Coastal retreat in Alaska is accelerating because of compound climate impacts
Woods Hole Oceanographic Institution
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Marine flooding degrades permafrost near Point Lonely, Alaska. As compound climate impacts accelerate coastal change, there is an urgent need for adaptive strategies to protect vulnerable communities and infrastructure.
view moreCredit: Photo by: Benjamin M. Jones, Institute of Northern Engineering, University of Alaska Fairbanks
Woods Hole, Mass. (Dec. 3, 2024) -- The overlapping effects of sea level rise, permafrost thaw subsidence, and erosion may lead to land loss in Arctic coastal regions that dwarfs the land loss from any single one of these climate hazards, scientists say.
While 75 years of aerial and satellite observations have established coastal erosion as an increasing Arctic hazard, other hazards—including the cumulative impact of sea level rise and permafrost thaw subsidence, have received less attention. This has prevented assessments of the impacts these processes have compared to and combined with coastal erosion.
A new study in Proceedings of the National Academy of Sciences by scientists with the Woods Hole Oceanographic Institution (WHOI) and other academic institutions focuses on Alaska’s Arctic Coastal Plain (ACP), a 60,000+ square kilometer, low-elevation, and low-relief landscape replete with ice-rich permafrost that has among the highest rates of sea-level rise and coastal erosion in the Arctic.
“Our findings highlight the risks that compounding climate hazards pose to coastal communities and underscore the need for adaptive planning for Arctic communities within zones of 21st-century land loss,” the study notes.
“Compound climate impacts accelerate coastal change,” said study lead author Roger Creel, a postdoctoral scholar in WHOI’s Department of Physical Oceanography. “There is this nonlinear acceleration in coastal impacts that we should be expecting will happen in places like Northern Alaska.”
“The findings from this study reveal an unprecedented transformation of Alaska’s Arctic coastlines. By 2100, the combined effects of coastal erosion, sea level rise, and permafrost thaw subsidence will likely push the North Slope shoreline inland to a location it hasn't reached since the last interglacial period over 100,000 years ago,” said study co-author Benjamin Jones, research associate professor at the Institute of Northern Engineering, the University of Alaska Fairbanks. “These findings represent a paradigm shift in the 21st Century Arctic, highlighting the urgent need for adaptive strategies to protect vulnerable communities and infrastructure in the face of these cumulative climate hazards.”
The study utilized 5-meter topography, satellite-derived coastal lake depth estimates, and empirical assessments of land subsidence due to permafrost thaw, along with projections of coastal erosion and sea level rise for medium and high emission scenarios from the IPCC’s 6th Assessment Report.
“This research highlights the value of working across disciplinary boundaries for more robust projections of coastal Arctic evolution in the coming century,” said co-author Julia Guimond, assistant scientist in WHOI’s Applied Ocean Physics and Engineering Department. “Our work shows that By 2100, total land loss will exceed erosional losses by up to eight times. Here we focus on processes affecting Alaska's Arctic Coastal Plain, but a key takeaway is the compounding effects of multiple hazards and that applies to coastal resilience planning across the globe.”
“Along ice-rich permafrost coastlines, the land surface is falling faster than the sea levels are rising. Over the coming decades, permafrost thaw subsidence will move the coastline farther inland than coastal erosion or sea level rise alone will move it, and this subsidence will dominate Arctic coastal change over the long term,” said co-author Pier Paul Overduin, senior scientist at the Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research in Potsdam, Germany.
Creel said the impact of permafrost thaw subsidence is familiar to people who live in northern Alaska. However, he adds agencies such as the U.S. Army Corps of Engineers and the Federal Emergency Management Agency allocate many of their resources based on published literature. “These sorts of bodies with a lot of resources may have not been paying enough attention to permafrost thaw subsidence as an agent of coastal change. This study is a wake-up call to expand the conversation.”
An Arctic shoreline governed by inundation “will pose new challenges to communities whose homelands – including infrastructure, hunting grounds, subsistence access routes, cultural heritage sites, landscapes, and the soil itself – are disappearing,” the study states. “Future research on Arctic shoreline evolution should be motivated by the needs of these communities, who will need support to respond to the paradigm shift in 21st century Arctic coastal change that we project here.”
Funding for this study was provided by a Woods Hole Oceanographic Institution Postdoctoral Scholarship and the President’s Innovation Fund, U.S. National Science Foundation grants, and the Deutsche Forschungsgemeinschaft under Germany‘s Excellence Strategy, with additional support provided under a Broad Agency Announcement award from the U.S. Army Corps of Engineers’ Engineer Research and Development Center - Cold Regions Research and Engineering Laboratory.
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Authors: Roger Creela, Julia Guimondb, Benjamin Jonesc, David M. Nielsend, Emily Bristole, Craig E. Tweedief, and Pier Paul Overduing
Affiliations:
aDepartment of Physical Oceanography, Woods Hole Oceanographic Institution (WHOI), Falmouth, MA, USA
bDepartment of Applied Ocean Physics and Engineering, WHOI, Falmouth, MA, USA
cInstitute of Northern Engineering, University of Alaska, Fairbanks, Alaska, USA
dMax-Planck -Institut für Meteorologie, Hamburg, Germany
eMarine Science Institute, University of Texas at Austin, Texas, USA
fDepartment of Biological Sciences & the Environmental Science & Engineering Program, University of Texas at El Paso, Texas, USA
gAlfred Wegener Institute Helmholtz-Centre for Polar and Marine Research, Potsdam, Germany
About Woods Hole Oceanographic Institution
The Woods Hole Oceanographic Institution (WHOI) is a private, non-profit organization on Cape Cod, Massachusetts, dedicated to marine research, engineering, and higher education. Established in 1930, its primary mission is to understand the ocean and its interaction with the Earth as a whole, and to communicate an understanding of the ocean’s role in the changing global environment. WHOI’s pioneering discoveries stem from an ideal combination of science and engineering—one that has made it one of the most trusted and technically advanced leaders in basic and applied ocean research and exploration anywhere. WHOI is known for its multidisciplinary approach, superior ship operations, and unparalleled deep-sea robotics capabilities. We play a leading role in ocean observation and operate the most extensive suite of data-gathering platforms in the world. Top scientists, engineers, and students collaborate on more than 800 concurrent projects worldwide—both above and below the waves—pushing the boundaries of knowledge and possibility. For more information, please visit www.whoi.edu
Journal
Proceedings of the National Academy of Sciences
Method of Research
Observational study
Subject of Research
Not applicable
Article Title
Permafrost thaw subsidence, sea-level rise, and erosion are transforming Alaska’s Arctic coastal zone
Article Publication Date
3-Dec-2024
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