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Increasing Contributions of Peatlands to Boreal Evapotranspiration in a Warming Climate
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The response of evapotranspiration (ET) to warming is of critical importance to the water and carbon cycle of the boreal biome, a mosaic of land cover types dominated by forests and peatlands. The...
Near-surface Controls on Peatland Hydrology: Implications for Rapid Disturbance Adaptation and Enhanced Resilience to Disturbance
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Northern peatlands faced compounding disturbances that transformed such critical ecosystems from long-term carbon sinks into carbon sources. Considerable investment is therefore directed for restoring...
Recent Climate Change has Driven Divergent Hydrological Shifts in High-latitude Peatlands
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High-latitude peatlands are changing rapidly in response to climate change, including permafrost thaw. Here, we reconstruct hydrological conditions since the seventeenth century using testate amoeba...