16 August 2018
Deposit Map: This shows where ash would move in one of thousands of possible simulations following a hypothetical Taupō
eruption modelled by researchers.
Research funded by the Earthquake Commission (EQC) has developed a way of calculating where the ash from a volcano is
most likely to fall, and its thickness, in different parts of New Zealand.
Research team leader Dr. Simon Barker, from Victoria University of Wellington, says that the research involves a
complicated calculation of volcanology, geology and meteorology.
“Volcanic ash is magma that has come to the surface and exploded into tiny particles of glass and crystals. Part of
modelling the ash fall is to understand how big those fragments are likely to be and where they will move through the
atmosphere,” says Dr. Barker.
“We based our work on the giant Taupō volcano. Its explosion was so big around 25,000 years ago that instead of forming
a cone, it left a giant hole in the earth’s crust – now partly filled by Lake Taupō. There’s already been a huge amount
of study on this volcano, so we had a good idea of the size and type of eruption that could happen in the future.
“We created scenarios based on different eruption sizes, spanning several orders of magnitude in volume, added in the
weather data, and ran each scenario 1000 times to see where the ash would fall, and how thick the resulting deposits
Dr. Barker says that weather conditions and wind direction is a big factor in calculating the direction of the ash fall.
“A westerly will blow the ash over Hawke’s Bay and out to sea, and a southerly will blow it up towards Auckland. Another
factor is the shape of the volcanic ash cloud – the ranges are from a weaker “bent” cloud like from Ruapehu in 1995 to
the massive “umbrella” cloud that can blast more than 20km up into the stratosphere. This means that we need to include
wind at different altitudes in the calculation.
“By adding in the interaction with the weather systems, we can also work out how long it will take for the ash to start
falling in different locations. This kind of information can help emergency managers work out which areas need immediate
evacuation. For instance in a large Taupō explosion, in the most common westerly weather pattern, it would take about
three hours for the ash to reach Napier.”
Dr. Barker says that one of the major benefits of the research so far has been the close work between scientists in New
Zealand and the US Geological Survey.
“We’ve been able to use a 3D ash fall model from the USA and add our knowledge about past eruptions from Taupō, which
has been great for us and the US-based researchers in testing ideas on large explosive eruptions. This collaboration
will also let us model what could happen with other volcanoes in New Zealand and this software could play a major role
in eruption forecasting.”
EQC Manager Research Strategy and Investment, Richard Smith, says Dr. Barker’s work has made a significant advance in
helping understand the impact that volcanic activity would have on regions across the country.
“The research has developed a model to shows where in New Zealand would be at risk of ash fall that could affect
buildings, farms and people under different volcanic eruption scenarios. This is a big help for emergency management
planning and risk reduction activity,” says Dr. Smith.