Titlebook: CENAS; Coastline Evolution Giuseppe Gambolati Book 1998 Springer Science+Business Media Dordrecht 1998 Deltas.Erosion.Groundwater.environm

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Wave refraction in the Upper Adriatic Sea,based on observations. These observations were done at two different platforms with a water depth of 26 and 50 m. The recording period for wave directions and wave periods differs considerably. A representative wave climate for the 30 m depth contour line was created from these measurements in order

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Storm Wave Simulation in the Adriatic Sea,0 and 100 year storms are estimated. Each of these storms is simulated for the bathymetry at present and in the year 2050 and 2100. The bathymetry changes due to subsidence and sea level rise. The extreme water level at the local site of Ravenna is used to determine the return period of the storm.

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Coastal Morphodynamics in Subsiding Areas, that the coastal erosion, which is observed at almost all investigated sites, can be reduced considerably, or even disappear completely if no subsidence occurred. The problems associated with subsidence are mainly of local character. The general pattern of coastal erosion in the region must be subs

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Local Morphological Evolution of the Coast in the Upper Adriatic Sea. Design and Management Stratege in determining coastal stability and the results of the macro and local scale flood risk analysis. The last two parts list the various territory management strategies which may be adopted through medium-to-long-term planning or short-term actions for the purpose of limiting the subsidence caused b

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0921-092X over the geological scale but also in historical and modern times. According to some Authors the Venice Lagoon was formed 2000-3000 years ago, and other lagoons (e. g. the Grado Lagoon in the northernmost part of the Adriatic) are even more recent. In addition to lagoons, the Upper Adriatic coastal

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