| Tag |
First Indicator |
Second Indicator |
Subfields |
| LEADER |
00000cam a2200000Ma 4500 |
| 001 |
in00003545679 |
| 006 |
m o d |
| 007 |
cr nn||||||||| |
| 008 |
121227s1998 ne o 000 0 eng d |
| 005 |
20260420210851.3 |
| 020 |
|
|
|a 9789401151474 (electronic bk.)
|
| 020 |
|
|
|a 9401151474 (electronic bk.)
|
| 035 |
|
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|a (OCoLC)840311130
|
| 040 |
|
|
|a I9W
|b eng
|e pn
|c I9W
|d OCLCO
|d OCLCQ
|d GW5XE
|d OCLCF
|d OCLCO
|d UtOrBLW
|
| 049 |
|
|
|a TXAM
|
| 050 |
|
4 |
|a GB457.71
|
| 082 |
0 |
4 |
|a 551.45/7/0916385
|2 21
|
| 100 |
1 |
|
|a Gambolati, G.
|q (Giuseppe)
|
| 245 |
1 |
0 |
|a CENAS :
|b Coastline Evolution of the Upper Adriatic Sea due to Sea Level Rise and Natural and Anthropogenic Land Subsidence /
|c edited by Giuseppe Gambolati.
|
| 264 |
|
1 |
|a Dordrecht :
|b Springer Netherlands,
|c 1998.
|
| 300 |
|
|
|a 1 online resource (360 pages)
|
| 336 |
|
|
|a text
|b txt
|2 rdacontent
|
| 337 |
|
|
|a computer
|b c
|2 rdamedia
|
| 338 |
|
|
|a online resource
|b cr
|2 rdacarrier
|
| 490 |
1 |
|
|a Water Science and Technology Library, 0921-092X ;
|v 28
|
| 520 |
|
|
|a 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. <br/> 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. <br/> 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.
|
| 500 |
|
|
|a Electronic resource.
|
| 650 |
|
0 |
|a Coast changes
|z Adriatic Sea Region.
|
| 650 |
|
0 |
|a Sea level
|z Adriatic Sea Region.
|
| 650 |
|
0 |
|a Subsidences (Earth movements)
|z Adriatic Sea Region.
|
| 650 |
|
7 |
|a Coast changes.
|2 fast
|0 (OCoLC)fst00865699
|
| 650 |
|
7 |
|a Sea level.
|2 fast
|0 (OCoLC)fst01110054
|
| 650 |
|
7 |
|a Subsidences (Earth movements)
|2 fast
|0 (OCoLC)fst01136712
|
| 651 |
|
7 |
|a Europe
|z Adriatic Sea Region.
|2 fast
|0 (OCoLC)fst01724861
|
| 655 |
|
7 |
|a Electronic books.
|2 local
|
| 710 |
2 |
|
|a SpringerLink (Online service)
|
| 830 |
|
0 |
|a Water science and technology library ;
|v 28.
|
| 856 |
4 |
0 |
|u http://proxy.library.tamu.edu/login?url=https://link.springer.com/10.1007/978-94-011-5147-4
|z Connect to the full text of this electronic book
|t 0
|
| 994 |
|
|
|a 92
|b TXA
|
| 999 |
|
|
|a MARS
|
| 999 |
f |
f |
|s 0770215d-1ec7-3e47-9f45-55859fbd182c
|i 2649524a-88cc-31bc-b9c0-0e0798974bc2
|t 0
|
| 952 |
f |
f |
|a Texas A&M University
|b College Station
|c Electronic Resources
|s www_evans
|d Available Online
|t 0
|e GB457.71
|h Library of Congress classification
|
| 998 |
f |
f |
|a GB457.71
|t 0
|l Available Online
|