The paper investigates on the hydro-acoustic waves propagation caused by the underwater earthquake, occurred on 6 February 2012, between the Negros and Cebu islands, in the Philippines. Hydro-acoustic waves are pressure waves that propagate at the sound celerity in water. These waves can be triggered by the sudden vertical sea-bed movement, due to underwater earthquakes. The results of three dimensional numerical simulations, which solve the wave equation in a weakly compressible sea water domain are presented. The hydro-acoustic signal is compared to an underwater acoustic signal recorded during the event by a scuba diver, who was about 12 km far from the earthquake epicenter.

Cecioni, C., Romano, A., Bellotti, G., De Girolamo, P. (2019). 3D numerical simulation of hydro-acoustic waves registered during the 2012 negros-cebu earthquake. GEOSCIENCES, 9(7), 300 [10.3390/geosciences9070300].

3D numerical simulation of hydro-acoustic waves registered during the 2012 negros-cebu earthquake

Cecioni C.;Romano A.;Bellotti G.;
2019-01-01

Abstract

The paper investigates on the hydro-acoustic waves propagation caused by the underwater earthquake, occurred on 6 February 2012, between the Negros and Cebu islands, in the Philippines. Hydro-acoustic waves are pressure waves that propagate at the sound celerity in water. These waves can be triggered by the sudden vertical sea-bed movement, due to underwater earthquakes. The results of three dimensional numerical simulations, which solve the wave equation in a weakly compressible sea water domain are presented. The hydro-acoustic signal is compared to an underwater acoustic signal recorded during the event by a scuba diver, who was about 12 km far from the earthquake epicenter.
2019
Cecioni, C., Romano, A., Bellotti, G., De Girolamo, P. (2019). 3D numerical simulation of hydro-acoustic waves registered during the 2012 negros-cebu earthquake. GEOSCIENCES, 9(7), 300 [10.3390/geosciences9070300].
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11590/360688
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