Variation of human perceptiveness of earthquakes during seismic sequences
Language
English
Obiettivo Specifico
1.1. TTC - Monitoraggio sismico del territorio nazionale
5.8. TTC - Formazione e informazione
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Journal
Issue/vol(year)
11/2007
Publisher
Springer Science
Pages (printed)
205–219
Date Issued
February 2007
Alternative Location
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.
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.
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
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
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