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Article: The characteristics of the Mocoa compound disaster event, Colombia

TitleThe characteristics of the Mocoa compound disaster event, Colombia
Authors
KeywordsEl Niño
Compound mountain hazards
Debris flow
Rainfall
Tropical alpine area
Vegetation coverage
Issue Date2018
Citation
Landslides, 2018, v. 15, n. 6, p. 1223-1232 How to Cite?
Abstract© 2018, The Author(s). A rainfall-induced compound disaster happened in Mocoa in the pre-dawn hours of 1 April 2017. More than 300 people were killed, and a large number of houses and roads were destroyed in the worst catastrophe in the history of Mocoa. To investigate this disaster, a detailed interpretation was carried out using high-resolution images. Analysis of disaster characteristics based on satellite image revealed that the disaster could be identified as a consequence of compound mountain hazards including landslides, debris flows, and mountain torrents. The mountain hazards converged in the mountain watershed, which amplified the disaster’s effects. Analysis considers that this disaster is the result of heavy rainfalls. Moreover, in-depth interpretation of rainfall data and satellite images spanning over 16 years reveals that the previous El Niño event (2014–2016) also played an important role, which caused reduced rainfall and vegetation coverage. The long period of drought brought by El Niño affected the growth of vegetation and reduced the ability of vegetation to cope with heavy rainfalls. The results reveal that both antecedent rainfalls and climate impact need to be taken into consideration for mountain hazard analysis.
Persistent Identifierhttp://hdl.handle.net/10722/273621
ISSN
2023 Impact Factor: 5.8
2023 SCImago Journal Rankings: 2.020
ISI Accession Number ID

 

DC FieldValueLanguage
dc.contributor.authorCheng, Deqiang-
dc.contributor.authorCui, Yifei-
dc.contributor.authorSu, Fenghuan-
dc.contributor.authorJia, Yang-
dc.contributor.authorChoi, Clarence Edward-
dc.date.accessioned2019-08-12T09:56:10Z-
dc.date.available2019-08-12T09:56:10Z-
dc.date.issued2018-
dc.identifier.citationLandslides, 2018, v. 15, n. 6, p. 1223-1232-
dc.identifier.issn1612-510X-
dc.identifier.urihttp://hdl.handle.net/10722/273621-
dc.description.abstract© 2018, The Author(s). A rainfall-induced compound disaster happened in Mocoa in the pre-dawn hours of 1 April 2017. More than 300 people were killed, and a large number of houses and roads were destroyed in the worst catastrophe in the history of Mocoa. To investigate this disaster, a detailed interpretation was carried out using high-resolution images. Analysis of disaster characteristics based on satellite image revealed that the disaster could be identified as a consequence of compound mountain hazards including landslides, debris flows, and mountain torrents. The mountain hazards converged in the mountain watershed, which amplified the disaster’s effects. Analysis considers that this disaster is the result of heavy rainfalls. Moreover, in-depth interpretation of rainfall data and satellite images spanning over 16 years reveals that the previous El Niño event (2014–2016) also played an important role, which caused reduced rainfall and vegetation coverage. The long period of drought brought by El Niño affected the growth of vegetation and reduced the ability of vegetation to cope with heavy rainfalls. The results reveal that both antecedent rainfalls and climate impact need to be taken into consideration for mountain hazard analysis.-
dc.languageeng-
dc.relation.ispartofLandslides-
dc.rightsThis work is licensed under a Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License.-
dc.subjectEl Niño-
dc.subjectCompound mountain hazards-
dc.subjectDebris flow-
dc.subjectRainfall-
dc.subjectTropical alpine area-
dc.subjectVegetation coverage-
dc.titleThe characteristics of the Mocoa compound disaster event, Colombia-
dc.typeArticle-
dc.description.naturepublished_or_final_version-
dc.identifier.doi10.1007/s10346-018-0969-1-
dc.identifier.scopuseid_2-s2.0-85046030341-
dc.identifier.volume15-
dc.identifier.issue6-
dc.identifier.spage1223-
dc.identifier.epage1232-
dc.identifier.eissn1612-5118-
dc.identifier.isiWOS:000432127000015-
dc.identifier.issnl1612-510X-

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