Experts Comments April 11 | Earthquake in Indonesia PDF Print E-mail
Earthquake in Indonesia

Below are some comments from Canadian researchers as well as some comments collected by our colleagues at the UK and Australian Science Media Centres on this morning's earthquake in Indonesia. Feel free to use these quotes in your stories. If you need help reaching an expert for this or any other story, please call us at 613-249-8209.

Tad Murty
Adjunct Professor in the Department of Civil Engineering, University of Ottawa
More information on Tad Murty

My career was mostly with the federal government. When I was with the government, I was in charge of research and programming of tsunami early warning systems. I was involved in developing computer programs for the Canadian early warning system. The system is similar in Canada, Indonesia, India, everywhere, because the same principles apply.

If there is a large earthquake far from the ocean, on land, there is no tsunami. The earthquake itself needs to be shallow - some 20 or 30 km below the ocean bottom before it can generate a tsunami, and it needs to be a dip slip, like a subduction. The movement needs to be vertical, not horizontal. In today's earthquake in Indonesia, the movement was horizontal, because the Indian plate slid past the Burmese plate.
In 2004, the Indian Plate went under the Burmese plate, and tens of cubic kilometres of water were suddenly displaced and piled at the ocean surface. This is what causes a tsunami.

How do early warning systems work?

There are many different kinds of detectors, and one can never depend on just one set of detectors. First, the earthquake itself has to be detected. This is done by seismographs, and these are mostly on land. Earthquake waves propagate through the interior of Earth's crust, as well as earth's surface.
We also have ocean-bottom pressure sensors. There are several dozen all around the ocean. They are the first indicators of a tsunami. Then we have tidal gauges, on land but on the coast, put in the water, and they catch the tsunami coming in. By then it's usually too late.

Indonesia has an early warning system. But all the international agencies work together. They are all part of the Intergovernmental Oceanographic Commission, and that's all coordinated by UNESCO.

Have there been any changes in the tsunami warning system since 2004?

Following the disaster in 2004, the first early warning systems were placed in the Indian Ocean.
With each disaster we learn new things. On the scientific side, we already know the physical principles but we fine-tune our computer models and we make our instruments more precise. The physical process is the same. On the social and economic side, there has been progress, for example, with evacuations.
When a cyclone hits in the area, almost all the damage and loss of life comes from the storm surge. In developing countries like India and Bangladesh, they use a 'vertical evacuation system'. Because you can't evacuate millions of people from the area, the infrastructure and the roads just aren't there. So they built cyclone shelters on the coast, that are well built and can withstand storm surges and cyclones. In the US, they use a 'horizontal evacuation system', because the highways are good and the roads are there so people just move away from the coast.

In the 2004 tsunami, none of the cyclone shelters in India were damaged. So they thought maybe they could use them for tsunamis as well. Now, if there has to be an evacuation for a tsunami, they use the cyclone shelters.

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Fiona Darbyshire
Professor, Centre de recherche en géochimie et géodynamique (GÉOTOP-UQAM-McGill)
More information on Fiona Darbyshire

La région de l’océan Indien à l’ouest / nord-ouest de Sumatra a subi deux grands tremblements de terre ce matin, de magnitudes 8.6 et 8.2, ainsi que quelque dizaines de répliques de magnitude entre 5 et 6. On peut prévoir d’autres répliques de ce type pendant les heures et jours à venir, et il reste toujours la possibilité de répliques plus fortes dans la région, associés à la redistribution des forces et contraintes causées par les séismes initiaux. Les répliques sont distribuées sur une région de quelques centaines de kilomètres.

Les plus grands séismes ont été ressentis dans toute la région de l’est de l’océan Indien, y compris en Inde, à Sumatra, en Indonésie, à Singapore et en Malaisie, mais pour la majorité des endroits les secousses ont été assez modérées en intensité. Un avis de possibilité de tsunami a été publié, mais heureusement il n’y avait rien significatif.

