Storm Surge Simulations in the Adriatic Sea

作者: C. S. Yu , C. Decouttere , J. Berlamont

DOI: 10.1007/978-94-011-5147-4_10

关键词:

摘要: A storm surge prediction model has been constructed for simulating seven historical storms in the Adriatic Sea. The which could cause highest levels at Ravenna coast chosen as a reference studying combined effects on this area of various regional topographical changes, sea-level rises and future events. These events have generated by increasing wind intensity weather pattern. Storm surges simulated with scenarios obtained from combinations bathymetry changes different intensities. Wind found to most significant influence future. Topographic due land subsidence rise very minor influences net residuals Due bathymetric nature Sea, residual can be slightly lower water depth (e.g. rise) Northern Adriatic.

参考文章(13)
C. Decouttere, K. De Backer, J. Monbaliu, J. Berlamont, Storm Wave Simulation in the Adriatic Sea CENAS. pp. 185- 205 ,(1998) , 10.1007/978-94-011-5147-4_9
J.G. de Ronde, G.K. Verboom, R.P. van Dijk, Een model van het Europese Kontinentale Plat voor windopzet en waterkwaliteitsberekeningen Z 96.00 GWAO-87.021. ,(1987)
Jin Wu, Wind stress and surface roughness at air‐sea interface Journal of Geophysical Research. ,vol. 74, pp. 444- 455 ,(1969) , 10.1029/JB074I002P00444