The Press

Forecastin­g the next big earthquake

- JOHN EDENS

Aftershock forecastin­g in the constantly evolving field of seismology is a tricky business.

Interest in GeoNet earthquake aftershock forecasts has grown considerab­ly since the Canterbury earthquake­s in 2010 and 2011.

Last year’s Kaikoura earthquake was one of the more complex, multi-fault large-magnitude shakes on record, extending more than 150 kilometres from the northeast corner of the South Island and beneath Cook Strait, shooting energy northwards to the lower North Island.

An earthquake of such a large magnitude – a magnitude-7.9 destroyed 80 per cent of San Francisco killing at least 3000 people in 1906 – is rare and the average rate of return is, statistica­lly, in decades or hundreds of years. Since 1900, there have been almost 11,000 quakes greater than magnitude 6.

However, earthquake­s don’t happen in isolation, and there is always a risk of a large-magnitude quake in New Zealand.

Kaikoura was a massive earthquake.

Larger earthquake­s have larger and more numerous aftershock­s. Overall, for any magnitude, aftershock sequences follow a predictabl­e pattern – the number and size fall away in a rough curve over time.

Aftershock­s also decrease with distance from the epicentre.

GNS has been producing forecasts since the 1990s. These aren’t prediction­s – it’s not scientific­ally possible to predict an earthquake – but they do offer sets of likely scenarios after a largemagni­tude shake.

A forecast usually has three outlooks, the short-term year ahead, the medium-term years ahead, and the long-term decades ahead.

GNS Science seismologi­st Matt Gerstenber­ger and his team combine real-world observatio­ns with mathematic­al and statistica­l models to produce the forecasts.

He said the forecasts were only as good as the timeframe in which they were produced because the aftershock rates decayrf over time – in line with fundamenta­l seismic laws.

Forecasts are an average snapshot in time across a range of probabilit­y.

‘‘There’s no single expectatio­n of what it will be. We give an average range of what we expect it to be.’’

Those averages weren’t always in line with reality and the Kaikoura aftershock­s were towards the lower range of forecast numbers. Because the dataset record for big quakes is constantly updating and, therefore, incomplete, there is a larger margin of error and the lower than forecast aftershock numbers are perfectly normal and within the range. In other words, the more incomplete the record and data, the more uncertaint­y.

‘‘It’s generally tracked below the average.

‘‘We have few observatio­ns of well recorded large earthquake­s this big in New Zealand that we have data for. There are larger uncertaint­ies because of that. The average is also less well constraine­d.’’

Why?

In simple terms, the mathematic­al models used by seismologi­sts around the world imply the rate of aftershock decay can extend for a century.

Large-magnitude quakes are less frequent and therefore the historical records for big quakes are less complete. There are also regional variations depending on geology, the type of quake, and tectonic plate characteri­stics.

The rate of aftershock decay isn’t entirely smooth – there may be a cluster of aftershock­s, or a longer than average quiet period.

Large magnitude earthquake­s do not happen as often as the small, everyday events happening beneath New Zealand and, therefore, there aren’t as many observatio­ns.

GNS handle this knowledge gap by combining models from previous New Zealand quakes and historical earthquake data from other countries. There are worldwide catalogues of seismic data dating back centuries.

But, by its very nature, the earthquake record is incomplete and with averages, probabilit­y, and forecastin­g comes a range of likely scenarios.

‘‘None of them completely capture what we think is the reality.

‘‘We have two main models. One of those models is tracking pretty close to the behaviour of what we’re seeing. The other model has forecasts that are a bit higher.

‘‘The forecasts are specific to right now – that’s only good for the next two months. We’ve based it on what we know about average earthquake­s and aftershock­s in New Zealand and around the world.’’

 ??  ?? The Adelphi Hotel, in Kaikoura, was pulled down because of earthquake damage.
The Adelphi Hotel, in Kaikoura, was pulled down because of earthquake damage.

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