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Arctic Hyporheic Zone Hydrology and Biogeochemistry |
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Overview: We
are investigating the responses of arctic tundra stream geomorphology,
hyporheic zone hydrology, and biogeochemical cycling to climate change.
In particular, we expect that hyporehic exchange dynamics in tundra
streams are controlled by 1) channel features (pools, riffles, etc.),
and 2) depth of thaw beneath the stream channel. Altered arctic climate
will likely alter stream flows and therefore the fluvial geomorphic
structure of stream channels. We hypothesize that the potential for
hyporheic exchange increases as the climate warms and active layers
deepen. At the same time, increased exchange of water between the
stream and the hyporheic zone could be driving more or different types
of hyporheic biogeochemical cycling, which may alter stream nutrient
budgets.
![]() Overview of this project within Arctic System Science, larger forcing factors, and other Arctic hydrologic research. |
Specific
Objectives: 2.
Monitor the sub-stream thaw bulb size through the thaw season using
ground penetrating radar and subsurface temperature measurement in
several stream cross-sections within each reach. 3.
Conduct repeated hyporheic exchange studies (stream solute addition
experiments) through the thaw season in each reach to determine
hyporheic hydraulic characteristics. 4. Conduct repeated measures of nutrient (N and P) concentrations and turnover time in the hyporheic zone through the thaw season in each reach to determine biogeochemical characteristics. |
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Location: Our field sites are within the Kuparuk River and Toolik Lake basins, north of the Brooks Range, Alaska. Our operations are based out of the Toolik Lake Research Station, run by the University of Alaska, Fairbanks.
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Theses/Dissertations:
Related Links:
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Climate Change Science Links: |
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Current
Weather at Toolik Lake
(from ARC LTER met station; only active during the summer) |
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This project is
funded through the National Science Foundation's Office of Polar
Programs.
This material is based upon work supported by the National Science Foundation under Grant No. 0327440. Any opinions, findings, and conclusions or recommendations expressed in this material are those of the author(s) and do not necessarily reflect the views of the National Science Foundation |