Rotational Motions Recorded at Hualien During the 2012 Wutai, Taiwan Earthquake
It is widely accepted that the effects of rotational motions on seismic waves can be neglected when ground motion is small and might be underestimated in near-fault and/or with extremely large ground motions. However, quantitative validation of these assumptions is still needed. During the 2012 Wuta...
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doaj-df149caf5e08405d92f3e5893d5ee3512020-11-25T00:25:40ZengChinese Geoscience UnionTerrestrial, Atmospheric and Oceanic Sciences1017-08392311-76802013-01-0124103110.3319/TAO.2012.10.22.01(T)1109Rotational Motions Recorded at Hualien During the 2012 Wutai, Taiwan EarthquakeHung-Chie ChiuFang-Ju WuHuey-Chu HuangIt is widely accepted that the effects of rotational motions on seismic waves can be neglected when ground motion is small and might be underestimated in near-fault and/or with extremely large ground motions. However, quantitative validation of these assumptions is still needed. During the 2012 Wutai earthquake in Taiwan (6.4 ML), a set of small rotation rate-strong motion velocity data was recorded at the HWLB (Hualien) seismographic station. This station is 161 km away from the epicenter and the recorded peak ground acceleration and rotation rate are about 7 cm s-1 s-1 and 0.1 mrad s-1, respectively. This data set is useful for evaluating the lower bound of ground motion that can be neglected regarding the effects of rotational motions. http://tao.cgu.org.tw/images/attachments/v241p031.pdf Wutai earthquakeRotational motionsStrong motionCentrifugal acceleration |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Hung-Chie Chiu Fang-Ju Wu Huey-Chu Huang |
spellingShingle |
Hung-Chie Chiu Fang-Ju Wu Huey-Chu Huang Rotational Motions Recorded at Hualien During the 2012 Wutai, Taiwan Earthquake Terrestrial, Atmospheric and Oceanic Sciences Wutai earthquake Rotational motions Strong motion Centrifugal acceleration |
author_facet |
Hung-Chie Chiu Fang-Ju Wu Huey-Chu Huang |
author_sort |
Hung-Chie Chiu |
title |
Rotational Motions Recorded at Hualien During the 2012 Wutai, Taiwan Earthquake |
title_short |
Rotational Motions Recorded at Hualien During the 2012 Wutai, Taiwan Earthquake |
title_full |
Rotational Motions Recorded at Hualien During the 2012 Wutai, Taiwan Earthquake |
title_fullStr |
Rotational Motions Recorded at Hualien During the 2012 Wutai, Taiwan Earthquake |
title_full_unstemmed |
Rotational Motions Recorded at Hualien During the 2012 Wutai, Taiwan Earthquake |
title_sort |
rotational motions recorded at hualien during the 2012 wutai, taiwan earthquake |
publisher |
Chinese Geoscience Union |
series |
Terrestrial, Atmospheric and Oceanic Sciences |
issn |
1017-0839 2311-7680 |
publishDate |
2013-01-01 |
description |
It is widely accepted that the effects of rotational motions on seismic waves can be neglected when ground motion is small and might be underestimated in near-fault and/or with extremely large ground motions. However, quantitative validation of these assumptions is still needed. During the 2012 Wutai earthquake in Taiwan (6.4 ML), a set of small rotation rate-strong motion velocity data was recorded at the HWLB (Hualien) seismographic station. This station is 161 km away from the epicenter and the recorded peak ground acceleration and rotation rate are about 7 cm s-1 s-1 and 0.1 mrad s-1, respectively. This data set is useful for evaluating the lower bound of ground motion that can be neglected regarding the effects of rotational motions. |
topic |
Wutai earthquake Rotational motions Strong motion Centrifugal acceleration |
url |
http://tao.cgu.org.tw/images/attachments/v241p031.pdf
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work_keys_str_mv |
AT hungchiechiu rotationalmotionsrecordedathualienduringthe2012wutaitaiwanearthquake AT fangjuwu rotationalmotionsrecordedathualienduringthe2012wutaitaiwanearthquake AT hueychuhuang rotationalmotionsrecordedathualienduringthe2012wutaitaiwanearthquake |
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