Evaluation of Rainfall-Induced Landslides triggering using a multidisciplinary approach
Published
Aug 27, 2020
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Ivo Fustos
https://orcid.org/0000-0002-3542-5477
Pablo Moreno-Yaeger
https://orcid.org/0000-0001-5219-4546
Daniel Vasquez
https://orcid.org/0000-0001-8106-4804
Bastian Morales
https://orcid.org/0000-0002-7863-5503
Antonieta Silva
https://orcid.org/0000-0002-4862-749X
Elisa Ramirez
https://orcid.org/0000-0001-5900-432X
https://orcid.org/0000-0002-3542-5477
Pablo Moreno-Yaeger
https://orcid.org/0000-0001-5219-4546
Daniel Vasquez
https://orcid.org/0000-0001-8106-4804
Bastian Morales
https://orcid.org/0000-0002-7863-5503
Antonieta Silva
https://orcid.org/0000-0002-4862-749X
Elisa Ramirez
https://orcid.org/0000-0001-5900-432X
##plugins.themes.bootstrap3.article.details##
Abstract
In a large part of South America, slow landslides are triggered by extreme hydrometeorological conditions leading to, for instance, Rainfall-Induced Landslides – RILs. These RILs are common in urban areas and have a negative impact on the population and infrastructure development. Despite their importance, these events are little understood. We aimed at understanding the spatial distribution of RILs in the urban zone of Temuco, Chile (38.8°S, 72.6°W). The area has the typical hydrometeorological conditions of southern Chile. We conducted our assessment with a temporal analysis of shallow deformations, obtained by synthetic aperture radar interferometry (Sentinel 1 A/B). These shallow deformation rates were compared with satellite precipitation data (CHIRPS product) and electrical resistivity tomography (ERT). We identified active RIL-prone zones with deformation rates greater than 60 mm during the period 2014 to 2017, supporting theories of hydrometeorological control. Slow movements were observed in volcanic soils, suggesting the influence of their geotechnical characteristics. Our results can be extrapolated to the southern Andes (35°S-43°S), where a large number of volcanic-sedimentary units are susceptible to RILs. Finally, integration of our multidisciplinary approach will facilitate understanding of the local RIL dynamics, allowing a better risk management to decision-makers in South American and other developing countries.
Keywords
InSAR Time-series, Rainfall-Induced Landslides
References
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doi: 10.1080/01431161.2017.1317944
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doi: 10.1002/joc.6219
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[20] Yalcin A. The effects of clay on landslides: A case study. Applied Clay Science, 38 (1-2): 77-85, 2007.
doi: 10.1016/j.clay.2007.01.007
[21] Hungr O, Leroueil S, Picarelli L. The Varnes classification of landslide types, an update. Landslides, 11 (2): 167-194, 2014.
doi: 10.1007/s10346-013-0436-y
[22] Cochachin A, Frey H, Huggel C, Strozzi T, Büech, E, Cui F, Flores A, Saito C. Integrated satellite InSAR and slope stability modeling to support hazard assessment at the Safuna Alta glacial lake, Peru. EGUGA2017-14505, 2017.
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doi: 10.1016/j.rse.2018.08.014
[24] Varnes DJ. Landslide hazard zonation: a review of principles and practice. United Nations International, Paris. 1984.
https://unesdoc.unesco.org/ark:/48223/pf0000063038
[25] Charrier R, Pinto L, Rodríguez M. Tectonostratigraphic evolution of the Andean Orogen in Chile. In Moreno T. y Gibbons W. (eds.) The Geology of Chile. The Geological Society, London. 21-114, 2007.
doi: 10.1144/goch.3
[26] Mella M, Quiroz D. Geología del Área Temuco-Nueva Imperial, Región de La Araucanía. Servicio Nacional de Geología y Minería, Carta Geológica de Chile, Serie Geología Básica, 1 mapa escala 1:100.000. 122: 46, 2010.
http://tienda.sernageomin.cl/TiendaVirtual2/ProductDetail.aspx?pid=2268
[27] Gunn DA, Chambers JE, Uhlemann S, Wilkinson PB, Meldrum PI, Dijkstra TA, Haslam E, Kirkham M, Wragg J, Holyoake S, Hughes PN, Hen-Jones R, Glendinning S. Moisture monitoring in clay embankments using electrical resistivity tomography. Construction and Building Materials, 92: 82-94, 2015.
