Rainfall-intensity effect on landslide hazard assessment due to climate change in north-western Colombian Andes

ABSTRACT : Landslides triggered by rainfall are one of the most frequent causes of disasters in tropical countries and mountainous terrains. Recent studies show an upsurge in landslide occurrence as an expected impact of human-induced climate change. This paper presents the analysis and implementati...

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Autores:
Aristizábal Giraldo, Edier Vicente
García Aristizábal, Edwin Fabián
Marín Sánchez, Roberto José
Gómez Cardona, Federico
Guzmán Martínez, Juan Carlos
Tipo de recurso:
Article of investigation
Fecha de publicación:
2022
Institución:
Universidad de Antioquia
Repositorio:
Repositorio UdeA
Idioma:
eng
OAI Identifier:
oai:bibliotecadigital.udea.edu.co:10495/32769
Acceso en línea:
https://hdl.handle.net/10495/32769
https://revistas.udea.edu.co/index.php/ingenieria/article/view/343311
Palabra clave:
Desastres naturales
Natural disasters
Desprendimientos de tierra
Landslides
Cambio climático
Climate change
Amenazas naturales
Natural hazards
http://aims.fao.org/aos/agrovoc/c_1666
Rights
openAccess
License
http://creativecommons.org/licenses/by-nc-sa/2.5/co/
id UDEA2_735f177afeeef30a89365f14eb65687b
oai_identifier_str oai:bibliotecadigital.udea.edu.co:10495/32769
network_acronym_str UDEA2
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repository_id_str
dc.title.spa.fl_str_mv Rainfall-intensity effect on landslide hazard assessment due to climate change in north-western Colombian Andes
dc.title.alternative.spa.fl_str_mv Efecto de la lluvia en la amenaza por movimientos en masa asociada al cambio climático
title Rainfall-intensity effect on landslide hazard assessment due to climate change in north-western Colombian Andes
spellingShingle Rainfall-intensity effect on landslide hazard assessment due to climate change in north-western Colombian Andes
Desastres naturales
Natural disasters
Desprendimientos de tierra
Landslides
Cambio climático
Climate change
Amenazas naturales
Natural hazards
http://aims.fao.org/aos/agrovoc/c_1666
title_short Rainfall-intensity effect on landslide hazard assessment due to climate change in north-western Colombian Andes
title_full Rainfall-intensity effect on landslide hazard assessment due to climate change in north-western Colombian Andes
title_fullStr Rainfall-intensity effect on landslide hazard assessment due to climate change in north-western Colombian Andes
title_full_unstemmed Rainfall-intensity effect on landslide hazard assessment due to climate change in north-western Colombian Andes
title_sort Rainfall-intensity effect on landslide hazard assessment due to climate change in north-western Colombian Andes
dc.creator.fl_str_mv Aristizábal Giraldo, Edier Vicente
García Aristizábal, Edwin Fabián
Marín Sánchez, Roberto José
Gómez Cardona, Federico
Guzmán Martínez, Juan Carlos
dc.contributor.author.none.fl_str_mv Aristizábal Giraldo, Edier Vicente
García Aristizábal, Edwin Fabián
Marín Sánchez, Roberto José
Gómez Cardona, Federico
Guzmán Martínez, Juan Carlos
dc.subject.lemb.none.fl_str_mv Desastres naturales
Natural disasters
Desprendimientos de tierra
Landslides
topic Desastres naturales
Natural disasters
Desprendimientos de tierra
Landslides
Cambio climático
Climate change
Amenazas naturales
Natural hazards
http://aims.fao.org/aos/agrovoc/c_1666
dc.subject.agrovoc.none.fl_str_mv Cambio climático
Climate change
dc.subject.proposal.spa.fl_str_mv Amenazas naturales
Natural hazards
dc.subject.agrovocuri.none.fl_str_mv http://aims.fao.org/aos/agrovoc/c_1666
description ABSTRACT : Landslides triggered by rainfall are one of the most frequent causes of disasters in tropical countries and mountainous terrains. Recent studies show an upsurge in landslide occurrence as an expected impact of human-induced climate change. This paper presents the analysis and implementation of two different physically-based models, SHALSTAB and TRIGRS, to evaluate the effect of rainfall on landslide hazard assessment in the north-western Colombian Andes. Intensity-Duration-Frequency curves were used in climate change scenarios for different return periods. According to the results, although higher rainfall intensities increase, landslide occurrence does not escalate in a direct or proportional relationship. Considering a steady infiltration process (SHALSTAB), the results show an expansion of d unstable areas, compared with a transient infiltration process (TRIGRS). A greater influence of rainfall duration instead of rainfall intensity was observed. The results highlight the need for studies that incorporate the scenarios of variability and climate change in the hazard assessment and land planning in the long term.
