4,047 research outputs found
Characteristics of Ambient Noise Cross-Correlations in Northern Italy within the 0.1- to 0.6-Hz Frequency Range
In this note, we investigate the characteristics of ambient noise cross-correlations for station pairs in northern Italy, considering the secondary microseism bandwidth (0.1-0.6 Hz). The preliminary analysis that we performed exploiting the available continuous recording in the investigated area, agrees with the recent results of Pedersen et al. (2007): the directionality of the noise signal cannot be disregarded when the group velocity is estimated in the range 0.1-0.6 Hz and the selection of the path orientation for tomography must be carefully performed. In particular, while the favourable directions with respect to microseisms generated along the Atlantic coasts of France, Norway and British Islands cover a quite wide azimuthal range (from about 270N to 5N), allowing us to reliably estimate the fundamental mode Rayleigh group velocity for paths in the Alps (about 2.7 km/s), more care must be taken when the microseisms are generated in the Mediterranean Sea. In that case, different locations of the generating areas of microseisms could provide biased estimates of the group velocity due to differences between the true and the apparent velocity of propagation between the stations
Characteristics of Ambient Noise Cross-Correlations in Northern Italy within the 0.1- to 0.6-Hz Frequency Range
In this note, we investigate the characteristics of ambient noise cross-correlations for station pairs in northern Italy, considering the secondary microseism bandwidth (0.1-0.6 Hz). The preliminary analysis that we performed exploiting the available continuous recording in the investigated area, agrees with the recent results of Pedersen et al. (2007): the directionality of the noise signal cannot be disregarded when the group velocity is estimated in the range 0.1-0.6 Hz and the selection of the path orientation for tomography must be carefully performed. In particular, while the favourable directions with respect to microseisms generated along the Atlantic coasts of France, Norway and British Islands cover a quite wide azimuthal range (from about 270N to 5N), allowing us to reliably estimate the fundamental mode Rayleigh group velocity for paths in the Alps (about 2.7 km/s), more care must be taken when the microseisms are generated in the Mediterranean Sea. In that case, different locations of the generating areas of microseisms could provide biased estimates of the group velocity due to differences between the true and the apparent velocity of propagation between the stations
Deblurring of frequency-wavenumber images from small-scale seismic arrays
Temporary arrays installed in urban areas for investigating the upper-most geological structure
typically comprised of a limited number of stations and are arranged in geometries constrained
by environmental boundaries. Therefore, it is expected that the frequency–wavenumber images
are significantly blurred by the array transfer function and are corrupted by noise.
In this paper, the effect of theRichardson–Lucy regularization method applied to the problem
of deblurring frequency–wavenumber images is investigated. The images are computed by
analysing data from two small-aperture 2-D arrays, installed with different configurations in
a test-site within the town of Potenza (Southern Italy) for near-surface investigations. We
show that removing the effects of the array response from the frequency–wavenumber images
improve the phase-velocity estimation, reducing the relevant level of uncertainty. Furthermore,
the Richardson–Lucy regularization method is effective in reducing the level of noise related
to spatial aliasing by eliminating spurious peaks, allowing the maxima related to different
seismic sources to be better discriminated
Task 2 - Deliverable 4: Software for strong-motion data display and processing
The deliverable 4 is composed by a set of routines created to read and process the time series stored in the data base format, that is an ASCII file with a 43 row header, with the name codified as specified in the Deliverable 1. The files can also be read in SAC format
Seismic input motion determined from a surface-downhole pair of sensors: a constrained deconvolution approach.
We apply a deconvolution approach to the problem of determining the
input motion at the base of an instrumented borehole using only a pair of recordings,
one at the borehole surface and the other at its bottom. To stabilize the bottom-tosurface
spectral ratio, we apply an iterative regularization algorithm that allows us
to constrain the solution to be positively defined and to have a finite time duration.
Through the analysis of synthetic data, we show that the method is capable of retrieving
reliable input motion, suppressing the effect of the negative interference generated
by the downgoing waves. Results obtained by applying the methodology to weak
earthquakes recorded at the Ataköy (Istanbul) vertical array are also presented and
show that removing the effect of the downgoing waves is remarkable, even considering
the recording at a depth of 140 m
Empirical site-specific response-spectra correction factors for the Gubbio basin (central Italy)
Providing quantitative microzonation results that can be taken into account in urban land-use plans is a challenging task that requires collaborative efforts between the seismological and engineering communities. In this study, starting from the results obtained by extensive geophysical and seismological investigations, we propose and apply an approach to the Gubbio basin (Italy) that can be easily implemented for cases of moderate-to-low ground motion and that takes into account not only simple 1D, but also more complicated 3D effects. With this method, the sites inside the basin are classified by their fundamental resonance frequencies, estimated from the horizontal-to-vertical spectral ratio applied to noise recordings (HVNSR). The correspondence between estimates of the fundamental frequency from this method and those derived from earthquake recordings was verified at several calibration sites. The amplification factors used to correct the response spectra are computed by the ratio between the response spectra at sites within the basin and the response spectra at a hard-rock site using data from two seismic transects. Empirical amplification functions are then assigned to the fundamental frequencies after applying an interpolation technique. The suitability of the estimated site-specific correction factors for response spectra was verified by computing synthetic response spectra for stations within the basin, starting from the synthetic recording at a nearby rock station, and comparing them with observed ones
Source Spectra and Site Response from S Waves of Intermediate-Depth Vrancea, Romania, Earthquakes
Seismograms from 55 intermediate-depth Vrancea earthquakes (M 4:0–
7:1) recorded at 43 stations of an accelerometric network in Romania are used to
derive source spectra and site amplification functions from S waves in the frequency
range 0.5–20 Hz with the generalized inversion technique (GIT) (Castro et al., 1990).
