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Título : Mapping hazard zones, rapid warning communication and understanding communities: primary ways to mitigate pyroclastic flow hazard
Otros títulos : Mapeo de zonas de peligro, comunicación de alerta rápida y comprensión de las comunidades: formas principales de mitigar el peligro de flujo piroclástico
Autor: Lavigne, Franck
Morin, Julie
Wulan Mei, Estuning Tyas
Calder, Eliza
Usamah Null, Muhibuddin Null
Nugroho, Ute
Correspondencia: Lavigne, Franck, franck.lavigne@univ-paris1.fr
Palabras clave : Crisis management
Evacuation
Pyroclastic density currents
Risk communication
Risk perception
Warning
Área de conocimiento FRASCATI amplio: 1. Ciencias Naturales y Exactas
Área de conocimiento FRASCATI detallado: 1.5.8 Ciencias del Medioambiente
Área de conocimiento FRASCATI específico: 1.5 Ciencias de la Tierra y el Ambiente
Área de conocimiento UNESCO amplio: 05 - Ciencias Físicas, Ciencias Naturales, Matemáticas y Estadísticas
ÁArea de conocimiento UNESCO detallado: 0521 - Ciencias Ambientales
Área de conocimiento UNESCO específico: 052 - Medio Ambiente
Fecha de publicación : 2018
Paginación: 107-119
Fuente: Advances in Volcanology
metadata.dc.identifier.doi: 10.1007/11157_2016_34
Editor: Springer
Tipo: CAPÍTULO DE LIBRO
Abstract: 
Protection against the consequences of Pyroclastic Density Currents (PDCs) is almost impossible due to their high velocity, temperature, sediment load and mobility. PDCs therefore present a challenge for volcanic crisis management in that specific precautionary actions, essentially evacuations, are required to reduce loss of life. In terms of crisis communication for PDC hazards, there are three challenging questions that arise in terms of reducing risk to life, infrastructure and livelihoods. (1) How do we accurately communicate the hazardous zones related to potential PDC inundation? The areas exposed to PDC hazard are difficult to assess and to map. In terms of risk/crisis management, the areas considered at risk are usually those that were affected by PDCs during previous eruptive episodes (decades or centuries ago). In case of “larger-than-normal” eruptions, the underestimation of the hazard zone may lead to refusals to evacuate in the “newly” threatened area. Another difficulty in assessing the PDC hazard zones relate to their transport processes that allow surmounting of the topography and in some cases across the surface of water. Therefore warning systems must be able to cover vast areas in a minimum of time. (2) How do we efficiently warn people in time? PDCs are extremely mobile and fast. It is therefore necessary to raise the alert early enough before the onset of the first PDCs. A challenging question in terms of crisis communication is related to the type of tools used by the local authorities, modern and traditional tools both of which have advantages and disadvantages. (3) Why are people reluctant to evacuate? Local inhabitants can be reluctant to evacuate during a crisis if traditional warning signs or signals they are familiar with are lacking, if they don’t receive both traditional and official warning, and because they may lose their livelihoods. Thus a deeper understanding of the at‐risk communities and efficient dissemination of information are key issues in order to reduce vulnerability in PDC hazard regions. © 2017, The Author(s).
Resumen : 
Protection against the consequences of Pyroclastic Density Currents (PDCs) is almost impossible due to their high velocity, temperature, sediment load and mobility. PDCs therefore present a challenge for volcanic crisis management in that specific precautionary actions, essentially evacuations, are required to reduce loss of life. In terms of crisis communication for PDC hazards, there are three challenging questions that arise in terms of reducing risk to life, infrastructure and livelihoods. (1) How do we accurately communicate the hazardous zones related to potential PDC inundation? The areas exposed to PDC hazard are difficult to assess and to map. In terms of risk/crisis management, the areas considered at risk are usually those that were affected by PDCs during previous eruptive episodes (decades or centuries ago). In case of “larger-than-normal” eruptions, the underestimation of the hazard zone may lead to refusals to evacuate in the “newly” threatened area. Another difficulty in assessing the PDC hazard zones relate to their transport processes that allow surmounting of the topography and in some cases across the surface of water. Therefore warning systems must be able to cover vast areas in a minimum of time. (2) How do we efficiently warn people in time? PDCs are extremely mobile and fast. It is therefore necessary to raise the alert early enough before the onset of the first PDCs. A challenging question in terms of crisis communication is related to the type of tools used by the local authorities, modern and traditional tools both of which have advantages and disadvantages. (3) Why are people reluctant to evacuate? Local inhabitants can be reluctant to evacuate during a crisis if traditional warning signs or signals they are familiar with are lacking, if they don’t receive both traditional and official warning, and because they may lose their livelihoods. Thus a deeper understanding of the at‐risk communities and efficient dissemination of information are key issues in order to reduce vulnerability in PDC hazard regions. © 2017, The Author(s).
URI : https://www.scopus.com/inward/record.uri?eid=2-s2.0-85064944742&doi=10.1007%2f11157_2016_34&partnerID=40&md5=356ae56e4f3048d33708c2564279c1cf
ISBN : 978-3-319-44095-8
ISSN : 2364-3277
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