CENAS

Name: CENAS
Brand: Springer
SKU: 9789401061636
Price: 895.27 RON
Availability: InStock

Coastline Evolution of the Upper Adriatic Sea due to Sea Level Rise and Natural and Anthropogenic Land Subsidence

Autor: Giuseppe Gambolati

Limbă:

Legare: Carte broșată

Editura: Springer

Disponibilitate: În depozitul extern în cantități mici

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895.27 lei

The CENAS Project funded by the EU as part of the Environmental Programme 1990-1994 addresses the is...

Informații despre carte

Autor

Giuseppe Gambolati

Limbă

engleză

Legare

Carte - Carte broșată

Publicat

2013

Pagini

346

EAN

9789401061636

ISBN

9401061637

Enbook ID

02191014

Editura

Springer

Greutate

581

Dimensiuni

160 x 240 x 20

Descriere completă

The CENAS Project funded by the EU as part of the Environmental Programme 1990-1994 addresses the issue of the coastland evolution of the Eastern Po Plain and future stability of the Upper Adriatic coastline in relation to mean sea level rise, natural and anthropogenic land subsidence, severe meteo-marine events and reduced sediment inflow from the watercourses. The huge amount of information needed to perform the study and the numerical models developed to make predictions of the various events are integrated into and handled by a Geographical Information System (GIS) combined with a DMRS (Data Management and Retrieval System) and a DEM (Digital Elevation Model) of the area of interest. §Numerical modelling predictions up to 2100 of the major processes which may impact on the Upper Adriatic morphodynamics point out the precariousness of this coastal environment, especially south of the Po river delta where much of the present lowland is expected to be submerged by the end of the next century and most of the area flooded during a storm with only a one-year return period. §The integrated modelling approach used in the CENAS Project is believed to be a good example of morphodynamical analysis that may be extended to other coastal areas of the world.

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CENAS

Coastline Evolution of the Upper Adriatic Sea due to Sea Level Rise and Natural and Anthropogenic Land Subsidence

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