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VolcaNZ—A volcanic loss model for Auckland,New Zealand
Institution:1. School of Geography, Environment and Earth Sciences, Victoria University of Wellington, PO Box 600, Wellington 6140, New Zealand;2. GNS Science, 1 Fairway Drive, Avalon, PO Box 30-368, Lower Hutt 5040, New Zealand;3. US Geological Survey, 345 Middlefield Road, MS-937, Menlo Park, CA 94025, USA;4. School of Biological, Earth and Environmental Sciences, University College Cork, College Road, T12 YN60 Cork, Ireland;1. GNS Science, PO Box 30 368, Lower Hutt 5040, New Zealand;2. Volcanic Risk Solutions, Institute of Agriculture and Environment, Massey University, Private Bag 11 222, Palmerston North, New Zealand;3. Department of Geological Sciences, University of Canterbury, Private Bag 4800, Christchurch 8140, New Zealand;4. Department of Conservation, Private Bag, Turangi 3334, New Zealand;1. GNS Science, Wairakei Research Centre, Private Bag 2000, Taupo 3352, New Zealand;2. GNS Science, PO Box 30-368, Lower Hutt 5040, New Zealand;1. Department of Geology, Bowling Green State University, Bowling Green, OH 43403, United States;2. School of Earth, Environment and Society, Bowling Green State University, Bowling Green, OH 43403, United States
Abstract:VolcaNZ is a probabilistic volcanic loss model developed for the Auckland Region in New Zealand that currently considers tephra fall hazards from the Auckland Volcanic Field (AVF), Tuhua volcano, Okataina volcanic centre, Taupo volcano, Tongariro volcanic centre and Egmont volcano. In this first version of the model, structural and non-structural damage to residential building envelopes and associated cleanup costs are calculated using Monte Carlo simulation.VolcaNZ assigns a Minimum and Maximum Damage Value to groups of buildings for every simulation, dependent on tephra thickness. A Central Damage Value, representing loss as a percentage of total replacement cost, is then randomly selected between these limits. Even with small-thickness falls, non-structural damage is expected to roof and wall coatings, air-conditioning units, aerials and satellite dishes due to the corrosive and abrasive properties of tephra. An average loss of $583, attributed to non-structural damage, was assigned to all residential buildings impacted by any thickness of tephra greater than 0.1 mm. The costs of tephra removal from buildings, cleaning of building exteriors and tephra transport and disposal are also calculated within the model, assuming much of the cleanup process will be carried out by homeowners.Losses from all simulations are plotted against calculated Average Recurrence Intervals (ARIs) to produce loss curves. Structural damage does not become apparent until ARIs of approximately 8000 years. $1 billion losses, due to structural damage, occur at about 35,000 years and this increases to about $26 billion at 1 million years. Loss due to non-structural damage is constant at approximately $160 million for ARIs above about 600 years. Between 600 and 3000 years, cleanup loss is approximately $50 million, increasing to over $450 million at a return period of 1 million years. At ARIs between 600 and 3000 years, total loss is approximately $210 million, increasing to $10 billion at 100,000 years and over $26 billion at 1 million years. Because we only consider residential building damage and associated cleanup, these values greatly underestimate total loss from the next volcanic event to impact Auckland. Loss calculations will be improved by adding additional hazard and loss modules to VolcaNZ, resulting in a complete catastrophe loss model.
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