OREGAN: On Dec 22, a 64-hectare chunk of Anak Krakatoa volcano, in Indonesia, slid into the ocean following an eruption. This landslide created a tsunami that struck coastal regions in Java and Sumatra, killing at least 426 people and injuring 7,202.
Satellite data and helicopter footage taken on Dec 23 confirmed that part of the southwest sector of the volcano had collapsed into the sea.
In a report on Dec 29, Indonesia’s Centre of Volcanology and Geological Hazard Mitigation said that the height of Anak Krakatoa went from 338m above sea level to 110m.
Although it was very difficult to forecast if and when Anak Krakatoa would partially collapse, the characteristics of the waves produced by such event were not totally unpredictable.
Although most tsunamis have a seismic origin (for example, the Sumatra, Indonesia one in 2004 and at Tohoku, Japan in 2011), they may also be triggered by phenomena related to large volcanic eruptions.
Tsunamis caused by volcanoes can be triggered by submarine explosions or by large pyroclastic flows – a hot mix of volcanic gases, ash and blocks travelling at tens of miles per hour – if they enter in a body of water.
Another cause is when a large crater forms due to the collapse of the roof of a magma chamber – a large reservoir of partially molten rock beneath the surface of the Earth – following an eruption.
At Anak Krakatoa, a large, rapidly sliding mass that struck the water led to the tsunami. These types of events are usually difficult to predict as most of the sliding mass is below water level.
These volcanic landslides can lead to major tsunamis. Landslide-triggered tsunamis, similar to what happened at Anak Krakatoa, occurred in December 2002 when 17 million cubic metres of volcanic material from Stromboli volcano in Italy triggered a 8m-high wave.
More recently in June 2017, a 10m-high wave was triggered by a 45 million cubic metre landslide in Karrat Fjord, in Greenland, causing a sudden surge of seawater that wreaked havoc and killed four people in the fishing village of Nuugaatsiaq located about 20km away from the collapse.
These two tsunamis had few fatalities as they occurred either in relatively isolated locations (Karrat Fjord) or during a period of no tourist activity (Stromboli). This was obviously not the case at Anak Krakatoa on Dec 22.
CHILD OF KRAKATOA
This part of the world is well-experienced with destructive volcanoes. In Aug 26 to Aug 28, 1883, Krakatoa volcano experienced one of the largest volcanic eruptions ever recorded in human history, generating 15m tsunami waves and causing more than 35,000 casualties along the coasts of the Sunda Strait in Indonesia.
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Nearly 45 years after this 1883 cataclysmal eruption, Anak Krakatoa (“Child of Krakatoa” in Indonesian) emerged from the sea in the same location as the former Krakatoa, and grew to reach about 338m, its maximum height on Dec 22, 2018.
Many tsunamis were produced during the 1883 eruption. How they were generated is still debated by volcanologists, as several volcanic processes may have acted successively or together.
TSUNAMIS REACHING THE SUNDA STRAIT IN UNDER AN HOUR
I worked on this very problem in 2011 with my colleagues but the short time left in my postdoctoral fellowship had me shift direction away from the 19th-century explosion to focus on Anak Krakatoa.
In 2012, we published a paper entitled Tsunami Hazards Related to a Flank Collapse of Anak Krakatoa Volcano, Sunda Strait, Indonesia.
This study started with the observation that Anak Krakatoa was partly built on a steep wall of the crater resulting from the 1883 eruption of Krakatoa. We thus asked ourselves “what if part of this volcano collapses into the sea?”
To tackle this question, we numerically simulated a sudden southwestwards destabilisation of a large part of the Anak Krakatoa volcano, and the subsequent tsunami formation and propagation. We showed results projecting the time of arrival and the amplitude of the waves produced, both in the Sunda Strait and on the coasts of Java and Sumatra.
When modelling landslide-triggered tsunamis, several assumptions need to be made concerning the volume and shape of the landslide, the way it collapses (in one go versus in several failures), or the way it propagates. In that study, we envisioned a somewhat “worst-case scenario” with a volume of 0.28 cubic kilometres of collapsed volcanic material – the equivalent of about 270 Empire State buildings.
We predicted that all the coasts around the Sunda Strait could potentially be affected by waves of more than 1m less than an hour after the event.
Unfortunately, it seems that our findings were not that far to what happened on Dec 22: The observed time of arrival and amplitude of the waves were in the range of our simulation, and it was estimated that 0.2 cubic kilometres of land actually collapsed.
Since the landslide occurred, there have been continuous Surtseyan eruptions. These involve explosive interactions between the magma of the volcano and the surrounding water, which is reshaping Anak Krakatoa as it continues to slowly slide to the southwest.
Indonesia remains on high alert as officials warn of potentially more tsunamis. As people wait, it’s worth returning to studies that have looked at the potential hazards caused by volcanoes.
Thomas Giachetti is assistant professor in volcanology in the Department of Earth Sciences at the University of Oregon. A version of this commentary first appeared on The Conversation. Read it here.