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

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Storm Wave Simulation in the Adriatic Sea, a steady south-easterly wind, which lasts for a few days. In the northern part of the sea, this results in powerful swell waves. They are very important for morphological effects during such a storm. The WAM wave model is used to hindcast the wave field during one of the historical Scirocco storms

Coordinate

JEER

Coastal Morphodynamics in Subsiding Areas,f relative sea level changes and external sediment sources such as fluvial sediment input and nourishments are included in the analysis. Prior to the coastline evolution studies, a baseline study was performed where the different process parameters of the coastal sediment balance have been identifie

Frequency-Range

Local Morphological Evolution of the Coast in the Upper Adriatic Sea. Design and Management Strategmulations conducted under the CENAS Project, regarding the morphological evolution of the coastline. The first part of the paper describes the local evolution around offshore breakwaters from a qualitative point of view. The accumulation rates related to waves, tides and longshore currents behind of

Affiliation

Geographic Information System (GIS) and Data Management and Retrieval System (DMRS) in the CENAS Pr CENAS have been organized in an “overall data management environment” developed in the course of the project. The structure of the environment is divided into two main modules: a Geographic Information System (GIS) and a Data Management and Retrieval System (DMRS). Manipulation of site-specific ras

WAX

Flood Risk Analysis in the Upper Adriatic Sea due to Storm Surge, Tide, Waves, and Natural and Antheltas) with a precarious hydrogeological features. In the years to come the setting of these zones will become more critical due to a relative sea level rise caused by global climate warming and natural and anthropic land subsidence, and increased mean sea level due to severe meteo-marine storms. Th

Iniquitous

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978-94-010-6163-6Springer Science+Business Media Dordrecht 1998

exophthalmos

abject

https://doi.org/10.1007/978-3-658-44709-0has 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