Les tremblements de terre se situent à environ 100 à 200 km vers le sud-ouest de la fosse associée à la zone de subduction de Sumatra, où la plaque Indo-Australienne plonge en-dessous de l’Indonésie à un taux de ~5 cm par année. Cette zone de subduction a produit le tremblement de terre de magnitude 9,1 de 2004, ainsi que plusieurs séismes de magnitude >7 depuis 2004. Les tremblements de terre d’aujourd’hui sont un peu différents de la majorité des séismes de cette région : au lieu d’être un mouvement chevauchant (faille inverse), le mouvement a été en direction horizontale, c.à.d. une faille décrochante (« strike-slip fault »). Ce type de mouvement dans cette région est plus rare que les failles inverses de la zone de subduction, mais il y a eu quelques séismes de ce type depuis 2004. La direction de mouvement correspond bien avec la direction des structures dans la plaque océanique de cette région.

La surveillance des tremblements de terre mondiaux est faite grâce aux réseaux régionaux, nationaux et globaux de sismomètres, qui peuvent enregistrer toutes les secousses produites. Ces appareils sont très sensibles; les ondes sismiques des tremblements de terre d’aujourd’hui sont bien enregistrées par les sismomètres au Canada, par exemple. Après le tremblement de terre, l’analyse des données nous fournit l’information de la localisation, de la magnitude, du type de mouvement, etc. Les informations donnent la possibilité des avertissements à court-terme. Dans le cas d’un tremblement de terre sous-marin, les informations sont utiles pour savoir si un avis de possibilité de tsunami est nécessaire.

Pour les grands tremblements de terre de Sumatra, un avertissement de tsunami est maintenant publié pour n’importe quel type de séisme, parce qu’il y a toujours des risques. Cependant,  un tsunami est moins probable dans le cas d’une faille décrochante comme les séismes d’aujourd’hui, parce que le mouvement sur la faille est horizontal; les mouvements verticaux associés aux failles inverses sont significativement plus susceptibles de déplacer la quantité d’eau nécessaire pour causer un tsunami. Depuis 2004, un nouveau système de surveillance des tsunamis a été mis en place dans et autour de l’océan Indien, afin de réduire la probabilité de fatalités.

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Comments from UK-Science Media Centre:

Expert reaction to Indonesian earthquake and tsunami warning

Dr Andy Gibson, Director of the Centre for Applied Geoscience at the University of Portsmouth, said:

"From our experience of the tsunami in 2004, we know that the worst affected regions are those low lying areas immediately adjacent to the coast. Broadly speaking, the shallower the slope of the shore, the greater the susceptibility to wave run-up.  Areas farther inland could be affected if the tsunami was able to move along a water inlet. Lessons learned from that tsunami go far beyond early warning systems, residents are encouraged to take part in emergency drills which may include understanding escape routes, identifying safe havens and knowing when it is safe to return to the coast.

"Early indications are that this earthquake and tsunami risk are actually much smaller than that of 2004, but it will be some time before the pattern of any damage is known. It is always difficult to estimate damage as any tsunami wave depends upon many factors such as the volume of water displaced, the angle it approaches the coast, tidal conditions, the gradient of land offshore and onshore and of course, what is found on the shoreline."


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Dr Susanne Sargeant, Seismologist & NERC Knowledge Exchange Fellow, British Geological Survey, said:

“Critical information that is required to assess the potential for a tsunami is the location, magnitude, depth and faulting mechanism. Tsunamis are caused when vertical displacement of the seafloor occurs. In the case of the 11 April earthquake, an earthquake of this magnitude (8.7 Mw) has the potential to generate an ocean-wide tsunami. However, although the earthquake is relatively shallow and offshore, the data indicate that the earthquake was the result of movement on a strike-slip fault. Strike slip earthquakes are caused when two blocks move horizontally past each other. Such an earthquake would not lead to the vertical displacement of the sea floor that would be required to generate a tsunami. Consequently, the potential for a large tsunami from this earthquake is likely to be low.