publishDate 2022
dc.date.accessioned.none.fl_str_mv 2022-12-13T16:00:19Z
dc.date.available.none.fl_str_mv 2022-12-13T16:00:19Z
dc.date.issued.none.fl_str_mv 2022
dc.type.spa.fl_str_mv info:eu-repo/semantics/article
dc.type.coarversion.fl_str_mv http://purl.org/coar/version/c_970fb48d4fbd8a85
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dc.identifier.citation.spa.fl_str_mv E. V. Aristizábal Giraldo, E. García Aristizábal, R. Marín Sánchez, F. Gómez Cardona, and J. C. Guzmán Martínez, “Rainfall-intensity effect on landslide hazard assessment due to climate change in north-western Colombian Andes”, Rev.Fac.Ing.Univ.Antioquia, no. 103, pp. 51–66, Dec. 2022.
dc.identifier.issn.none.fl_str_mv 0120-6230
dc.identifier.uri.none.fl_str_mv https://hdl.handle.net/10495/32769
dc.identifier.doi.none.fl_str_mv 10.17533/udea.redin.20201215
dc.identifier.eissn.none.fl_str_mv 2422-2844
dc.identifier.url.spa.fl_str_mv https://revistas.udea.edu.co/index.php/ingenieria/article/view/343311
identifier_str_mv E. V. Aristizábal Giraldo, E. García Aristizábal, R. Marín Sánchez, F. Gómez Cardona, and J. C. Guzmán Martínez, “Rainfall-intensity effect on landslide hazard assessment due to climate change in north-western Colombian Andes”, Rev.Fac.Ing.Univ.Antioquia, no. 103, pp. 51–66, Dec. 2022.
0120-6230
10.17533/udea.redin.20201215
2422-2844
url https://hdl.handle.net/10495/32769
https://revistas.udea.edu.co/index.php/ingenieria/article/view/343311
dc.language.iso.spa.fl_str_mv eng
language eng
dc.relation.ispartofjournalabbrev.spa.fl_str_mv Rev. Fac. Ing. Univ. Antioquia
dc.rights.spa.fl_str_mv info:eu-repo/semantics/openAccess
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dc.rights.creativecommons.spa.fl_str_mv https://creativecommons.org/licenses/by-nc-sa/4.0/
eu_rights_str_mv openAccess
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dc.publisher.spa.fl_str_mv Universidad de Antioquia, Facultad de Ingeniería
dc.publisher.group.spa.fl_str_mv Grupo de Investigación en Infraestructura (GII)
dc.publisher.place.spa.fl_str_mv Medellín, Colombia
institution Universidad de Antioquia
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spelling Aristizábal Giraldo, Edier VicenteGarcía Aristizábal, Edwin FabiánMarín Sánchez, Roberto JoséGómez Cardona, FedericoGuzmán Martínez, Juan Carlos2022-12-13T16:00:19Z2022-12-13T16:00:19Z2022E. V. Aristizábal Giraldo, E. García Aristizábal, R. Marín Sánchez, F. Gómez Cardona, and J. C. Guzmán Martínez, “Rainfall-intensity effect on landslide hazard assessment due to climate change in north-western Colombian Andes”, Rev.Fac.Ing.Univ.Antioquia, no. 103, pp. 51–66, Dec. 2022.0120-6230https://hdl.handle.net/10495/3276910.17533/udea.redin.202012152422-2844https://revistas.udea.edu.co/index.php/ingenieria/article/view/343311ABSTRACT : Landslides triggered by rainfall are one of the most frequent causes of disasters in tropical countries and mountainous terrains. Recent studies show an upsurge in landslide occurrence as an expected impact of human-induced climate change. This paper presents the analysis and implementation of two different physically-based models, SHALSTAB and TRIGRS, to evaluate the effect of rainfall on landslide hazard assessment in the north-western Colombian Andes. Intensity-Duration-Frequency curves were used in climate change scenarios for different return periods. According to the results, although higher rainfall intensities increase, landslide occurrence does not escalate in a direct or proportional relationship. Considering a steady