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DOI10.1126/science.1232887
Simple scaling of catastrophic landslide dynamics
Ekström G.; Stark C.P.
发表日期2013
ISSN0036-8075
起始页码1416
结束页码1419
卷号339期号:6126
英文摘要Catastrophic landslides involve the acceleration and deceleration of millions of tons of rock and debris in response to the forces of gravity and dissipation. Their unpredictability and frequent location in remote areas have made observations of their dynamics rare. Through real-time detection and inverse modeling of teleseismic data, we show that landslide dynamics are primarily determined by the length scale of the source mass. When combined with geometric constraints from satellite imagery, the seismically determined landslide force histories yield estimates of landslide duration, momenta, potential energy loss, mass, and runout trajectory. Measurements of these dynamical properties for 29 teleseismogenic landslides are consistent with a simple acceleration model in which height drop and rupture depth scale with the length of the failing slope.
英文关键词catastrophic event; debris flow; dissipation; gravity field; inverse analysis; landslide; real time; rock avalanche; satellite imagery; seismic data; slope failure; teleseismic wave; article; disaster; gravity; landslide; mechanical torsion; priority journal; torque
语种英语
来源期刊Science
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/243606
作者单位Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY 10964, United States
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Ekström G.,Stark C.P.. Simple scaling of catastrophic landslide dynamics[J],2013,339(6126).
APA Ekström G.,&Stark C.P..(2013).Simple scaling of catastrophic landslide dynamics.Science,339(6126).
MLA Ekström G.,et al."Simple scaling of catastrophic landslide dynamics".Science 339.6126(2013).
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