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

anaerobic

Nahverkehrsbahnen der Grosst?dte subsidence and due to sea-level rise have very minor influences on the net surge residuals in the future. Due to the bathymetric nature of the Adriatic Sea, the surge residual can be slightly lower by increasing the water depth (. due to sea-level rise) in the Northern Adriatic.

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Prediction of Mean Sea Level Rise in the Upper Adriatic Sea,has been considered as the sum of the eustatic change (caused by . in the volume of ocean water for thermal expansion, . in the mass of ocean water, change in the volume of ocean basins and .) and the absolute land elevation change (caused by down-lift by regional and local subsidence, up- lift by t

得意人

Collection and analysis of historical data on shoreline evolution at the sites of Ravenna, Cesenati eustatism, storm-surges, natural subsidence, and subsidence caused by anthropic activity. The cities present various problems regarding the morphological evolution of the coastline. These problems are linked firstly to natural factors and secondly to the influence of various human activities relate

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Numerical Analysis of Land Subsidence due to Natural Compaction of the Upper Adriatic Sea Basin,atic coastline. The analysis is performed by a 1-D nonlinear finite element model of soil compaction driven by groundwater flow in an isothermal sedimentary basin subject to a continuous vertical sedimentation process. The constitutive relationship of the most important parameter controlling the eve

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人類(lèi)學(xué)家

Wave refraction in the Upper Adriatic Sea,d ray tracing refraction model LOMBOK is applied on a high resolution bathymetry in order to compute the annual inshore wave climate at the local sites of Ravenna, Rimini and Cesenatico. Wave observations from offshore platforms are used as model input. The refraction model brings the offshore wave