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Phenological shifts in lake stratification under climate change
R Iestyn Woolway1,2, Sapna Sharma3, Gesa A Weyhenmeyer4
1Centre for Freshwater and Environmental Studies, Dundalk Institute of Technology, Dundalk, Ireland. riwoolway@gmail.com.
Lake stratification phenology is changing due to climate change. This prolonged stratification will accelerate lake deoxygenation and impact aquatic ecosystems.
Area of Science:
- Environmental Science
- Climate Science
- Ecology
Background:
- Lake stratification, a key physical process, significantly influences aquatic ecosystems by controlling resource availability.
- Variations in stratification phenology (timing of onset and break-up) have profound ecological consequences.
- Global changes in lake stratification phenology remain largely unknown.
Purpose of the Study:
- To investigate historical and projected changes in lake stratification phenology across the Northern Hemisphere.
- To understand the impact of climate change on lake stratification timing from 1901 to 2099.
Main Methods:
- Utilized a lake-climate model ensemble for projections.
- Incorporated long-term observational data for historical analysis.
- Focused on the Northern Hemisphere to assess regional changes.
Main Results:
- Under a high-greenhouse-gas-emission scenario, stratification is projected to begin 22 days earlier and end 11 days later by 2100.
- This results in a significant prolongation of stratification duration (33 days).
- Accelerated lake deoxygenation and increased phosphorus release from sediments are likely consequences.
Conclusions:
- Projected changes in lake stratification phenology will significantly impact lake ecosystems.
- Prolonged stratification is expected to exacerbate deoxygenation, affecting nutrient cycling.
- Potential for irreversible changes in lake ecosystems due to altered lifecycle events and environmental conditions.
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