HR: 0800h
AN: S31B-1050 [Abstracts]
TI: Filtering Applications on Seismogram Analysis
AU: * Djordjevic, M
EM: marija.djordjevic@mail.uh.edu
AF: University of Houston, 4800 Calhoun Rd, SR1,RM312, Houston, TX 77204
United States
AB:
Useful data extraction from registered signals is an
everyday problem. Seismogram filtering can be used to enhance the
earthquake signal, especially, knowing that period range is
strongly amplified by the seismograph itself.
The goal of this project was to estimate tradeoffs between noise
reduction and the sharpness of the filtered earthquake signal. The
different filter bands were applied on the seismograms from
different epicentral distances, including both local and regional
earthquakes, in order to see the quality of the data.
During the seismogram analysis we had two approaches: reading the
wave phase (arrival time, amplitude, period) and spectral
analysis, since frequency filtering is essential. The well-known
set of Fourier orthogonal basis functions was used for spectral
analysis.
The main purpose of filtering was to remove the noise from the
seismograms and to get as much possible information from the
record. Practical application was obtained using custom made
"Analysis" software. We processed 5 earthquake signals; four local
and one distant earthquake. The data came from Djerdap
Seismological Station, Serbia. Filtering was based on a band-pass
filter with frequency cut-offs from 0.2Hz to 10Hz. Every record
was filtered with five filters (10-1Hz,10-2.5Hz, 2.5-1Hz,
1-0.2Hz). The manipulation with different filter bands allowed us
to define precisely the beginning of the earthquakes and first
arrivals of different wave phases. The best result for the 45km
epicentral distance earthquake was obtained using window
0.1-0.5sec, where very clear Pg and Sg arrivals could be
distinguished. The distant earthquake showed the advantages of
filtering seismograms to enhance the long period energy. The
lowest frequency band-pass filter (1-0.2Hz) was the most
successful.
The results of the experiment were with very clear Pg and Sg
arrivals when the right bands were used for filtering. This
improved the quality of the original signals by emphasizing the
temporal and frequency characteristics of interest.
DE: 7299 General or miscellaneous
DE: 7200 SEISMOLOGY
DE: 7215 Earthquake parameters
SC: Seismology [S]
MN: 2004 AGU Fall Meeting