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  4. Investigating the Impacts of a Wet Typhoon on Microseismicity: A Case Study of the 2009 Typhoon Morakot in Taiwan Based on a Template Matching Catalog
 
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Investigating the Impacts of a Wet Typhoon on Microseismicity: A Case Study of the 2009 Typhoon Morakot in Taiwan Based on a Template Matching Catalog

Journal
Journal of Geophysical Research: Solid Earth
Journal Volume
126
Journal Issue
12
Date Issued
2021
Author(s)
Zhai Q
Peng Z
Chuang L.Y
Wu Y.-M
Hsu Y.-J
YIH-MIN WU  
DOI
10.1029/2021JB023026
URI
https://www.scopus.com/inward/record.uri?eid=2-s2.0-85121699529&doi=10.1029%2f2021JB023026&partnerID=40&md5=e1b5a2f86c69ac0ef529eeb4f2c9671a
https://scholars.lib.ntu.edu.tw/handle/123456789/606246
Abstract
Recent studies suggested that transient and long-term stress changes caused by Earth's surface processes (e.g., extreme weather events, annual variations on groundwater storages) can affect earthquake activities in the subsurface. However, these studies may be limited by the completeness of standard earthquake catalogs, especially during or right after extreme weather events. Here we apply the template matching method to build a more complete earthquake catalog in Taiwan spanning seven months before and 12 months after 2009 typhoon Morakot, which brought the highest rainfall in southern Taiwan in the past 60?years and triggered numerous landslides. We then use the enhanced catalog to investigate possible influences of typhoon-driven Earth's surface processes (atmospheric pressure, precipitation, and erosion) on local seismicity. We find that the seismicity rate of a 40-day earthquake sequence in northeastern Taiwan was reduced significantly right after the passage of typhoon Morakot's eye center. In the typhoon-triggered landslide zone in southern Taiwan, we find a slight increase in background seismicity rate in the next year after Morakot, matching the results of a recent study. However, we do not observe a clear change in the Gutenberg-Richter b-value in this zone, which is different from the recent study. Station outages during and right after Morakot prevents us from better understanding short-term precipitation effect on local seismicity. Overall, except for a reduction in seismicity rate near the typhoon's low-pressure eye center in northeastern Taiwan, we do not observe other clear seismicity changes that can be attributed to surface changes induced by typhoon Morakot. ? 2021. American Geophysical Union. All Rights Reserved.
Subjects
deep learning
Morakot
seismicity
Taiwan
template matching
typhoon
atmospheric pressure
earthquake catalogue
erosion
extreme event
landslide
precipitation (climatology)
seismic zone
stress change
Type
journal article

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