infiltration process (SHALSTAB), the results show an expansion of d unstable areas, compared with a transient infiltration process (TRIGRS). A greater influence of rainfall duration instead of rainfall intensity was observed. The results highlight the need for studies that incorporate the scenarios of variability and climate change in the hazard assessment and land planning in the long term.RESUMEN : Los movimientos en masa detonados por lluvias son una de las causas más frecuentes de desastres en países tropicales y terrenos montañosos. Estudios recientes muestran un aumento en la ocurrencia de movimientos en masa como un impacto esperado del cambio climático inducido por el hombre. Este documento presenta el análisis y la implementación de dos modelos diferentes basados en la física, SHALSTAB y TRIGRS, para evaluar el efecto de las lluvias en la evaluación de peligros de movimientos en masa en los Andes del noroeste colombiano. Las curvas intensidad-duración-frecuencia se utilizaron en escenarios de cambio climático para diferentes períodos de retorno. Según los resultados, aunque aumentan las intensidades de lluvia más altas, la ocurrencia de movimientos en masa no aumenta en una relación directa o proporcional. Teniendo en cuenta un proceso de infiltración constante (SHALSTAB), los resultados muestran áreas inestables mayores, en comparación con un proceso de infiltración transitoria (TRIGRS). Se observó una mayor influencia de la duración de la lluvia en lugar de la intensidad de la lluvia. Los resultados resaltan la necesidad de estudios que incorporen los escenarios de variabilidad y cambio climático en la evaluación de amenaza y la ordenación del territorio a largo plazo.COL015536716application/pdfengUniversidad de Antioquia, Facultad de IngenieríaGrupo de Investigación en Infraestructura (GII)Medellín, Colombiainfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articlehttp://purl.org/coar/resource_type/c_2df8fbb1https://purl.org/redcol/resource_type/ARTArtículo de investigaciónhttp://purl.org/coar/version/c_970fb48d4fbd8a85info:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by-nc-sa/2.5/co/http://purl.org/coar/access_right/c_abf2https://creativecommons.org/licenses/by-nc-sa/4.0/Rainfall-intensity effect on landslide hazard assessment due to climate change in north-western Colombian AndesEfecto de la lluvia en la amenaza por movimientos en masa asociada al cambio climáticoDesastres naturalesNatural disastersDesprendimientos de tierraLandslidesCambio climáticoClimate changeAmenazas naturalesNatural hazardshttp://aims.fao.org/aos/agrovoc/c_1666Rev. Fac. Ing. Univ. AntioquiaRevista Facultad de Ingeniería Universidad de Antioquia5166103CC-LICENSElicense_rdflicense_rdfapplication/rdf+xml; charset=utf-81051https://bibliotecadigital.udea.edu.co/bitstream/10495/32769/2/license_rdfe2060682c9c70d4d30c83c51448f4eedMD52LICENSElicense.txtlicense.txttext/plain; charset=utf-81748https://bibliotecadigital.udea.edu.co/bitstream/10495/32769/3/license.txt8a4605be74aa9ea9d79846c1fba20a33MD53ORIGINALAristizabalEdier_2022_Rainfallintensityeffect.pdfAristizabalEdier_2022_Rainfallintensityeffect.pdfArtículo de investigaciónapplication/pdf435852https://bibliotecadigital.udea.edu.co/bitstream/10495/32769/1/AristizabalEdier_2022_Rainfallintensityeffect.pdfa1a9a231abf754070ad8e7c7f6b1e5bbMD5110495/32769oai:bibliotecadigital.udea.edu.co:10495/327692022-12-13 11:00:20.374Repositorio Institucional Universidad de Antioquiaandres.perez@udea.edu.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