Vulnerability of the Atlantic Patagonian coast to tsunamis generated by submarine earthquakes located in the Scotia Arc region. Some numerical experiments
The Scotia Arc is one of two regions in the Atlantic Ocean with greater potential for tsunami generation from seismic and volcanic sources. A numerical modeling study was undertaken to determine tsunami generation from postulated sources along the Arc and tsunami wave amplification or attenuation al...
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| Formato: | Capítulo de libro |
| Lenguaje: | Inglés |
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2009
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| LEADER | 17796caa a22013817a 4500 | ||
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| 001 | PAPER-9025 | ||
| 003 | AR-BaUEN | ||
| 005 | 20250306092126.0 | ||
| 008 | 190411s2009 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-67349172172 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Dragani, W.C. | |
| 245 | 1 | 0 | |a Vulnerability of the Atlantic Patagonian coast to tsunamis generated by submarine earthquakes located in the Scotia Arc region. Some numerical experiments |
| 260 | |c 2009 | ||
| 270 | 1 | 0 | |m Dragani, W.C.; Departamento Oceanografía, Servicio de Hidrografía Naval, ESCM-INUN, Av. Montes de Oca 2124, C1270ABV Buenos Aires, Argentina; email: dragani@hidro.gov.ar |
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| 506 | |2 openaire |e Política editorial | ||
| 520 | 3 | |a The Scotia Arc is one of two regions in the Atlantic Ocean with greater potential for tsunami generation from seismic and volcanic sources. A numerical modeling study was undertaken to determine tsunami generation from postulated sources along the Arc and tsunami wave amplification or attenuation along the Patagonian continental shelf. Sea level oscillation represented by a simple sinusoidal wave function applied at the boundary of the numerical grid, which simulated the tsunami entering the computational domain, was implemented as forcing. The validation of this model was carried out by comparing the maximum amplitudes recorded and simulated at Santa Teresita and Mar del Plata (Buenos Aires province) after the occurrence of earthquake and subsequent tsunami in Sumatra (December 2004). From numerical simulations it can be seen that the tsunami propagation is highly affected by bathymetric refraction on the Patagonian continental shelf and the wave amplitude is significantly attenuated on the inner continental shelf. Maximum amplifications were obtained around Malvinas (Falkland) Islands and Burdwood bank because the wave propagates almost without refracting and the shoaling effect is highly significant there. © Springer Science+Business Media B.V. 2008. |l eng | |
| 536 | |a Detalles de la financiación: Consejo Nacional de Investigaciones Científicas y Técnicas | ||
| 536 | |a Detalles de la financiación: Consejo Nacional de Investigaciones Científicas y Técnicas | ||
| 536 | |a Detalles de la financiación: W. C. Dragani (&) · E. E. D’Onofrio · W. Grismeyer · M. M. E. Fiore · R. A. Violante Departamento Oceanografía, Servicio de Hidrografía Naval and ESCM-INUN, Av. Montes de Oca 2124 (C1270ABV) Ciudad Autónoma de Buenos Aires, Buenos Aires, Argentina e-mail: dragani@hidro.gov.ar W. C. Dragani · E. E. D’Onofrio · M. M. E. Fiore Departamento Ciencias de la Atmósfera y los Océanos, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, (1428) Ciudad Universitaria, Pabellón II, 2do. piso, Ciudad Autónoma de Buenos Aires, Buenos Aires, Argentina W. C. Dragani CONICET, Consejo Nacional de Investigaciones Científicas y Técnicas, Av. Rivadavia 1917 (C1033AAJ) Ciudad Autónoma de Buenos Aires, Buenos Aires, Argentina E. E. D’Onofrio Facultad de Ingeniería, Instituto de Geodesia, Universidad de Buenos Aires, Av. Las Heras 2214, (1127) Ciudad Autónoma de Buenos Aires, Buenos Aires, Argentina E. I. Rovere Geología Regional, Servicio Geológico Minero Argentino, Av. Julio A. Roca 651 (1067) Ciudad Autónoma de Buenos Aires, Buenos Aires, Argentina | ||
| 593 | |a Departamento Oceanografía, Servicio de Hidrografía Naval, ESCM-INUN, Av. Montes de Oca 2124, C1270ABV Buenos Aires, Argentina | ||
| 593 | |a Departamento Ciencias de la Atmósfera y los Océanos, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Pabellón II, 2do. piso, Buenos Aires, Argentina | ||
| 593 | |a CONICET, Consejo Nacional de Investigaciones Científicas y Técnicas, Av. Rivadavia 1917, C1033AAJ Buenos Aires, Argentina | ||
| 593 | |a Facultad de Ingeniería, Instituto de Geodesia, Universidad de Buenos Aires, Av. Las Heras 2214, 1127 Buenos Aires, Argentina | ||
| 593 | |a Geología Regional, Servicio Geológico Minero Argentino, Av. Julio A. Roca 651, 1067 Buenos Aires, Argentina | ||
| 651 | 4 | |a ARGENTINA | |
| 651 | 4 | |a BUENOS AIRES [ARGENTINA] | |
| 651 | 4 | |a SOUTH AMERICA | |
| 690 | 1 | 0 | |a ARGENTINEAN CONTINENTAL SHELF |
| 690 | 1 | 0 | |a NUMERICAL SIMULATION |
| 690 | 1 | 0 | |a OCEANOGRAPHY |
| 690 | 1 | 0 | |a SCOTIA ARC |
| 690 | 1 | 0 | |a TSUNAMI |
| 690 | 1 | 0 | |a BATHYMETRY |
| 690 | 1 | 0 | |a CONTINENTAL SHELF |
| 690 | 1 | 0 | |a EARTHQUAKE MECHANISM |
| 690 | 1 | 0 | |a NUMERICAL MODEL |
| 690 | 1 | 0 | |a SEISMIC SOURCE |
| 690 | 1 | 0 | |a TSUNAMI |
| 690 | 1 | 0 | |a VULNERABILITY |
| 690 | 1 | 0 | |a WAVE ATTENUATION |
| 690 | 1 | 0 | |a WAVE GENERATION |
| 690 | 1 | 0 | |a WAVE PROPAGATION |
| 690 | 1 | 0 | |a ANTARCTICA |
| 690 | 1 | 0 | |a ATLANTIC OCEAN |
| 690 | 1 | 0 | |a BURDWOOD BANK |
| 690 | 1 | 0 | |a MAR DEL PLATA |
| 690 | 1 | 0 | |a PATAGONIAN SHELF |
| 690 | 1 | 0 | |a SCOTIA ARC |
| 700 | 1 | |a D'Onofrio, Enrique Eduardo | |
| 700 | 1 | |a Grismeyer, W. | |
| 700 | 1 | |a Fiore, M.M.E. | |
| 700 | 1 | |a Violante, R.A. | |
| 700 | 1 | |a Rovere, E.I. | |
| 773 | 0 | |d 2009 |g v. 49 |h pp. 437-458 |k n. 3 |p Nat. Hazards |x 0921030X |t Natural Hazards | |
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