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Volcanic threat in developing countries of the Asia–Pacific region: probabilistic hazard assessment, population risks, and information gaps

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Abstract

The importance of disaster reduction has gained increased awareness within the international development community and thereby highlighted a need for a preliminary assessment of natural hazard risk in developing countries of the Asia–Pacific, including that for volcanic eruption. In this paper, we present a key component of such an assessment, which involved qualifying the frequency and potential consequences of large—Volcanic Explosivity Index of four or more—volcanic eruptions. The frequencies of large eruptions from volcanoes grouped by region were determined from frequency–magnitude plots using data provided by the Smithsonian Institution’s Global Volcanism Program. However, calculated frequencies represent only minimum values due to an incomplete eruption record. Unfortunately, limited data precluded the calculation of eruption frequencies for the Solomon Islands, Fiji and Samoa. A first-order analysis of the populations potentially impacted by large volcanic eruptions suggest that (1) volcanic disasters affecting populations of >100,000 can be expected at least every decade in Indonesia and once every few decades in the Philippines and (2) a volcanic disaster impacting >1% of the population can be expected twice a century in Vanuatu, twice a millennium for Indonesia and the Philippines, and around every millennium in Papua New Guinea and Tonga.

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Notes

  1. A VEI 4 eruption has a bulk tephra volume of >0.1 km3 (Newhall and Self 1982).

  2. It should be noted that the 1815 Tambora eruption is unlikely to be repeated at Tambora in the short-term; however, this example does provide an illustration of the possible impact of an eruption of this magnitude elsewhere.

References

  • Blong R (1982) A time of darkness: local legends and volcanic reality in Papua New Guinea. Aust Natl Univ Press, Canberra, pp 1–257

    Google Scholar 

  • Blong R (2000) Volcanic hazards and risk management. In: Sigurdsson H, Houghton BF, McNutt SR, Rymer H, Stix J (eds) Encyclopedia of volcanoes. Academic Press, Orlando, pp 1215–1227

    Google Scholar 

  • Cronin SJ, Bebbington MS, Lai CD (2001) A probabilistic assessment of eruption recurrence on Taveuni volcano, Fiji. Bull Volcanol 63:274–288

    Article  Google Scholar 

  • EM-DAT: The International emergency events database—www.em-dat.net—Université Catholique de Louvain, Brussels, Belgium

  • Huppert HE, Sparks RSJ (2006) Extreme natural hazards: population growth, globalization and environmental change. Phil Trans R Soc A 364:1875–1888

    Article  Google Scholar 

  • Landscan™ Global population database. Oak Ridge National Laboratory, Oak Ridge. Available at http://www.ornl.gov/sci/landscan/

  • Mercado RA, Lacsamana JBT, Pineda GL (1996) Socioeconomic impacts of the Mount Pinatubo eruption. In: Newhall CG, Punongbayan RS (eds) Fire and Mud: eruptions and lahars of Mount Pinatubo, Philippines. Philippine Institute of Volcanology and University of Washington Press, Seattle, pp 1063–1069

    Google Scholar 

  • Newhall CG, Self S (1982) The volcanic explosivity index (VEI): an estimate of explosive magnitude for historical volcanism. J Geophys Res 87:1231–1238

    Article  Google Scholar 

  • Self S, Rampino MR, Newton MS, Wolff JA (1984) Volcanological study of the great Tambora eruption of 1815. Geology 12:659–663

    Article  Google Scholar 

  • Siebert L, Simkin T (2002) Volcanoes of the world: an illustrated catalog of Holocene volcanoes and their eruptions. Smithsonian Institution, Global Volcanism Program Digital Information Series, GVP-3, (http://www.volcano.si.edu/world/)

  • Simkin T (1993) Terrestrial volcanism in space and time. Annu Rev Earth Planet Sci Lett 21:427–452

    Article  Google Scholar 

  • Simkin T, Siebert L (1994) Volcanoes of the world. Geoscience Press, Tuscon, pp 1–349

    Google Scholar 

  • Stirling MW, Wilson CJN (2002) Development of a volcanic hazard model for New Zealand: first approaches from the methods of probabilistic seismic hazard analysis. Bull N Z Soc Earthq Eng 35:266–277

    Google Scholar 

Download references

Acknowledgments

This work was financially supported by Australian Agency for International Development (AusAID). We gratefully acknowledge Lee Siebert and the Smithsonian Institution’s Global Volcanism Program for supplying eruption data for the Asia–Pacific region, and for Lee Siebert’s insightful review of this manuscript. Alanna Simpson and Phil Cummins publish with the permission of the Chief Executive Officer of Geoscience Australia.

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Correspondence to Alanna Simpson.

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Simpson, A., Johnson, R.W. & Cummins, P. Volcanic threat in developing countries of the Asia–Pacific region: probabilistic hazard assessment, population risks, and information gaps. Nat Hazards 57, 151–165 (2011). https://doi.org/10.1007/s11069-010-9601-y

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