View of the north end of Resurrection Bay at Seward, Alaska, about 75 km from the epicenter. An overturned ship, a demolished Texaco chemical truck, and a torn-up dock strewn with logs and scrap metal are visible. At Seward, a community of about 2,300, a section of the waterfront slid into Resurrection Bay. Waves spread in all directions, destroying the Alaska railroad docks, washing out railroad and highway bridges, and piling railroad rolling stock into giant windrows of wreckage. The waves left a shambles of houses and boats in the lagoon area, some still looking relatively undamaged and some almost completely battered. The waves spread flaming petroleum over the waterfront, igniting the rolling stock, the electrical generation plant, and some residences. Resurrection Bay received $14.6 million in damage. Eleven fatalities occurred in the Seward area. (Source: NOAA/NCEI, US DOI)

Do You Live in an Area of High Tsunami Risk?

Just as the Midwest United States is known as ‘Tornado Alley’ and earthquakes occur along fault lines more regularly than other locations, there are coastal areas at increased tsunami risk. As discussed previously, tsunamis are mostly caused by intense and sudden seafloor motion. While the first ideas to come to mind may be earthquakes and volcanoes (among others), the coastal areas most near these events are not necessarily the area(s) at highest risk.

Tsunami evacuation signs from around the world, posted in areas of high tsunami risk (L to R: Thailand, California USA, Colombia, Japan; see end for credits)

Tsunami evacuation signs from around the world, posted in areas of high tsunami risk (L to R: Thailand, California USA, Colombia, Japan; see end for credits)

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How Tsunami Early Warning Systems Work, and Why Indonesia’s System Failed.

Tsunamis are a scary and devastating natural phenomenon. On average, two damaging tsunamis occur globally each year. A major, devastating, ocean-wide tsunami occurs roughly every 15 years. To prevent catastrophic loss of life, many countries have independently or jointly developed tsunami early warning systems. Indonesia was hit with a massive earthquake and subsequent tsunami last month, and their warning system failed. To understand how these systems work and how they can fail, it is important to understand the causes of tsunamis. At the most basic, a tsunami is caused by a large, sudden motion on the seafloor. Earthquakes beneath or near the ocean most commonly cause this motion, but other potential causes include volcanic eruptions, underwater landslides, or even an above water landslide, such as a large piece of ice breaking off an iceberg or a meteor striking the ocean.

How Tsunami Early Warning Systems Work

Since a vast majority of tsunamis are caused by seismic activity on the seafloor, warning systems start with seismic monitoring. Sensors on the seafloor monitor for seismic activity caused by earthquakes and volcanoes. If a substantial seismic incident occurs, surface buoy sensors then monitor for changes in the sea level. Tsunami waves could be as shallow as three feet high, so these sensors are placed in an array to determine motion as well as height. These seafloor and surface buoy sensors send data to tsunami warning centers, which are staffed 24/7. The centers monitor the data, perform analysis, and quickly determine whether conditions are met to issue a tsunami warning alert. If an alert is sent, it goes to local radio and television, wireless emergency alerts, NOAA Weather Radio, and NOAA websites. Some tsunami threat areas might also issue warnings through sirens, text message alerts, and phone notifications.


NOAA’s Deep-ocean Assessment and Reporting of Tsunami System (NOAA)


What Failed in Indonesia?

On September 28, 2018, a 7.5 magnitude earthquake hit Sulawesi, Indonesia. A tsunami alert was briefly issued cautioning a possible tsunami of 0.5 meters, before a tsunami struck the city of Palu. The tsunami that hit was later estimated to be closer to 5 or 6 meters, causing widespread destruction and leading to over 7,000 people confirmed dead or never found. Another 10,000 people were reported injured.

“Indonesia built a network of buoys for detecting tsunamis, but due to lack of maintenance, the system is no longer operational”

Following the tsunami, officials in Indonesia faced heavy criticism for failing to warn the people of the severity of the incident, and several investigations were conducted into what failed within the system. As is common with system failures of this magnitude, several factors combined to bring about the failure.

Detection: Indonesia built a network of buoys for detecting tsunamis, but due to lack of maintenance, the system is no longer operational. Their closest tidal gauge was 125 miles away from Palu, and only recorded a 2.3 inch rise in water level. These tidal gauges are not primarily intended to detect tsunamis, since their sample rate is only every 15 minutes. Seismometers alone proved inadequate to predict the severity of the tsunami.

Warning: Cell phone towers in the area had already been damaged and were inoperable due to the earthquake that preempted the tsunami and many areas did not receive cell phone alerts. Palu was seen as a fairly protected city due to its deep bay and surrounding mountains. Due to this perceived natural protection, the beach regions were not equipped with warning sirens. The geography of this bay likely contributed to the severity of the tsunami instead of protecting the bay by funneling the water to a concentrated point, similar to how a narrowing river speeds up the flow.

Due to the limitations of the detection and warning systems in Indonesia, officials are stressing educating the public that any earthquake lasting longer than 20 seconds is a tsunami threat. If an earthquake occurs, they recommend getting to higher ground immediately and not waiting for a warning.