as evidenced, for example, in the recent floods in Ravenna (Italy) (Bevacqua et al., 2017) or in the Hurricane Harvey Flood in Houston Area (Valle-Levinson