In order to reconstruct the late Pleistocene-Holocene sea-level rise along the Eastern Adriatic Coast, eight speleothems were collected from three submerged caves along the Croatian coast from depths of ร38.5 to ร17 m. The marine biogenic overgrowth layer and the youngest and the oldest parts of the
GIS simulations of the inundation risk in the coastal lowlands of the Northern Adriatic Sea
โ Scribed by G. Gambolati; P. Teatini; M. Gonella
- Publisher
- Elsevier Science
- Year
- 2002
- Tongue
- English
- Weight
- 1008 KB
- Volume
- 35
- Category
- Article
- ISSN
- 0895-7177
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โฆ Synopsis
The Northern Adriatic Coastland, between the cities of Monfalcone and Cattolica, is characterized by locations of great tourist interest, such as the Venice Lagoon and the Romagna Riviera, and areas with a very precarious environmental setting, such as the Valli di Comacchio and the Po River Delta. Therefore, the coastal management and the design of new defence works of the littoral have to be made with the utmost care, possibly with the aid of numerical predictions of the coastal morphodynamics and the flood risk analysis of the lowland involved. In the study area, land may subside due to sediment naturM compaction and subsurface fluid (water and gas) withdrawal. At the same time, littoral transport of solid material can contribute appreciably to change the shore morphology. Mean sea level may rise permanently due to global climate change (eustatism) and occasionally due to tides and intensive storm events. The predictions of each individual process is obtained using various ad hoc mathematical models and the outcome of the numerical simulations are managed with a GIS (geographical information system). Coastline evolution until the year 2100 is investigated and risk factor maps of the low-lying coastal areas are generated which account for the hazard of the expected event, and the land economic value and vulnerability.
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