doi: 10.1016/j.conbuildmat.2014.06.007
[28] Fustos I, Hermosilla M, Moreno-Yaeger P, Abarca-del-Río R. Solifluction and complex movements observed from InSAR time series and satellite precipitation products: Cases over central south of Chile. Conference: South America Water from Space, 1, 2018.
doi: 10.13140/rg.2.2.14952.37122
[29] Kearey P, Brooks M, Hill I. An introduction to geophysical exploration, Ed. John Wiley & Sons. 2013. 294
[30] Sandwell DT, Myer D, Mellors R, Shimada M, Brooks B, Foster J. Accuracy and resolution of ALOS interferometry: Vector deformation maps of the Father's Day intrusion at Kilauea. IEEE Transactions on Geoscience and Remote Sensing, 46 (11): 3524-3534, 2008.
doi: 10.1109/tgrs.2008.2000634
[31] Ahmed R, Siqueira P, Hensley S, Chapman B, Bergen K. A survey of temporal decorrelation from spaceborne L-Band repeat-pass InSAR. Remote Sensing of Environment, 115 (11): 2887-2896, 2011.
doi: 10.1016/j.rse.2010.03.017
[32] Galve J P, Pérez-Peña JV, Azañón JM, Closson D, Caló F, Reyes-Carmona C, ..., Herrera G. Evaluation of the SBAS InSAR service of the European space Agency’s Geohazard Exploitation Platform (GEP). Remote Sensing, 9 (12): 1291, 2017.
doi: 10.3390/rs9121291
[33] Zhao C, Kang Y, Zhang Q, Lu Z, Li B. Landslide identification and monitoring along the Jinsha River catchment (Wudongde reservoir area), China, using the InSAR method. Remote Sensing, 10 (7): 993, 2018.
doi: 10.3390/rs10070993
[34] Massonnet D, Souyris JC. Imaging with synthetic aperture radar, Ed. CRC Press. 2008.
[35] Funk C, Peterson P, Landsfeld M, Pedreros D, Verdin J, Shukla S, Husak G, Rowland J, Harrison L, Hoell A, Michaelsen J. The climate hazards infrared precipitation with stations: a new environmental record for monitoring extremes, Scientific data, 2 (1): 1-21, 2015.
doi: 10.1038/sdata.2015.66
doi: 10.1007/978-3-642-31313-4_32
[2] Kim HG, Lee DK, Park C. Assessing the cost of damage and effect of adaptation to landslides considering climate change. Sustainability, 10 (5): 1-22, 2018.
doi: 10.3390/su10051628
[3] Vega JA, Hidalgo CA. Risk Assessment of Earthquake-Induced Landslides in Urban Zones. In Advancing Culture of Living with Landslides, Ed. Springer, 953-963, 2017.
doi: 10.1007/978-3-319-53498-5
[4] Harp EL, Reid ME, McKenna JP, Michael JA. Mapping of hazard from rainfall-triggered landslides in developing countries: examples from Honduras and Micronesia. Engineering Geology, 104 (3-4), 295-311, 2009.
doi: 10.1016/j.enggeo.2008.11.010
[5] Angeli MG, Pasuto A, Silvano S. A critical review of landslide monitoring experiences. Engineering Geology, 55 (3), 133-147, 2000.
doi: 10.1016/s0013-7952(99)00122-2
[6] Kim HG, Lee DK, Park C. Assessing the cost of damage and effect of adaptation to landslides considering climate change. Sustainability, 10 (5): 1628, 2018.
doi: 10.3390/su10051628
[7] Felizardo Batista E, De Brum Passini L, & Christopher Morales Kormann A. Methodologies of Economic Measurement and Vulnerability Assessment for Application in Landslide Risk Analysis in a Highway Domain Strip: A Case Study in the Serra Pelada Region (Brazil). Sustainability, 11 (21), 6130, 2019.
doi: 10.3390/su11216130
[8] Fustos I, Abarca-del-Río R, Mardones M, González L, Araya LR. Rainfall-induced landslide identification using numerical modelling: A southern Chile case. Journal of South American Earth Sciences, 101: 102587, 2020.
