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New analysis finds real, though rare, tsunami threat to upper Cook Inlet

Scientists assessing tsunami threats throughout ���Ϻ�����Ƶ recently modeled the flooding scenario of the 1964 Great ���Ϻ�����Ƶ Earthquake and discovered that a tsunami could reach upper Cook Inlet, countering a long-held public belief that the region has no tsunami risk.

A new report by the University of ���Ϻ�����Ƶ Fairbanks and ���Ϻ�����Ƶ Division of Geological & Geophysical Surveys reveals an updated understanding of how tsunamis interact with tides and of the region’s potential tsunami hazard.

The report indicates that flooding could follow about four hours after an earthquake similar to that of 1964 that ruptured in the Gulf of ���Ϻ�����Ƶ off the Kenai Peninsula. Affected areas could include low-lying parts of Anchorage, as well as Knik Arm up to the mouths of the Matanuska and Knik rivers and past the Glenn Highway crossings. Turnagain Arm, Hope and Girdwood could also experience flooding. 

Associated coastal currents could be several knots faster than normal tidal currents and could persist for up to 72 hours.

For decades, public perception has been that upper Cook Inlet, including ���Ϻ�����Ƶ’s biggest city, Anchorage, has virtually no tsunami risk. This belief has persisted because many, including scientists, thought wave energy dissipates as it travels Cook Inlet’s length along the shallow, gently sloping floor.

“When I looked at all the arguments about why Anchorage is immune to tsunamis, I couldn’t find a single good argument,” said Elena Suleimani, a tsunami modeler with ���Ϻ�����Ƶ’s ���Ϻ�����Ƶ Earthquake Center and member of a three-person team that has been investigating tsunami threat throughout ���Ϻ�����Ƶ.

Suleimani worked with Dmitry Nicolsky, research associate professor with the ���Ϻ�����Ƶ Geophysical Institute, and Barrett Salisbury, Earthquake and Tsunami Hazards Program manager at the ���Ϻ�����Ƶ Division of Geological & Geophysical Surveys. Their full report was released today on the division’s .

Although it was generally believed that no tsunami reached Anchorage from 1964’s magnitude 9.2 earthquake, the computer modeling shows a tsunami likely did occur.

“How was this wave not noticed by people?” Nicolsky said. The answer: It arrived hours later at low tide, according to the modeling results.

The impact could have been extensive had the tsunami arrived at high tide. It turns out that assessing potential tsunami impacts in upper Cook Inlet is much more complicated than simply considering its length and depth. 

This new comprehensive tsunami hazard study for upper Cook Inlet was funded by NOAA’s National Tsunami Hazard Mitigation Program. It is part of a wider campaign, begun in 1998, to assess the flooding hazard to all coastal ���Ϻ�����Ƶ communities. The program’s scientists prioritized communities with a history of significant tsunami damage, so it wasn’t until around 2018 that they began examining upper Cook Inlet.

The scientists combined three significant tsunami hazard components to produce the upper Cook Inlet tsunami hazard assessment: 

• Tides and water depth: The ability to forecast tsunami inundation at different coastal locations wasn’t available until the 1990s, when researchers started using numerical modeling to integrate the complex movements of tsunamis with real ocean bathymetry. 
• Previous large earthquakes in ���Ϻ�����Ƶ: Geologic research in the past two decades around Southcentral ���Ϻ�����Ƶ shows that the region has experienced earthquakes as large or larger than the 1964 Great ���Ϻ�����Ƶ Earthquake in the past 1,500 years.
• Location: The 2011 magnitude 9.1 earthquake off Tohoku, Japan, gave new insight into how and where large subduction-zone earthquakes can generate tsunamis. Southern ���Ϻ�����Ƶ sits on a similar subduction zone.

A tsunami arriving during high tide could cause significant flooding and damage. At high tide, upper Cook Inlet’s water level is, on average, 40 vertical feet higher than it is at low tide. The extent of flooding depends on how — and for how long — a tsunami navigates such a dynamic tidal regime.

The 1964 quake struck at 5:36 p.m. on March 27, at high tide in Anchorage, but according to the model it would take a tsunami wave more than eight hours to traverse the inlet and reach Anchorage. At its 2 a.m. landfall, the tsunami would have encountered empty shores at low tide. Despite being 10 feet high, according to the model, the wave was lower than high-tide level in upper Cook Inlet, so it caused no flooding.

“A rare combination of earthquake magnitude, location and timing must be satisfied for tsunami wave energy to reach upper Cook Inlet at the same time as a natural high tide,” Salisbury said.

While the risk of this exact confluence of events is rare, upper Cook Inlet residents should still be aware and prepared.

ADDITIONAL INFORMATION: 

• , including GIS data and map sheets and a simulation video of hypothetical earthquake–tsunami dynamics.

ADDITIONAL CONTACT: Barrett Salisbury, Earthquake and Tsunami Hazards Program manager, ���Ϻ�����Ƶ Division of Geological & Geophysical Surveys, 907-451-5974, barrett.salisbury@alaska.gov

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