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Climate Signatures on Lake And Wetland Size Distributions in Arctic Deltas
Lawrence Vulis1, Alejandro Tejedor1,2, Ilya Zaliapin3
1Department of Civil and Environmental Engineering University of California Irvine Irvine CA USA.
Summary
Arctic thermokarst lakes are shrinking with warming temperatures, unlike wetlands. Colder regions with deeper permafrost preserve larger lakes, impacting carbon storage projections.
Area of Science:
- Environmental science
- Geosciences
- Climate science
Background:
- Thermokarst lakes are sensitive indicators of Arctic climate change.
- Understanding their response to warming is crucial for carbon cycle projections.
- Distinguishing between perennial lakes and ephemeral wetlands is challenging with remote sensing.
Purpose of the Study:
- To differentiate perennial lakes from ephemeral wetlands across 12 Arctic deltas.
- To analyze the distinct size distributions and climate trends of these water bodies.
- To investigate the relationship between Arctic warming and thermokarst lake dynamics.
Main Methods:
- Rigorous separation of perennial lakes and ephemeral wetlands using satellite observations.
- Analysis of distinct size distribution patterns (lognormal for lakes, power-law for wetlands).
- Statistical assessment of trends in water body size in relation to temperature variations.
Main Results:
- Perennial lakes exhibit a lognormal size distribution, while wetlands follow a power-law distribution.
- No significant temperature trend was observed for ephemeral wetlands.
- A statistically significant decrease in mean perennial lake size was found with increasing temperatures.
Conclusions:
- Warmer temperatures lead to a reduction in the size of Arctic thermokarst lakes.
- Deeper permafrost in colder regions supports larger lakes, influencing landscape carbon storage.
- The distinct responses of lakes and wetlands to warming necessitate tailored monitoring strategies.
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