The rural district of Aurich in Lower Saxony is the northernmost district of Germany, bordering the Netherlands and the North Sea. Its natural environment is characterised by the Wadden Sea, by three islands off the coast and by more than 70km of coastline.
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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
Šibenik-Knin County in Croatia has 960 km of coast and 285 islands and rocks. Its coastal zone consists of seven municipalities and three cities including Šibenik, the administrative centre.
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.
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.
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 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.