2016
DOI: 10.1093/gji/ggv556
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Effects of realistic topography on the ground motion of the Colombian Andes – A case study at the Aburrá Valley, Antioquia

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Cited by 25 publications
(14 citation statements)
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“…The undulating nature of surface topography leads to scat-tering or focusing of propagating waves (Lee et al, 2009a, b). Previous studies found that topography amplifies ground shaking at mountain tops and ridges, while it de-amplifies it in valleys; see, for example, Hartzell et al (1994) and Spudich et al (1996) in California, Lee et al (2009a, b) in Taiwan, Hough et al (2010) in Haiti, Kumagai et al (2011) in Ecuador and Restrepo et al (2016) in Colombia. Most seismic active areas are rugged in nature, which makes these regions prone to topographic (de-)amplification (Lee et al, 2009a;Hough et al, 2010;Shafique and van der Meijde, 2015).…”
Section: Introductionmentioning
confidence: 99%
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“…The undulating nature of surface topography leads to scat-tering or focusing of propagating waves (Lee et al, 2009a, b). Previous studies found that topography amplifies ground shaking at mountain tops and ridges, while it de-amplifies it in valleys; see, for example, Hartzell et al (1994) and Spudich et al (1996) in California, Lee et al (2009a, b) in Taiwan, Hough et al (2010) in Haiti, Kumagai et al (2011) in Ecuador and Restrepo et al (2016) in Colombia. Most seismic active areas are rugged in nature, which makes these regions prone to topographic (de-)amplification (Lee et al, 2009a;Hough et al, 2010;Shafique and van der Meijde, 2015).…”
Section: Introductionmentioning
confidence: 99%
“…Several satellite-based studies primarily focused on field displacement and slip distribution, such as Parsons et al (2006), Avouac et al (2006), Pathier et al (2006), Wang et al (2007) and Leprince et al (2008). Others addressed relationships between co-seismic displacement and landslides (e.g., Kamp et al, 2010;Dunning et al, 2007;Saba et al, 2010). Topographic amplification of seismic responses induced by the Kashmir earthquake was first evaluated by Shafique et al (2008) using the topographic aggravation factor (TAF) after Bouckovalas and Papadimitriou (2005).…”
Section: Introductionmentioning
confidence: 99%
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“… boldKe=n=15βnboldKnt, boldMe=n=15βnboldMnt.Due to its simplicity, the VT method uses the viscous Rayleigh type model damping as the material attenuation model. Further details on the VT method and its application to a case study for the Aburrá valley, Colombia can be found in Restrepo and Bielak 28 and Restrepo et al, 30 respectively. Below, there is a brief description of the three input models used by Hercules to conduct the simulations and the approximation of the nonlinear site effects.…”
Section: Methodology For the Assessment Of The Seismic Risk Of Determmentioning
confidence: 99%
“…The undulating nature of surface topography leads to scattering or focusing of propagating waves (Lee et al, 2009a,b). Previous studies found that topography amplifies the ground shaking at mountain tops and ridges, while it de-amplifies in valleys; for example Hartzell et al (1994) and Spudich et al (1996) in California; Lee et al (2009a,b) in Taiwan; Hough et al (2010) in Haiti, Kumagai et al (2011) in Ecuador, and Restrepo et al (2016) in Colombia. Most seismic active areas are rugged in nature, which makes these regions prone to topographic (de-)amplification (Lee et al, 2009a;Hough et al, 2010;Shafique and van der Meijde, 2015).…”
Section: Introductionmentioning
confidence: 98%