“The alert from the Pacific Tsunami Warning Centre issued after the earthquake indicates that an Indian Ocean wide tsunami watch is in place. See http://ptwc.weather.gov/ptwc/text.php?id=indian.TSUIOX.2012.04.11.1054 for info. Arrival time estimates issued by PTWC indicate that the initial wave (had one been generated) would have reached Banda Aceh a little under an hour after the earthquake. Whether any wave has been observed in this region has yet to be confirmed. The PTWC alert gives estimated arrival times for other locations in the Indian Ocean.

“The Sunda trench region is highly active. Earthquakes here are related to subduction of the Indian plate beneath Eurasia. Today's earthquake occurred on a structure related to the subduction that is occurring here. The tectonics of the region are complex and large earthquakes are relatively frequent. The aftershock sequence has started and this includes an earthquake of magnitude 8.3.

“Although large, the 08:38 UTC earthquake is located approximately 400 km from the coast of Banda Aceh. As such, the potential for significant damage caused by ground shaking is likely to be relatively low although the actual impact of the earthquake in this region has yet to be confirmed.”


Q&A ON AFTERSHOCKS Dr Bruce D. Malamud, Reader of Natural and Environmental Hazards, Department of Geography, King's College London:

How many and what size aftershocks might we expect?
“When an earthquake occurs, it releases stress that has built up over time, along a fault. However, in addition to releasing stress, it redistributes the stress along that fault, and sometimes these will be redistributed to other nearby faults. In the case of the 11 April 2012 earthquake that occurred off the west coast of Northern Sumatra, the preliminary estimate of magnitude by the USGS is M8.6, and hundreds of km of fault may have been affected. With the redistribution of stress, aftershocks occur, for weeks, to months (and sometimes years) after the main shock. The magnitude 8.6 earthquake will result in aftershocks occurring all along the fault on which the original earthquake occurred. Some scientists say that one can expect aftershocks as much as 1 unit less than the original shock. So in this case, we might expect aftershocks of all sizes, but as big as a magnitude of about 7.6 (which would be in itself a concern of potentially triggering a tsunami).

How long might aftershocks continue for?
“After an earthquake occurs along a fault, stress is released in parts. But then, part of this stress is redistributed to other parts of the fault. This means that they are now more likely to become unstable, with many subsequent earthquakes. Aftershocks can continue for weeks and months after the main shock (the biggest earthquake in the sequence), sometimes even years.

How frequent have earthquakes been over the last century and are they increasing?
“One of the questions that has been asked by many is whether there have been more frequent large earthquakes in the last few years. Let’s take as a ‘large’ earthquake one with moment magnitude 7. The number of earthquakes per year with moment magnitude greater than or equal to 7 varies certainly, year to year, but the average from 1900 to present is about 17 magnitude 7 or greater earthquakes per year (compared to about 1 magnitude 8 or greater earthquake). If we just look at 1990 to 2010, then the average was about 15 magnitude 7 or greater earthquakes per year. And if we look at the last three years, then the average is also 15 of this size earthquake per year. So, no, the actual number of very large earthquakes is not increasing over time. It fluctuates year to year, with some years less and some years more.

How much energy is released in a magnitude 7 earthquake?
“Equivalent to the energy released in half a megaton nuclear bomb.

How much energy is released in a magnitude 9 earthquake?
“Equivalent to 1000 times the energy released in a magnitude 7 earthquake, or one thousand half-megaton nuclear bombs. If we converted this to energy, this would be roughly enough to power every home in the USA for 50 days.

How accurately can an earthquake like this be predicted? Why is it so difficult to predict the timing of earthquakes?
“For a complete prediction, we need to tell people when a disaster will occur, where, and how big. As scientists, we have a good idea of where large events might occur based on written and instrumental records of past events. So for instance, we know that Indonesia is near subduction zones, and that there is an extensive history of earthquakes in the past, so we know that Indonesia is likely to experience earthquakes. Based on these past records, we can also forecast the chance that a given size or larger earthquake might occur, in a given year. This is called probabilistic hazard forecasting, and has been very useful in telling us about how big we might expect, on average, each year. But true prediction is much more difficult, where we tell people that ‘next week there will be an earthquake of magnitude of 9’. Although scientists have been trying for many years to predict earthquakes (the when and how big), they so far have not succeeded, but are still working at it.”


