Climate change driving greater slope instability in the Central Andes

Global climate change linked to meso-scale environment modifications such as regional above average precipitations, stronger El Niño-ENSO warm phase, global warming,permafrost degradation, and glacier retreatment could promote slope instability. However,which of these mechanisms is leading landslide...

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Main Authors: Moreiras, Stella Maris, Vergara Dal Pont, Iván Pablo
Other Authors: Mikos, Matjaz, Vilímek, Vít, Sassa, Kyoji, Yueping Yin
Format: Book Part
Language:English
Published: Springer
Subjects:
Online Access:http://hdl.handle.net/11336/99180
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author Moreiras, Stella Maris
Vergara Dal Pont, Iván Pablo
author2 Mikos, Matjaz
Vilímek, Vít
Sassa, Kyoji
Yueping Yin
author_facet Moreiras, Stella Maris
Vergara Dal Pont, Iván Pablo
author_sort Moreiras, Stella Maris
collection CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas)
container_start_page 191
description Global climate change linked to meso-scale environment modifications such as regional above average precipitations, stronger El Niño-ENSO warm phase, global warming,permafrost degradation, and glacier retreatment could promote slope instability. However,which of these mechanisms is leading landslide activity in the high mountain landscape of Central Andes is still uncertain. Otherwise, changes of landslide features as consequence of these climate drivers is rare approached so proposal of effective preventive measures is not viable. The main concern of this research is to elucidate whether climate change is driving more frequent slope instability in the Central Andes. We focus on two key questions of our research: (1) Which landslide features are changing due to climate change? and (2) Which climate change mechanisms are certainly forcing landslides generation in the Central Andes? Our findings explain how the global environment change is shifting slope behavior in the Central Andes increasing landslide frequency and intensity, modifying landslide spatial distribution, shifting initial points of slope instability to higher topography, and generating more complex landslides. Main explanation for this shifting on slope instability behavior is intensified summer rainfall and global warming. Fil: Moreiras, Stella Maris. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; Argentina Fil: Vergara Dal Pont, Iván Pablo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad ...
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op_doi https://doi.org/10.1007/978-3-319-53483-1_22
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http://hdl.handle.net/11336/99180
Moreiras, Stella Maris; Vergara Dal Pont, Iván Pablo; Climate change driving greater slope instability in the Central Andes; Springer; 2018; 191-197
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spelling ftconicet:oai:ri.conicet.gov.ar:11336/99180 2025-01-17T00:16:12+00:00 Climate change driving greater slope instability in the Central Andes Moreiras, Stella Maris Vergara Dal Pont, Iván Pablo Mikos, Matjaz Vilímek, Vít Sassa, Kyoji Yueping Yin application/pdf http://hdl.handle.net/11336/99180 eng eng Springer info:eu-repo/semantics/altIdentifier/url/https://link.springer.com/chapter/10.1007/978-3-319-53483-1_22 info:eu-repo/semantics/altIdentifier/doi/10.1007/978-3-319-53483-1_22 http://hdl.handle.net/11336/99180 Moreiras, Stella Maris; Vergara Dal Pont, Iván Pablo; Climate change driving greater slope instability in the Central Andes; Springer; 2018; 191-197 978-3-319-53482-4 CONICET Digital CONICET info:eu-repo/semantics/restrictedAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ Global warming 0º Isotherm Permafrost degradation Above mean rainfall https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 info:eu-repo/semantics/publishedVersion info:eu-repo/semantics/bookPart info:ar-repo/semantics/parte de libro ftconicet https://doi.org/10.1007/978-3-319-53483-1_22 2023-09-24T20:25:35Z Global climate change linked to meso-scale environment modifications such as regional above average precipitations, stronger El Niño-ENSO warm phase, global warming,permafrost degradation, and glacier retreatment could promote slope instability. However,which of these mechanisms is leading landslide activity in the high mountain landscape of Central Andes is still uncertain. Otherwise, changes of landslide features as consequence of these climate drivers is rare approached so proposal of effective preventive measures is not viable. The main concern of this research is to elucidate whether climate change is driving more frequent slope instability in the Central Andes. We focus on two key questions of our research: (1) Which landslide features are changing due to climate change? and (2) Which climate change mechanisms are certainly forcing landslides generation in the Central Andes? Our findings explain how the global environment change is shifting slope behavior in the Central Andes increasing landslide frequency and intensity, modifying landslide spatial distribution, shifting initial points of slope instability to higher topography, and generating more complex landslides. Main explanation for this shifting on slope instability behavior is intensified summer rainfall and global warming. Fil: Moreiras, Stella Maris. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; Argentina Fil: Vergara Dal Pont, Iván Pablo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad ... Book Part permafrost CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Argentina Argentino Pablo ENVELOPE(-63.717,-63.717,-64.283,-64.283) Stella ENVELOPE(-64.254,-64.254,-65.249,-65.249) 191 197 Cham
spellingShingle Global warming
0º Isotherm
Permafrost degradation
Above mean rainfall
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
Moreiras, Stella Maris
Vergara Dal Pont, Iván Pablo
Climate change driving greater slope instability in the Central Andes
title Climate change driving greater slope instability in the Central Andes
title_full Climate change driving greater slope instability in the Central Andes
title_fullStr Climate change driving greater slope instability in the Central Andes
title_full_unstemmed Climate change driving greater slope instability in the Central Andes
title_short Climate change driving greater slope instability in the Central Andes
title_sort climate change driving greater slope instability in the central andes
topic Global warming
0º Isotherm
Permafrost degradation
Above mean rainfall
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
topic_facet Global warming
0º Isotherm
Permafrost degradation
Above mean rainfall
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
url http://hdl.handle.net/11336/99180