Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/2784
DC Field | Value | Language |
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dc.contributor.authorall | Cucci, L.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia | en |
dc.contributor.authorall | Tertulliani, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia | en |
dc.date.accessioned | 2007-11-09T08:49:25Z | en |
dc.date.available | 2007-11-09T08:49:25Z | en |
dc.date.issued | 2007-02 | en |
dc.identifier.uri | http://hdl.handle.net/2122/2784 | en |
dc.description.abstract | This paper describes the variation of the human perception of earthquakes under the peculiar condition of seismic sequence occurrence. To this aim, we chose and have analyzed four seismic sequences that reflect the most common models of seismicity occurrence in the Italian territory. Our data always refer to the epicentral area, so that the contribution of the epicentral distance to the earthquake sensitiveness is considered constant. To search for recurrent behavior of people in the perception of earthquakes, we crossed seismological data to sensitivity data coming from the archives of the Italian Civil Protection. In each sequence, we individuate a number of “indicators”, such as the rate between felt and not-felt events and the minimum magnitude for which 100% of the events are felt. Such indicators are proportional to the energy released by the sequence and can be particularly affected by the time protraction of the sequence, and/or by the different familiarity with the seismic phenomenon, and/or by the intensity of the emotional impact of a seismic crisis. The observed trends of sensitiveness show a significant variation of the people perceptivity within the sequence development. From the analysis of the dataset, one can distinguish the variation of perceptivity due to emotional factors from those due to physical factors. An important observation, which is confirmed by a statistical analysis, is that the source depth does not affect the perceptiveness of earthquakes. Finally, we find important differences between on-sequence and off-sequence human perceptiveness that are connected with the different levels of alert. | en |
dc.language.iso | English | en |
dc.publisher.name | Springer Science | en |
dc.relation.ispartof | Journal of Seismology | en |
dc.relation.ispartofseries | 11/2007 | en |
dc.subject | seismic sequence . magnitude . | en |
dc.subject | perceptiveness . human reaction | en |
dc.title | Variation of human perceptiveness of earthquakes during seismic sequences | en |
dc.type | article | en |
dc.description.status | Published | en |
dc.type.QualityControl | Peer-reviewed | en |
dc.description.pagenumber | 205–219 | en |
dc.identifier.URL | http://www.springerlink.com/content/91587544m7135r17/ | en |
dc.subject.INGV | 04. Solid Earth::04.06. Seismology::04.06.99. General or miscellaneous | en |
dc.identifier.doi | 10.1007/s10950-007-9048-0 | en |
dc.relation.references | Castello B, Selvaggi G, Chiarabba C, Amato A (2005) CSI Catalogo della sismicità italiana 1981–2002, versione 1.1. INGV-CNT. http://www.ingv.it/CSI//. Cited 25 Sep 2006 Celsi R, Wolfinbarger M, Wald D (2005) The effects of earthquakes measurement concepts and magnitude anchoring on individuals’ perceptions of earthquake risk. Earthq Spectra 21(4):987–1008 Dengler LA, Dewey JW (1998) An intensity survey of households by the Northridge, California, earthquake of 17 January 1994. Bull Seismol Soc Am 88:441–462 Di Maro R, Tertulliani A (1990) The relation between intensity and magnitude for Italian earthquakes. Pure Appl Geophys 132(4):711–718 Frankel A (1994) Implications of felt area–magnitude relations for earthquake scaling and the average frequency of perceptible ground motion. Bull Seismol Soc Am 84:462–465 Goldman DE, Gierke HE (1961) Effects of shock and vibration on man. In: Harris CM, Crede CE (eds) Shock and vibration handbook. McGraw-Hill, New York INGV (2002–2003) Centro Nazionale Terremoti, Centro Dati e Informazione sui Terremoti http://www.ingv.it/~roma/reti/ rms/bollettino/index.php. Cited 20 Sep 2006 Maruyama S, Kwon Y, Morimoto K (2001) Seismic intensity and mental stress after the great Hanshin-Awaji earthquake. Environ Health Prev Med 6:165–169 Musson RMW (2006) On the perceptibility of earthquakes. J Seismol 10:157–162 Peronaci F (1939) Limite di sensibilità umana alle accelerazioni sismiche orizzontali. Pubbl Ist Naz Geofis CNR 15:1–8 Shaw R, Shiwaku K, Kobayashi H, Kobayashi M (2004) Linking experience, education, perception and earthquake preparedness. Disaster Prev Manag 13:39–49 Sibol MS, Bollinger GA, Birch JB (1987) Estimation of magnitudes in Central and Eastern North America using intensity and felt area. Bull Seismol Soc Am 77(5):1635–1654 Sieberg A (1930) Geologie der Erdbeben. Handbuch der Geophysic, Tabb. 2–3, Berlin, Germany Slovic P (1987) Perception of risk. Science 236:280–285 Souriau A (2006) Quantifying felt events: a joint analysis of intensities, accelerations and dominant frequencies. J Seismol 10:23–38 Strack F, Mussweiler T (1997) Explaining the enigmatic anchoring effect: mechanisms of selective accessibility. J Pers Soc Psychol 73:437–446 Wood HO, Neumann F (1931) Modified Mercalli Intensity Scale of 1931. Bull Seismol Soc Am 21:277–283 J Seismol (2007) 11:205–219 219 | en |
dc.description.obiettivoSpecifico | 1.1. TTC - Monitoraggio sismico del territorio nazionale | en |
dc.description.obiettivoSpecifico | 5.8. TTC - Formazione e informazione | en |
dc.description.journalType | JCR Journal | en |
dc.description.fulltext | reserved | en |
dc.contributor.author | Cucci, L. | en |
dc.contributor.author | Tertulliani, A. | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia | en |
item.openairetype | article | - |
item.cerifentitytype | Publications | - |
item.languageiso639-1 | en | - |
item.grantfulltext | restricted | - |
item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
item.fulltext | With Fulltext | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia | - |
crisitem.author.orcid | 0000-0002-0238-2730 | - |
crisitem.author.orcid | 0000-0002-3746-0858 | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
Appears in Collections: | Article published / in press |
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