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QUOTES FROM THE AUSTRALIAN SCIENCE MEDIA CENTRE:

Kevin McCue is an adjunct professor at CQUniversity, President of the Australian Earthquake Engineering Society and Director of the Australian Seismological Centre.
“According to the USGS website the magnitude 8.7 earthquake occurred well offshore, at least 300 km west of Sumatra so the damage onshore on Sumatra is likely to be minimal. The magnitude may well be decrease to 8.5 or 8.4 after more analysis. The epicentre is well west of the plate boundary and in the Indian Ocean, a fracture along the hinge where the subducting slab of oceanic crust starts bending downward and under Sumatra. The mechanism seems to have been predominantly strike-slip i.e. no substantial vertical displacement of the sea floor so any tsunami would be small and local.”

Professor James Goff is Director of the Australia-Pacific Tsunami Research Centre and Natural Hazards Research Laboratory, University of New South Wales.
“Like everyone else who just heard this news, we are now waiting to see what comes to pass. BUT, the tsunami warning system has worked well, and a tsunami watch is in place. Many people have self-evacuated and fortunately, because of the incredible amount of tsunami-related work in the region, since the massive 2004 event authorities and the general public are considerably better prepared this time. Those of us who are not in the region at the moment will now be monitoring developments over the next few hours. It appears to be a strike-slip fault which means that it is unlikely to generate a large tsunami, but then we hear that at least small ones have been reported. Of course such a large shake could generate submarine landslides (like in Haiti) which can also generate tsunamis. We continue to watch.”

Professor Kevin Furlong from Pennsylvania State University
“The 11 April 2012, Mw 8.7 earthquake west of Banda Aceh, Sumatra, Indonesia is a very large earthquake within the Indo-Australian plate. Although it is within the plate, its occurrence is almost certainly linked to the plate interactions between Indo-Australian plate and Indonesia (part of the Sunda segment of the Eurasian plate). This earthquake reflects a style of faulting (strike-slip) which involves principally horizontal motion, and thus is unlikely to generate a significant tsunami; although very strong ground shaking would be felt on Sumatra. This is also an extremely large magnitude earthquake for this style of faulting, meaning that it likely involved substantial fault movement, and the fault likely extends for 200+ km. This earthquake is of the same style of faulting and in approximately the same location as a Mw 7.2 earthquake on January 10, 2012. Although this earthquake was within the Indo-Australian plate, any earthquake of this size will change the stress regimes acting on the nearby plate boundaries. The result is that stress conditions on the subduction plate boundary beneath Sumatra have changed, although the implications of that change are uncertain.”


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Dr David Rothery, who runs the Open University’s Volcanoes, Earthquakes and Tsunamis course, said:

“Today’s M8.7 quake in the Indian Ocean offshore of Sumatra has the potential to cause a tsunami that could cause devastation to coasts all around the Indian ocean. A tsunami warning from the Pacific Tsunami Warning Centre predicts tsunami wave arrival at Banda Aceh (Sumatra) 10:31 BST, and Sri  Lanka between 11.30 and 12.30 BST.
http://ptwc.weather.gov/ptwc/text.php?id=indian.TSUIOX.2012.04.11.0845

“A tsunami detection buoy (a DART station) in the Bay of Bengal http://www.ndbc.noaa.gov/station_page.php?station=23227
detected a wave with an amplitude of 30 cm in deep water (see figs below), which has the potential to become several times higher as it approaches the shore.

“Today’s quake was probably about ten times less energetic than the M9.1 quake that caused the 26 Dec 2004 Indian Ocean tsunami. In addition, the nature of the quake, on the bending Indian ocean floor as it approaches the Sunda Trench (rather than a megathrust quake in the trench itself) may mean that the displacement of water to trigger the tsunami is less bad; the motion of the sea bed is different to that which occurred in 2004.”