EGU23-10799, updated on 13 Mar 2023
https://doi.org/10.5194/egusphere-egu23-10799
EGU General Assembly 2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.

Regional decrease in hazards from ice-dammed lakes in Alaska since the 1960s

Brianna Rick1, Daniel McGrath2, Scott McCoy3, and William Armstrong4
Brianna Rick et al.
  • 1Alaska Climate Adaptation Science Center, United States (bri.rick07@gmail.com)
  • 2Colorado State University, Department of Geosciences, Fort Collins, CO, United States
  • 3University of Nevada Reno, Department of Geological Sciences and Engineering, Reno, NV, United States
  • 4Appalachian State University, Geological and Environmental Sciences, Boone, NC, United States

As ice thins and retreats due to climate change, glacial lakes can form and grow. Rapid lake drainage can produce devastating outburst floods leading many to propose that hazards from glacial lakes are increasing. Outburst flood compilations do show an increase in the number of events documented over time, however, recent studies attribute such trends to observational bias. This leaves large uncertainty about current and future glacial-lake hazards. Here, we focus on ice-dammed lake drainages in Alaska, as a third of documented events globally occurred in this region. Using multitemporal satellite imagery (Landsat and Sentinel-2), we documented 1150 drainages from 106 lakes over 1985–2020. Accounting for the increase in satellite imagery availability over time, we find no temporal trend in drainage frequency. Furthermore, 70% of lakes decreased in estimated volume and peak discharge since the 1960s, and nearly a third of lakes released earlier through time. These results suggest a decrease in overall regional flood hazard from ice-dammed lakes and motivates an unbiased look at other regions.

How to cite: Rick, B., McGrath, D., McCoy, S., and Armstrong, W.: Regional decrease in hazards from ice-dammed lakes in Alaska since the 1960s, EGU General Assembly 2023, Vienna, Austria, 24–28 Apr 2023, EGU23-10799, https://doi.org/10.5194/egusphere-egu23-10799, 2023.