Hidden magnitude-8.2 earthquake source of mysterious 2021 global tsunami
Date:
February 8, 2022
Source:
American Geophysical Union
Summary:
Scientists have uncovered the source of a mysterious 2021 tsunami
that sent waves around the globe. In August 2021, a magnitude 7.5
earthquake hit near the South Sandwich Islands, creating a tsunami
that rippled around the globe. The epicenter was 47 kilometers
below the Earth's surface -- too deep to initiate a tsunami --
and the rupture was nearly 400 kilometers long, which should have
generated a much larger earthquake.
FULL STORY ========================================================================== Scientists have uncovered the source of a mysterious 2021 tsunami that
sent waves around the globe.
==========================================================================
In August 2021, a magnitude 7.5 earthquake hit near the South Sandwich
Islands, creating a tsunami that rippled around the globe. The epicenter
was 47 kilometers below the Earth's surface -- too deep to initiate a
tsunami -- and the rupture was nearly 400 kilometers long, which should
have generated a much larger earthquake.
Seismologists were puzzled and sought to understand what really happened
that day in the remote South Atlantic.
A new study revealed the quake wasn't a single event, but five, a series
of sub-quakes spread out over several minutes. The third sub-quake was a shallower, slower magnitude 8.2 quake that hit just 15 kilometers below
the surface. That unusual, "hidden" earthquake was likely the trigger
of the worldwide tsunami.
The study was published in the AGU journal Geophysical Research Letters,
which publishes short-format, high-impact papers with implications that
span the Earth and space sciences.
Because the South Sandwich Islands earthquake was complex, with multiple
sub- quakes, its seismic signal was difficult to interpret, according to
lead study author Zhe Jia, a seismologist at the California Institute
of Technology. The magnitude 8.2 quake was hidden within the tangle
of seismic waves, which interfered with each other over the course of
the event. The hidden quake's signal wasn't clear until Jia filtered
the waves using a much longer period, up to 500 seconds. Only then did
the 200-second-long quake, which Jia said accounted for over 70% of the
energy released during the earthquake, become clear.
==========================================================================
"The third event is special because it was huge, and it was silent,"
Jia said.
"In the data we normally look at [for earthquake monitoring], it was
almost invisible." Predicting hazards for complex earthquakes can be difficult, as the South Sandwich Islands quake demonstrates. The USGS
initially reported the magnitude 7.5 quake and only added the 8.2 event
the following day, as the surprise tsunami lapped on shores up to 10,000 kilometers away from its point of origin.
"We need to rethink our way to mitigate earthquake-tsunami hazards. To
do that, we need to rapidly and accurately characterize the true size
of big earthquakes, as well as their physical processes," Jia said.
Because this type of earthquake can result in unexpected tsunami, it's
critical to improve our predictions. "With these complex earthquakes,
the earthquake happens and we think, 'Oh, that wasn't so big, we don't
have to worry.' And then the tsunami hits and causes a lot of damage,"
said Judith Hubbard, a geologist at the Earth Observatory of Singapore who
was not involved in the study. "This study is a great example of how we
can understand how these events work, and how we can detect them faster
so we can have more warning in the future." Sneaky seismic signals When
an earthquake hits, it sends waves of vibration through the Earth. The
global network of earthquake monitors uses those seismic waves to
pinpoint the time, location, depth and magnitude of an earthquake. Common monitoring often focuses on short- and medium-periods of waves, Jia said,
and longer periods can be left out. But even incorporating long periods
into monitoring, on its own, isn't enough to catch complex earthquakes
with messy seismic signals.
========================================================================== "It's hard to find the second earthquake because it's buried in the
first one," Jia said. "It's very seldom complex earthquakes like this are observed. ... And if we don't use the right dataset, we cannot really see
what was hidden inside." A simple earthquake can easily be pinpointed
and described, Jia said. But a messy one needs to be carefully broken
down into its constituent parts, to find out what unique combination of
simpler earthquakes built up the complex one.
Jia and his colleagues developed an algorithm to tease apart the
seismic signals during those messy earthquakes. By "decomposing" complex earthquake signals into simpler forms, using waves over different periods (varying from 20 to 500 seconds long), the algorithm can identify the
location and properties of different sub-earthquakes. It's akin to
someone with perfect pitch hearing five dissonant notes struck at once,
yet being able to identify each individual note.
"I think a lot of people are daunted by trying to work on events like
this," said Hubbard. "That somebody was willing to really dig into the
data to figure it out is really useful." Both Jia and Hubbard noted a long-term goal is to automate the detection of such complex earthquakes,
as we can for simple earthquakes. For the 2021 quake, the tsunami was
small by the time it reached shores, and most of the permanent residents
of the remote, volcanic islands are penguins. But complex earthquakes
can pose significant hazards if they generate larger tsunami or strike
in a densely populated region.
========================================================================== Story Source: Materials provided by American_Geophysical_Union. Note:
Content may be edited for style and length.
========================================================================== Related Multimedia:
* South_Sandwich_Trench_illustration_and_image_of_South_Georgia_Island ========================================================================== Journal Reference:
1. Zhe Jia, Zhongwen Zhan, Hiroo Kanamori. The 2021 South Sandwich
Island M
w 8.2 Earthquake: A Slow Event Sandwiched Between Regular Ruptures.
Geophysical Research Letters, 2022; 49 (3) DOI: 10.1029/2021GL097104 ==========================================================================
Link to news story:
https://www.sciencedaily.com/releases/2022/02/220208124428.htm
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