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  5. New insights on the tsunami recording of the May, 21, 2003, Mw 6.9Boumerdès earthquake from tidal data analysis
 
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New insights on the tsunami recording of the May, 21, 2003, Mw 6.9Boumerdès earthquake from tidal data analysis

Author(s)
Vecchio, A.  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia  
Anzidei, M.  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia  
Carbone, V.  
Dipartimento di Fisica, Università della Calabria, Italy  
Language
English
Obiettivo Specifico
3T. Pericolosità sismica e contributo alla definizione del rischio
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Journal
Journal of geodynamics  
Issue/vol(year)
/79 (2014)
ISSN
0264-3707
Publisher
Elsevier Science Limited
Pages (printed)
39-49
Date Issued
2014
DOI
10.1016/j.jog.2014.05.001
URI
https://www.earth-prints.org/handle/2122/9690
Subjects
04. Solid Earth::04.06. Seismology::04.06.09. Waves and wave analysis  
Subjects

tsunami, algeria, bou...

Abstract
We analyzed sea level data from a set of tide gauge stations located in the central and western Mediter-ranean Sea, that recorded the tsunami generated by the Mw 6.8 Boumerdès earthquake striking the coastof Algeria on May 21, 2003. This earthquake caused more than 2200 victims and thousands of injured. Thecausative fault was located a few kilometers offshore and during the rupture a tsunami was triggered.Waves were felt along a large part of the western and northern Mediterranean coasts, and in the Balearicislands waves higher that 2 m were measured. In this paper we analyze a more complete tidal data set,with respect to previous studies, now consisting of 22 tidal stations located in Italy, France and Spain. Tocharacterize the change of the tidal signal at each station we used the Empirical Mode Decomposition(EMD). By means of this technique, which is suitable to analyze and to characterize the dynamical behav-ior of non-stationary time series, we provide a precise measurement of the arrival times and amplitudesat the tidal stations and identify how this tsunami affected the principal and long term tidal components.Our findings improve previous results for this earthquake, since they allow the detection of significantamplitude fluctuations associated with the tsunami in the majority of stations, including the farthestones.
Type
article
File(s)
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vecchio et al boumerdes_JGeoDin_2014.pdf

Size

2.04 MB

Format

Adobe PDF

Checksum (MD5)

1bb5dd9982411ec978349a857f76788b

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