Attenuation is taken into account using the nonparametric attenuation functions derived
by Oth et al. (2008) from the same dataset, and the attenuation-corrected data are
then split into source and site contributions. The source spectra follow the ω 2 model
(Brune, 1970, 1971) with high corner frequencies and a related Brune stress drop of
the order of 100 MPa. The site amplification functions are separately determined for
both horizontal and vertical components. Contrary to widespread expectation, the
vertical component shows significant amplification effects at high frequencies. The
H=Z ratios determined from the GIT results compare well with H=V ratios computed
directly from the S-wave window of the accelerograms (Lermo and Chávez-GarcÃa,
1993). The basic assumption for the determination of site effects from H=V ratios is
that the vertical component is not or only little affected by site effects. For Vrancea
earthquakes, this assumption is incorrect; consequently, site effects should not be
estimated from H=V ratios. The reason for this peculiar fact is the geometry of
intermediate-depth seismicity that leads to almost vertical ray paths beneath the
stations
S-Wave Attenuation Characteristics beneath the Vrancea Region in Romania: New Insights from the Inversion of Ground-Motion Spectra
The S-wave attenuation characteristics beneath the Vrancea region in
Romania are analyzed from the spectra (frequency range 0.5–20 Hz) of more than
850 recordings at 43 accelerometric stations of 55 intermediate-depth earthquakes
(M 4:0–7:1) that occurred in the Vrancea seismogenic zone. The method commonly
chosen for this type of investigation in the case of crustal earthquakes is the generalized
inversion technique (GIT) (e.g., Andrews, 1986; Castro et al., 1990). Yet the
Vrancea dataset is entirely different from common crustal datasets. Because of the
strong clustering of the hypocenters within a very small focal volume, there are only
few crossing ray paths from sources to receivers. As a consequence, inhomogeneities
in the attenuation properties are not averaged out, which leads to unphysical results if
the standard GIT approach is adopted. The problem is discussed qualitatively by performing
tests with synthetic data and solved quantitatively by adapting the GIT technique
in view of these peculiarities.With the optimally adapted inversion scheme, it is
possible to unravel differences in the attenuation characteristics between two (or more)
sets of stations. The results show that the attenuation of seismic waves is roughly
comparable in the low frequency range (<4–5 Hz) but stronger by up to an order
of magnitude at higher frequencies within the Carpathian mountain arc as compared
with the foreland area. Modeling this strongly frequency-dependent lateral variation of
seismic attenuation by a significantly lower Q beneath Vrancea (1) provides a very
good fit of observed strong-motion characteristics, (2) sheds new light on the distribution
of intensities of the previous strong earthquakes, (3) will have strong implications
for future hazard assessment, and (4) is fully compatible with structural models
from deep seismic sounding, tomography, and teleseismic attenuation
Detecting long-lasting transients of earthquake activity on a fault system by monitoring apparent stress, ground motion and clustering
Damaging earthquakes result from the evolution of stress in the brittle upper-crust, but the understanding of the mechanics of faulting cannot be achieved by only studying the large ones, which are rare. Considering a fault as a complex system, microearthquakes allow to set a benchmark in the system evolution. Here, we investigate the possibility to detect when a fault system starts deviating from a predefined benchmark behavior by monitoring the temporal and spatial variability of different micro-and-small magnitude earthquakes properties. We follow the temporal evolution of the apparent stress and of the event-specific residuals of ground shaking. Temporal and spatial clustering properties of microearthquakes are monitored as well. We focus on a fault system located in Southern Italy, where the Mw 6.9 Irpinia earthquake occurred in 1980. Following the temporal evolution of earthquakes parameters and their time-space distribution, we can identify two long-lasting phases in the seismicity patterns that are likely related to high pressure fluids in the shallow crust, which were otherwise impossible to decipher. Monitoring temporal and spatial variability of micro-to-small earthquakes source parameters at near fault observatories can have high potential as tool for providing us with new understanding of how the machine generating large earthquakes works
On-site earthquake early warning: a partially non-ergodic perspective from the site effects point of view
We introduce in the on-site earthquake early warning (EEW) a partially non-ergodic perspective
from the site effects point of view. We consider the on-site EEW approach where the peak
ground velocity (PGV) for S waves is predicted from an early estimate, over the P waves,
of either the peak-displacement (PD) or cumulative squared velocity (IV2). The empirical
PD-PGV and IV2-PGV relationships are developed by applying a mixed-effect regression
where the site-specific modifications of ground shaking are treated as random effects. We
considered a large data set composed of almost 31 000 selected recordings in central Italy, a
region struck by four earthquakes with magnitude between 6 and 6.5 since the 2009 L’Aquila
earthquake. We split the data set into three subsets used for calibrating and validating the
on-site EEW models, and for exemplifying their application to stations installed after the
calibration phase. We show that the partially non-ergodic models improve the accuracy of
the PGV predictions with respect to ergodic models derived for other regions of the world.
Moreover, considering PD and accounting for site effects, we reduce the (apparent) aleatory
variability of the logarithm of PGV from 0.31 to 0.36, typical values for ergodic on-site EEW
models, to about 0.25. Interestingly, a lower variability of 0.15 is obtained by considering IV2
as proxy, which suggests further consideration of this parameter for the design of on-site EEW
systems. Since being site-specific is an inherent characteristic of on-site EEW applications,
the improved accuracy and precision of the PGV predicted for a target protection translate in
a better customization of the alert protocols for automatic actions
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