The UK is generally projected to experience increases in extremes of the precipitation regime as a result of climate change, especially in terms of higher occurrence and intensity of heavy summer rainfall events.
You are here
Case studies
Furthermore, in this publication you can find a selection of adaptation case studies with some of the most representative practices.
Note: The views and documentation provided in the case studies are the sole responsibility of the author(s) of the case studies.
Other Case studies
Klaipėda is a coastal city with almost all of its territory located on coastal lowland, and the Smeltalė river situated in the Southern part of the city, falling into the Curonian Lagoon within the city area.
The Sigma Plan is an integrated flood protection plan that was firstly established in 1977, in reaction to a major storm surge flood in 1976. The Sigma Plan offers protection against storm surges as well as river floods caused by excessive rainfall.
The Kruibeke Bazel Rupelmonde (KBR) Controlled Flood Area (CFA) is a key component of the Belgian Sigma Plan for the Scheldt Estuary.
At Nijmegen, the Waal River bends sharply and narrows. This creates a bottleneck, which often caused flooding of the historic city centre of Nijmegen, located on the south bank of the Wall.
The increasing exposure to floods is a consequence of the river regulation and land reclamation works that shaped the landscape in the Tisza River floodplain.
Climate change impact assessment has been an integrated part of the design and planning of the Copenhagen metro since the first metro line was designed in the mid-1990s.
Titchwell Marsh lies towards the western end of the North Norfolk coast in UK. It forms a key part of the North Norfolk Coast Special Protection Area (SPA) and Special Area of Conservation (SAC). The freshwater and brackish habitats at Titchwell are protected by seawalls.
The Alfacada and Tancada coastal lagoons are located in the Delta del Ebro Natural Park. The lagoons are vulnerable to the effects of climate change, particularly sea level rise, in combination with sediment deficit due to river regulation, leading to exacerbated coastal erosion and subsidence.