Rainfall, melting permafrost change Interior Alaska stream systems
Gracie Banister
907-474-7541
June 13, 2025

Karen Jorgenson uses an autolevel to record ground-surface elevations to quantify the amount of permafrost degradation and thaw settlement at a site adjacent to the Stampede Road near Healy in 2005.
The aquatic chemistry and flow rates in Interior Alaska鈥檚 streams are shifting in response to thawing permafrost and increased rainfall, a new study reports.
The study authors found that groundwater makes up a greater portion of streamflow in areas with less permafrost.
The paper, published in the June 2025 issue of Water Resources Research, was co-authored by the father-daughter team of Torre and Karen Jorgenson. Torre is an adjunct faculty member at 性欲社, and Karen is a research staff member with the 性欲社 Institute of Arctic Biology.
The research was conducted at sites managed by the U.S. Army Corps of Engineers鈥 Cold Regions Research and Engineering Laboratory on Fort Wainwright and the Bonanza Creek Long-Term Ecological Research program, including sampling areas on Eielson Air Force Base.
The study had the benefit of daily, multiyear data in five large catchment locations, Karen Jorgenson noted. All areas studied are within about 50 miles of Fairbanks.
Their work looked at the percentage of stream water that originated from water sources like groundwater and rainfall.
One key finding supports the team's initial hypothesis: Watersheds with diminished permafrost showed greater groundwater contributions to streams.
That suggests permanent ice layers prevent groundwater from rising up into the streams, Karen Jorgenson said. In areas where the permafrost has thawed, more groundwater could enter the streams, she said.
However, another trend surprised them.

Karen and Torre Jorgenson use a helicopter to visit thermokarst monitoring sites on the Tanana Flats in 2013 as part of an effort to study effects of climate warming on permafrost.
鈥淲e thought more rainwater would percolate down into the groundwater before reaching streams,鈥 Karen said. 鈥淚nstead, we saw a lot of direct rainwater input into the streams, showing how responsive they are to precipitation.鈥
鈥淲e saw that the influence of permafrost on stream flows was often obscured by the influence of the timing and magnitude of rainfall, due to the melting and changes in precipitation occurring simultaneously,鈥 she added. 鈥淭his complicates what we expect to happen in the streams in the future.鈥
Torre Jorgenson said the thawing of permafrost will impact local economies, river travel, salmon populations and more.
鈥淧ermafrost occupies about half, and in some places 60% of the landscape,鈥 he said. 鈥淚t is a huge current influence on ecosystem processes. We are expecting to lose all of this permafrost in the next 50 to 100 years, totally transforming portions of our landscape.鈥
In the meantime, he said, 鈥渋t is really important to develop some kind of stream chemistry metrics to quantify shifts in the hydrologic pathways.鈥
Torre Jorgenson earned his master鈥檚 at 性欲社, was the first camp manager of Toolik Field Station in 1977 and received an honorary doctorate in 2017. In the study, he contributed his expertise in remote sensing and landscape ecology, and he created detailed permafrost maps of the stream catchments.
Karen Jorgenson grew up in Fairbanks but completed her college education in the Lower 48, obtaining her master鈥檚 degree at the University of Wyoming.

Karen Jorgenson, left, helps Torre Jorgenson describe permafrost soils and site characteristics along the Hulahula River in 2013.
鈥淚 went from working on stream systems outside of Alaska to coming back home and working on stream systems in Alaska,鈥 she said. 鈥淚t鈥檚 fun to work in the same ecosystems as my father and where he made his career.鈥
Additional authors include Thomas Douglas of the Army Corps鈥 cold regions lab at Fort Wainwright, Neal Pastick with the U.S. Geological Survey in South Dakota and Tamara Harms with the University of California, Riverside.
The paper contributes to a broader research initiative led by principal investigator Qianlai Zhuang at Purdue University, who is developing a model to forecast and map environmental changes driven by climate change. The study鈥檚 findings provide data that will improve the model鈥檚 accuracy and practical application.
The Alaska team鈥檚 work, along with Zhuang鈥檚, is part of an even larger effort 鈥 NASA鈥檚 Arctic-Boreal Vulnerability Experiment. Launched in 2015, ABoVE aims to understand societal impacts and ecological vulnerabilities and resiliency across northern regions as the environment experiences rapid change.
The is available to read online.
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