Effect of Finite Frequency Bandwidth Limitation on Evaluations of Seismic Radiation Energy of the 1999 Chi-Chi Earthquake

Based on the £s−2 and £s−3 source models, we explore the effect on estimates of seismic radiation energy, Es , caused by finite frequency bandwidth limitation of source spectra. Let fc be the corner frequency of a source spectrum and fu and fc are, respectively, the upper and lower bounds of a frequ...

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Main Author: Jeen-Hwa Wang Ming-Wey Huang
Format: Article
Language:English
Published: Chinese Geoscience Union 2007-01-01
Series:Terrestrial, Atmospheric and Oceanic Sciences
Subjects:
Online Access: http://tao.cgu.org.tw/images/attachments/v183p567.pdf
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spelling doaj-1cf3086372d843c5800d24bd7ec8aa7c2020-11-24T22:14:43ZengChinese Geoscience UnionTerrestrial, Atmospheric and Oceanic Sciences1017-08392311-76802007-01-0118356710.3319/TAO.2007.18.3.567(T)Effect of Finite Frequency Bandwidth Limitation on Evaluations of Seismic Radiation Energy of the 1999 Chi-Chi EarthquakeJeen-Hwa Wang Ming-Wey HuangBased on the £s−2 and £s−3 source models, we explore the effect on estimates of seismic radiation energy, Es , caused by finite frequency bandwidth limitation of source spectra. Let fc be the corner frequency of a source spectrum and fu and fc are, respectively, the upper and lower bounds of a frequency band in use. Results show that the effect depends on fu/fc and fl/fc , and Es is under-estimated when fl > 0 and fu < ¡_. When fu/fc < 20, the effect is sensitive to both fl/fc and fu/fc for the £s−2 source model, but mainly to fl/fc for the £s−3 model. When fu/fc > 20, the effect is insensitive only to fu/fc for the two models. Let Es¡¦ be the seismic radiation energy estimated without removal of finite frequency bandwidth limitation. Results show: (1) Es¡¦/Es first slightly increases and then decreases with increasing fc ; or (2) Es¡¦/Es monotonously decrease with increasing fc. For the 1999 Ms 7.6 Chi-Chi earthquake, Taiwan, Es was under-estimated by Hwang et al. (2001), and the degree of under-estimates varies from station to station. http://tao.cgu.org.tw/images/attachments/v183p567.pdf Seismic radiation energyCorner frequencyFinite frequency bandwidth limitation
collection DOAJ
language English
format Article
sources DOAJ
author Jeen-Hwa Wang Ming-Wey Huang
spellingShingle Jeen-Hwa Wang Ming-Wey Huang
Effect of Finite Frequency Bandwidth Limitation on Evaluations of Seismic Radiation Energy of the 1999 Chi-Chi Earthquake
Terrestrial, Atmospheric and Oceanic Sciences
Seismic radiation energy
Corner frequency
Finite frequency bandwidth limitation
author_facet Jeen-Hwa Wang Ming-Wey Huang
author_sort Jeen-Hwa Wang Ming-Wey Huang
title Effect of Finite Frequency Bandwidth Limitation on Evaluations of Seismic Radiation Energy of the 1999 Chi-Chi Earthquake
title_short Effect of Finite Frequency Bandwidth Limitation on Evaluations of Seismic Radiation Energy of the 1999 Chi-Chi Earthquake
title_full Effect of Finite Frequency Bandwidth Limitation on Evaluations of Seismic Radiation Energy of the 1999 Chi-Chi Earthquake
title_fullStr Effect of Finite Frequency Bandwidth Limitation on Evaluations of Seismic Radiation Energy of the 1999 Chi-Chi Earthquake
title_full_unstemmed Effect of Finite Frequency Bandwidth Limitation on Evaluations of Seismic Radiation Energy of the 1999 Chi-Chi Earthquake
title_sort effect of finite frequency bandwidth limitation on evaluations of seismic radiation energy of the 1999 chi-chi earthquake
publisher Chinese Geoscience Union
series Terrestrial, Atmospheric and Oceanic Sciences
issn 1017-0839
2311-7680
publishDate 2007-01-01
description Based on the £s−2 and £s−3 source models, we explore the effect on estimates of seismic radiation energy, Es , caused by finite frequency bandwidth limitation of source spectra. Let fc be the corner frequency of a source spectrum and fu and fc are, respectively, the upper and lower bounds of a frequency band in use. Results show that the effect depends on fu/fc and fl/fc , and Es is under-estimated when fl > 0 and fu < ¡_. When fu/fc < 20, the effect is sensitive to both fl/fc and fu/fc for the £s−2 source model, but mainly to fl/fc for the £s−3 model. When fu/fc > 20, the effect is insensitive only to fu/fc for the two models. Let Es¡¦ be the seismic radiation energy estimated without removal of finite frequency bandwidth limitation. Results show: (1) Es¡¦/Es first slightly increases and then decreases with increasing fc ; or (2) Es¡¦/Es monotonously decrease with increasing fc. For the 1999 Ms 7.6 Chi-Chi earthquake, Taiwan, Es was under-estimated by Hwang et al. (2001), and the degree of under-estimates varies from station to station.
topic Seismic radiation energy
Corner frequency
Finite frequency bandwidth limitation
url http://tao.cgu.org.tw/images/attachments/v183p567.pdf
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