By Zbigniew Bednarczyk (auth.), Claudio Margottini, Paolo Canuti, Kyoji Sassa (eds.)
ISBN-10: 3642314449
ISBN-13: 9783642314445
ISBN-10: 3642314457
ISBN-13: 9783642314452
This booklet comprises peer-reviewed papers from the second one global Landslide discussion board, organised through the overseas Consortium on Landslides (ICL), that happened in September 2011. the whole fabric from the convention has been cut up into seven volumes, this one is the second one: 1. Landslide stock and Susceptibility and chance Zoning, 2. Early caution, Instrumentation and tracking, three. Spatial research and Modelling, four. worldwide Environmental switch, five. complicated atmosphere, 6. probability review, administration and Mitigation, 7. Social and fiscal influence and Policies.
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Extra resources for Landslide Science and Practice: Volume 2: Early Warning, Instrumentation and Monitoring
Example text
2004). Volumetric Analysis Since the landslide movement was in progress and works for cleaning the railway and defining stable profile were executed during the months of observation, it’s not possible to quantify the slide down materials or the removal one by volumetric analysis at the landslide tip. The comparison between the terrain surfaces of different dates defines just reprofiling of landslide for anthropic or natural causes (Table 3). Every comparison is obtained subtracting terrain elevation of the newer scan from terrain elevation of the older scan.
2002) However, the following challenges remain to be solved, according to Colesanti and Wasowski 2006; Rocca 2003; Manzo et al. 2006: 1. PS data represent a one-demensional line of sight (1D LOS) projection of a deformation occurring in a 3D world. Some attempts to resolve horizontal displacements from 1D LOS were carried out by Cascini et al. (2010); 2. Deformation greater than l/4 between two following visits of the satellite are difficult to track due to the ambiguity of radar phase measurements; 3.
Experimental surveys were performed for the Montaguto landslide (Campania, Italy), the greatest of Europe, by means of laser scanner Riegl LPM-321 (Alba et al. 2005), with measurement range up to 6,000 m. Differential volume maps from different surveys were obtained. The complex morphology of the Montaguto landslide, located in the Cervaro river valley, had required a viewshed analysis for the selection of the base station locations. Detailed laser scanner acquisitions were conducted on the tip landslide zone, because of the presence of strategic mobility.
Landslide Science and Practice: Volume 2: Early Warning, Instrumentation and Monitoring by Zbigniew Bednarczyk (auth.), Claudio Margottini, Paolo Canuti, Kyoji Sassa (eds.)
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