Megaincendio de febrero de 2024 en la conurbación de la provincia de Valparaíso y zonas de interfaz urbano-forestal, Chile

Descripción del Articulo

On February 2 and 3, 2024, the conurbation of the Province of Valparaíso, Chile, was affected by a catastrophic megafire. In this context, the article presents the results of a qualitative study with an exploratory-descriptive approach, aimed at analyzing the event from the perspective of the contri...

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Detalles Bibliográficos
Autor: Castañeda-Meneses, Patricia Lorena
Formato: artículo
Fecha de Publicación:2025
Institución:Pontificia Universidad Católica del Perú
Repositorio:PUCP-Institucional
Lenguaje:español
OAI Identifier:oai:repositorio.pucp.edu.pe:20.500.14657/204993
Enlace del recurso:https://revistas.pucp.edu.pe/index.php/Kawsaypacha/article/view/30436/27967
http://hdl.handle.net/20.500.14657/204993
https://doi.org/10.18800/kawsaypacha.202502.D012
Nivel de acceso:acceso abierto
Materia:Climate change
Environmental disasters
Fourth generation fires
Fifth generation fires
Megafire
Wildland-urban interface zones
Valparaíso, Chile
Cambio climático
Desastres ambientales
Incendios de cuarta generación
Incendios de quinta generación
Megaincendio
Zonas urbano-forestales
https://purl.org/pe-repo/ocde/ford#2.07.01
Descripción
Sumario:On February 2 and 3, 2024, the conurbation of the Province of Valparaíso, Chile, was affected by a catastrophic megafire. In this context, the article presents the results of a qualitative study with an exploratory-descriptive approach, aimed at analyzing the event from the perspective of the contribution of wildland-urban interface zones to the occurrence of the disaster. The findings show that the wildland-urban interface zones of the Valparaíso conurbation constituted a powerful fuel load that increased the territory’s vulnerability to the megafire. This vulnerability was exacerbated by high temperatures, low humidity, and strong winds, resulting in a high destructive potential that reached an unprecedented level of devastation. There is a high risk that such an event will recur in the territory, given the structural geographic conditions that favor the presence of wildland-urban interface zones, compounded by a decade-long megadrought, the existence of fast-growing forest plantations on urban margins, and human impact. It is concluded that the occurrence of the megafire is linked at a macro level to the process of climate change and its consequences—megadrought and heat waves—factors that, in this case, contributed to the development of a catastrophic event.
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