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Updated: Jul 14, 2026

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Continuous Hydrologic and Water Quality Monitoring of Vernal Ponds
Published on: November 13, 2017
Crossing the final ecological threshold in high Arctic ponds
John P Smol1, Marianne S V Douglas
1Paleoecological Environmental Assessment and Research Laboratory, Department of Biology, Queen's University, Kingston, ON, Canada K7L 3N6. smolj@biology.queensu.ca
Summary
High Arctic ponds are disappearing due to climate change. Increased evaporation is causing these vital ecosystems to completely dry up each summer, crossing an ecological threshold.
Area of Science:
- Arctic ecology
- Limnology
- Climate change impacts
Background:
- Arctic regions feature numerous shallow ponds crucial for biodiversity.
- These ponds are vulnerable to climate change due to low water volume and high surface area.
- Paleolimnological data suggest some ponds have been permanent for millennia.
Purpose of the Study:
- To investigate the drying of high Arctic ponds.
- To link pond desiccation to climatic changes.
- To identify the ecological threshold crossed by these aquatic ecosystems.
Main Methods:
- Comparing recent pond water specific conductance to 1980s measurements.
- Analyzing evaporation/precipitation ratios.
- Assessing paleolimnological data for pond permanence.
Main Results:
- Some high Arctic ponds are now completely drying during the polar summer.
- Increased evaporation/precipitation ratios are linked to pond disappearance.
- This phenomenon is likely associated with climatic warming.
Conclusions:
- High Arctic shallow ponds are crossing an ecological threshold leading to complete desiccation.
- Climate warming is a probable driver of increased evaporation and pond drying.
- The long-term persistence of these vital aquatic habitats is threatened.
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