doi: 10.1016/j.jsames.2020.102587
[9] Mansour MF, Morgenstern NR, Martin CD. Expected damage from displacement of slow-moving slides. Landslides, 8 (1): 117-131, 2011.
doi: 10.1007/s10346-010-0227-7
[10] Fustos I, Remy D, Abarca-del-Río R, Muñoz A. Slow movements observed with in situ and remote-sensing techniques in the central zone of Chile. International Journal of Remote Sensing, 38 (24): 7514-7530, 2017.
doi: 10.1080/01431161.2017.1317944
[11] Bordoni M, Persichillo MG, Meisina C, Bartelletti C, Barsanti M, Avanzi, GD. Estimation of the susceptibility of a road network to shallow landslides with the integration of the sediment connectivity. Natural Hazards and Earth System Sciences, 18 (6): 1735-1758, 2018.
doi: 10.5194/nhess-18-1735-2018
[12] Heckmann T, Cavalli M, Cerdan O, Foerster S, Javaux M, Lode E, Smetanova A, Vericat D, Brardinoni F. Indices of sediment connectivity: opportunities, challenges and limitations. EarthScience Reviews, 187: 77-108, 2018.
doi: 10.1016/j.earscirev.2018.08.004
[13] Demaria EM, Maurer EP, Thrasher B, Vicuña S, Meza FJ. Climate change impacts on an alpine watershed in Chile: Do new model projections change the story?. Journal of Hydrology, 502: 128-138, 2013.
doi: 10.1016/j.jhydrol.2013.08.027
[14] Barros V, Field C, Dokken D, Mastrandrea M, Mach K, Bilir T, Chatterjee M, …, White L. Climate change 2014: impacts, adaptation, and vulnerability. Part B: regional aspects. Contribution of working group II to the fifth assessment report of the intergovernmental panel on climate change. Cambridge: Cambridge University Press. 2014.
https://www.ipcc.ch/report/ar5/wg2/
[15] Sepúlveda SA, Petley DN. Regional trends and controlling factors of fatal landslides in Latin America and the Caribbean. Natural Hazards and Earth System Science, 15 (8): 1821-1833, 2015.
doi: 10.5194/nhess-15-1821-2015
[16] Handwerger AL, Fielding EJ, Huang MH, Bennett GL, Liang C, Schulz WH. Widespread initiation, reactivation, and acceleration of landslides in the northern California Coast Ranges due to extreme rainfall. Journal of Geophysical Research: Earth Surface, 124 (7): 1782-1797, 2019.
doi: 10.1029/2019JF005035
[17] Handwerger AL, Huang MH, Fielding EJ, Booth AM, Bürgmann, R. A shift from drought to extreme rainfall drives a stable landslide to catastrophic failure. Scientific reports, 9 (1): 1-12, 2019.
doi: 10.1038/s41598-018-38300-0
[18] Garreaud RD, Boisier JP, Rondanelli R, Montecinos A, Sepúlveda HH, Veloso-Aguila D. The central Chile mega drought (2010–2018): a climate dynamics perspective. International Journal of Climatology, 40 (1): 421-439, 2019.
doi: 10.1002/joc.6219
[19] Terzaghi K. Theoretical Soil Mechanics. Chapman and Hali, Limited John Wiler and Sons, Inc, New York. 1944.
doi: 10.1002/9780470172766
[20] Yalcin A. The effects of clay on landslides: A case study. Applied Clay Science, 38 (1-2): 77-85, 2007.
doi: 10.1016/j.clay.2007.01.007
[21] Hungr O, Leroueil S, Picarelli L. The Varnes classification of landslide types, an update. Landslides, 11 (2): 167-194, 2014.
doi: 10.1007/s10346-013-0436-y
[22] Cochachin A, Frey H, Huggel C, Strozzi T, Büech, E, Cui F, Flores A, Saito C. Integrated satellite InSAR and slope stability modeling to support hazard assessment at the Safuna Alta glacial lake, Peru. EGUGA2017-14505, 2017.
