18 hydrolink number 1/ 2020 Coastal zones are exposed to a series of haz- ards, such as sea-level rise (SLR) and intensi- fied storminess [1] , which are estimated to increase due the effects of the climate change. According to IPCC [2] , the sea water level has been rising about 3.2 mm/year since 1993 - three times faster than the rates observed over most of the 20 th century! - and this increase is expected to continue. At the same time, popu- lation in coastal zones is expected to grow into the future [3] . This is true especially in low eleva- tion coastal zones (LECZs) - areas contiguous with the coast that are 10 m or less in elevation - where population will grow from 625 million to nearly a billion people by 2060 [4] , 56 million of which in Europe. Two-thirds of world’s largest cities are located in LECZs; in Europe, urban areas represent actually the 40% of the popula- tion in LECZs, values that will reach the 58% by 2060. Will coastal cities and urban areas in LECZs survive the SLR and flood events in the near future? How much the risk for people living in LECZs will increase? How to tackle it? Over the last century, the growing number of extra- tropical cyclones led to more frequent and dis- astrous flooding events: waves overtopped and breached coastal defences, causing major economic damages and loss of life. The “1953 North Sea flood” was one of these events, con- sidered the worst natural disaster of the 20 th century in The Netherlands, the U.K. and Bel- gium, recording over 2,500 lives and widespread property damage (around 10,000 buildings were destructed). Unfortunately, simi- lar severe storms are likely to occur again as a result of climate change. A clear evidence is the intensive stormy weather that is affecting Eu- rope over the last 10 years (e.g. the “2013–14 Atlantic winter storms”), causing severe flood- ing and casualties from Scotland to Spain, from Sweden to Poland (Figure 1). Very recently, be- tween January and February 2017, storms char- acterized by exceptional wave heights (>6-7m) hit the southern coast of Spain, washing away entire parts of the coastal protections and causing major damages (≈36.131.000€) to ports, promenades and other infrastructure. Under these scenarios, the performance of coastal defences in the next 20-100 years will become increasingly important to prevent flooding due to extreme overtopping events. Recently the DURCWAVE project (https:/ cordis.europa.eu/project/id/792370) was granted within the European Union’s Horizon 2020 research and innovation programme DURCWAVE “AMENDING THE DESIGN CRITERIA OF URBAN DEFENCES IN LECZS THROUGH COMPOSITE-MODELLING OF WAVE OVERTOPPING UNDER CLIMATE CHANGE SCENARIOS” BY XAVIER GIRONELLA & CORRADO ALTOMARE Figure 1. Examples of winter storms that struck the northern Europe over the last 6 years (a & b) and damages to the sea frontages (c & d) under the Marie Sklodowska-Curie (grant agreement No 792370). The project is ongoing at the Maritime Engineering Laboratory of Uni- versitat Politecnica de Catalunya-BarcelonaT- ech (LIM/UPC). Its scope is to contribute to long term solutions to cope with climate change in terms of requirements regarding coastal safety for LECZs. The main scientific objective of DURCWAVE project is to define new design criteria for wave action by modelling wave overtopping and post-overtopping processes of these urban de- fences. Specific objectives (SOs) are defined as follows: 1. To study post-overtopping processes by characterising overtopping flows on urban defences. 2. To explore the influence of structural geome- tries on post-overtopping processes. 3. To relate overtopping flow characteristics to maximum exerted loads. 4. To determine the most appropriate overtop- ping flow characteristics in terms of design purposes. 5. To define new design criteria for overtopping wave action as upgrade of European Stan- dards. To reach these objectives, the project is imple- menting a composite-modelling approach: physical modelling (hereafter “PM”) and numer- ical modelling (hereafter “NM”) are combined and applied to wave overtopping and overtop- ping loading assessment. The complementary use of PM and NM is essential since each ap- proach counterbalances the drawbacks of the other. On the one hand, PM is an established and reliable method for studying wave loads and wave overtopping of arbitrary coastal struc- tural geometries. However, PM is often a costly and time-consuming solution with further practi- cal shortcomings due to limitations in measure- ment techniques. On the other hand, NM is less restrictive in structure configurations and provides much more detailed information on the overtopping and post-overtopping flows (velocities, pressures, forces and overtopping CLIMATE CHANGE ADAPTATION AND COUNTERMEASURES IN COASTAL ENVIRONMENTS