Abstract
Abstract. A methodology to detect local incompleteness of
macroseismic intensity data at the local scale is presented. In particular,
the probability that undocumented effects actually occurred at a site is
determined by considering intensity prediction equations (in their
probabilistic form) integrated by observations relative to known events
documented at surrounding sites. The outcomes of this analysis can be used
to investigate how representative and known the seismic histories of
localities are (i.e., the list of documented effects through time). The proposed approach is applied to the Italian area. The analysis shows that, at most of
the considered sites, the effects of intensity ≥ 6 should most probably
have occurred at least once, but they are not contained in the current
version of the Italian macroseismic databases. In a few cases, instead, the
lack of data may concern higher intensity levels (i.e., ≥ 8). The
geographical distribution of potentially lost information reflects the
heterogeneity of the seismic activity over the Italian territory.
Subject
General Earth and Planetary Sciences
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