Glacier Detachments: A New Hazard in a Warming World?
Boulder, Colo., USA: On the evening of 5 August 2013, a startling event
occurred deep in the remote interior of the United States’ largest national
park. A half-kilometer-long tongue of Alaska’s Flat Creek glacier suddenly
broke off, unleashing a torrent of ice and rock that rushed 11 kilometers
down a rugged mountain valley into the wilderness encompassed by
Wrangell–St. Elias National Park and Preserve
.
After National Park Service geologist Michael Loso documented a similar
event in the same location in 2015, he recruited Mylène Jacquemart, a Ph.D.
student at the University of Colorado Boulder, to investigate. “We were
aware of glacier detachments that had happened in Tibet, Russia, and
Argentina, but started out thinking we were investigating a regular
landslide,” says Jacquemart. “Then we noticed that the entire glacier was
missing.”
The results, published in Geology, indicate the Alaskan
detachments occurred at the height of the summer melt seasons and suggest
these highly destructive events could occur more frequently in a warming
world.
After National Park Service geologist Michael Loso conducted preliminary
research that ruled out a seismic trigger for these events, he, Jacquemart,
and other experts began a research project to investigate what had happened
at Flat Creek. The team used a variety of tools, including satellite
imagery, field measurements, digital elevation models, and meltwater
modeling, to piece together the sequence of events. “This project was a
real sleuthing challenge,” says Jacquemart, “and the pieces finally fell
into place when we discovered the bulge on the Flat Creek glacier.”
Although the researchers were aware that an odd ice bulge existed on the
glacier’s tongue prior to the first detachment in 2013, it wasn’t until
they obtained 10-year-old, high-resolution satellite images and estimated
that the bulge was an impressive 70 meters high that they began to
understand its implications. “Our data indicate that the lowermost part of
the glacier tongue was very thin, stagnant, and firmly frozen to the
glacier bed,” Jacquemart says. “We believe this frozen tongue did two
things: it blocked ice flowing down from higher on the glacier, forcing it
to bulge; and it slowed meltwater drainage, allowing the water to pool
under the glacier.” The resulting increase in subglacial water pressure,
she says, eventually caused the glacier tongue to suddenly detach,
resulting in two mass flows so large that they each buried about 3 square
kilometers of 400-year-old forest.
Glaciers are primarily disappearing as a result of their ice melting at a
faster pace, says Jacquemart. “But the new insights we’re gaining from
places like Flat Creek show that we also need to consider new processes we
weren’t previously aware of.” Ultimately, says Jacquemart, scientists will
need to develop a better understanding of these new processes and
potentially reevaluate hazard assessments in mountain communities.
“Flat Creek is fortunately in a very remote place,” says Jacquemart, “but
the detachments that occurred in Russia and Tibet claimed numerous lives.”
Given that the mass flows produced by glacier detachments appear to travel
quite far, she says, emergency planners also need to consider possible
cascading hazards, such as the temporary damming of a river followed by the
water’s release. “Suddenly, a remote event can have far-reaching impacts
downstream,” says Jacquemart.
The similarity of the glacier detachments in Alaska with those that
occurred in Tibet suggest that all of these events shared a common cause.
Other detachments elsewhere in the world have also been recently
discovered, says Jacquemart, suggesting that large-scale glacier
detachments may be exacerbated by global warming. “We conclude that the
meltwater produced by increasingly warmer summers has the potential to
create unexpected consequences in the form of hazards that we didn’t
previously know about”, says Jacquemart, “and that we are only just
beginning to understand.”
FEATURED ARTICLE
What drives large-scale glacier detachments? Insights from Flat Creek
glacier, St. Elias Mountains, Alaska
Mylène Jacquemart et al., Mylene.Jacquemart@colorado.edu
URL:
https://pubs.geoscienceworld.org/gsa/geology/article/doi/10.1130/G47211.1/583706/What-drives-large-scale-glacier-detachments
Video: https://youtu.be/9Zl1RrehmdA
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