Detection of landslides and submarine slumps using broadband seismic networks

[1] We detected 52 seismic events associated with landslides and submarine slumps on 8 August 2009 when Typhoon Morakot hit Taiwan. These events were neither felt nor reported because their seismic energy was primarily in the long period band (20-50 s). Most of these events were located in mountain areas where the accumulated rainfall was extremely high, though some were found offshore southern Taiwan. Among all events, the fatal landslide earthquake was located at Hsiaolin Village, where 474 people were buried. Inversion modelling of the seismic waveforms generated by the Hsiaolin landslide shows that the seismic source was represented by single force, consistent with downhill sliding. Some offshore seismic events indicate that submarine slumps probably occurred along submarine canyons and steep slopes. Our study shows that broadband seismic monitoring can be used to issue early warnings for mitigating disasters generated by inland and offshore landslides.

[1]  John Ristau,et al.  Implementation of Routine Regional Moment Tensor Analysis in New Zealand , 2008 .

[2]  H. Kawakatsu Centroid single force inversion of seismic waves generated by landslides , 1989 .

[3]  J. Caplan-Auerbach,et al.  Recent and future warm extreme events and high-mountain slope stability , 2010, Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences.

[4]  Y. Tsai,et al.  A preliminary report on the 1999 Chi-Chi (Taiwan) earthquake , 2000 .

[5]  H. Kanamori,et al.  Analysis of long‐period seismic waves excited by the May 18, 1980, eruption of Mount St. Helens—A terrestrial monopole? , 1982 .

[6]  Barbara Romanowicz,et al.  Regional and far-regional earthquake locations and source parameters using sparse broadband networks: A test on the Ridgecrest sequence , 1998, Bulletin of the Seismological Society of America.

[7]  M. Nakano,et al.  Waveform inversion of volcano‐seismic signals assuming possible source geometries , 2005 .

[8]  Hiroyuki Fujiwara,et al.  Recent Progress of Seismic Observation Networks in Japan , 2004 .

[9]  J. Knight,et al.  Climate change and geomorphological hazards in the eastern European Alps , 2010, Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences.

[10]  J. M. Vilaplana,et al.  Seismic detection and characterization of landslides and other mass movements , 2005 .

[11]  E. R. Engdahl,et al.  Constraints on seismic velocities in the Earth from traveltimes , 1995 .

[12]  G. Wieczorek,et al.  Unusual July 10, 1996, rock fall at Happy Isles, Yosemite National Park, California , 2000 .

[13]  D. Petley On the impact of urban landslides , 2009 .

[14]  Tim Li,et al.  What causes the extremely heavy rainfall in Taiwan during Typhoon Morakot (2009)? , 2010 .

[15]  H. Kanamori,et al.  A single-force model for the 1975 Kalapana, Hawaii, Earthquake , 1987 .

[16]  H. Kanamori,et al.  Source mechanism of the magnitude 7.2 Grand Banks earthquake of November 1929: Double couple or submarine landslide? , 1987 .

[17]  E. E. Brabb,et al.  The world landslide problem , 1991 .

[18]  Jean-Claude Sibuet,et al.  Turbidity currents, submarine landslides and the 2006 Pingtung earthquake off SW Taiwan , 2008 .

[19]  Hitoshi Kawakatsu Automated near‐realtime CMT inversion , 1995 .

[20]  Philip Watts,et al.  Tsunami hazard from submarine landslides on the Oregon continental slope , 2004 .

[21]  M. Nakano,et al.  Waveform inversion in the frequency domain for the simultaneous determination of earthquake source mechanism and moment function , 2008 .

[22]  Hubert Chanson,et al.  The Impact of Typhoon Morakot on the Southern Taiwan Coast , 2010 .

[23]  H. Kao,et al.  Moment‐tensor inversion for offshore earthquakes east of Taiwan and their implications to regional collision , 1998 .

[24]  M. Kumazawa,et al.  Why have the single force and torque been excluded from seismic source models , 1994 .