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Published on: January 7, 2019
Rain events decrease boreal peatland net CO2 uptake through reduced light availability.
Jelmer J Nijp1, Juul Limpens, Klaas Metselaar
1Nature Conservation and Plant Ecology Group, Wageningen University, Wageningen, The Netherlands; Soil Physics and Land Management Group, Wageningen University, Wageningen, The Netherlands.
Daytime rain events reduce carbon dioxide uptake in boreal peatlands. Reduced light availability during rain significantly impacts carbon sequestration, affecting 24% of annual uptake.
Area of Science:
- Ecology
- Environmental Science
- Climate Science
Background:
- Boreal peatlands are significant global carbon sinks.
- Carbon dioxide (CO2) exchange is sensitive to water availability and drought.
- Sphagnum moss, crucial for peat formation, relies on wet conditions.
Purpose of the Study:
- Investigate how daytime rain events affect net ecosystem exchange of CO2 (NEE) in peatlands.
- Determine if environmental changes during rain modify the NEE response.
- Assess the impact of rainfall timing and characteristics on peatland carbon uptake.
Main Methods:
- Analyzed an 11-year dataset of eddy covariance and meteorological measurements.
- Utilized half-hourly data from Degerö Stormyr, a boreal peatland in northern Sweden.
- Examined the relationship between rain events, environmental factors, and CO2 exchange.
Main Results:
- Daytime rain events consistently reduced peatland CO2 sink strength.
- Reduced light availability was the primary driver of decreased CO2 uptake.
- An average rain event decreased net CO2 uptake by 0.23-0.54 gC m(-2).
Conclusions:
- Reduced light during rain events is more impactful than water availability on NEE.
- Peatland CO2 uptake is highly sensitive to altered rainfall patterns and cloud cover.
- This highlights a critical, overlooked factor in peatland carbon cycle dynamics.
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