[23] Strozzi T, Klimeš J, Frey H, Caduff R, Huggel C, Wegmüller U, Rapre AC. Satellite SAR interferometry for the improved assessment of the state of activity of landslides: A case study from the Cordilleras of Peru. Remote sensing of environment, 217: 111-125, 2018.
doi: 10.1016/j.rse.2018.08.014
[24] Varnes DJ. Landslide hazard zonation: a review of principles and practice. United Nations International, Paris. 1984.
https://unesdoc.unesco.org/ark:/48223/pf0000063038
[25] Charrier R, Pinto L, Rodríguez M. Tectonostratigraphic evolution of the Andean Orogen in Chile. In Moreno T. y Gibbons W. (eds.) The Geology of Chile. The Geological Society, London. 21-114, 2007.
doi: 10.1144/goch.3
[26] Mella M, Quiroz D. Geología del Área Temuco-Nueva Imperial, Región de La Araucanía. Servicio Nacional de Geología y Minería, Carta Geológica de Chile, Serie Geología Básica, 1 mapa escala 1:100.000. 122: 46, 2010.
http://tienda.sernageomin.cl/TiendaVirtual2/ProductDetail.aspx?pid=2268
[27] Gunn DA, Chambers JE, Uhlemann S, Wilkinson PB, Meldrum PI, Dijkstra TA, Haslam E, Kirkham M, Wragg J, Holyoake S, Hughes PN, Hen-Jones R, Glendinning S. Moisture monitoring in clay embankments using electrical resistivity tomography. Construction and Building Materials, 92: 82-94, 2015.
doi: 10.1016/j.conbuildmat.2014.06.007
[28] Fustos I, Hermosilla M, Moreno-Yaeger P, Abarca-del-Río R. Solifluction and complex movements observed from InSAR time series and satellite precipitation products: Cases over central south of Chile. Conference: South America Water from Space, 1, 2018.
doi: 10.13140/rg.2.2.14952.37122
[29] Kearey P, Brooks M, Hill I. An introduction to geophysical exploration, Ed. John Wiley & Sons. 2013. 294
[30] Sandwell DT, Myer D, Mellors R, Shimada M, Brooks B, Foster J. Accuracy and resolution of ALOS interferometry: Vector deformation maps of the Father's Day intrusion at Kilauea. IEEE Transactions on Geoscience and Remote Sensing, 46 (11): 3524-3534, 2008.
doi: 10.1109/tgrs.2008.2000634
[31] Ahmed R, Siqueira P, Hensley S, Chapman B, Bergen K. A survey of temporal decorrelation from spaceborne L-Band repeat-pass InSAR. Remote Sensing of Environment, 115 (11): 2887-2896, 2011.
doi: 10.1016/j.rse.2010.03.017
[32] Galve J P, Pérez-Peña JV, Azañón JM, Closson D, Caló F, Reyes-Carmona C, ..., Herrera G. Evaluation of the SBAS InSAR service of the European space Agency’s Geohazard Exploitation Platform (GEP). Remote Sensing, 9 (12): 1291, 2017.
doi: 10.3390/rs9121291
[33] Zhao C, Kang Y, Zhang Q, Lu Z, Li B. Landslide identification and monitoring along the Jinsha River catchment (Wudongde reservoir area), China, using the InSAR method. Remote Sensing, 10 (7): 993, 2018.
doi: 10.3390/rs10070993
[34] Massonnet D, Souyris JC. Imaging with synthetic aperture radar, Ed. CRC Press. 2008.
[35] Funk C, Peterson P, Landsfeld M, Pedreros D, Verdin J, Shukla S, Husak G, Rowland J, Harrison L, Hoell A, Michaelsen J. The climate hazards infrared precipitation with stations: a new environmental record for monitoring extremes, Scientific data, 2 (1): 1-21, 2015.
doi: 10.1038/sdata.2015.66
How to Cite
Fustos, I., Moreno-Yaeger, P., Vasquez, D., Morales, B., Silva, A., & Ramirez, E. (2020). Evaluation of Rainfall-Induced Landslides triggering using a multidisciplinary approach. Universitas Scientiarum, 25(2), 277–298. https://doi.org/10.11144/Javeriana.SC25-2.eorl
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Geology and Land Sciences