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A Strong Mitigation Scenario Maintains Climate Neutrality of Northern Peatlands
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Northern peatlands store 300–600 Pg C, of which approximately half are underlain by permafrost. Climate warming and, in some regions, soil drying from enhanced evaporation are progressively...
A Techno-Economic Evaluation of Bracke and M-Planter Tree Planting Devices
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Techno-economically reasonable mechanization of tree planting has proved to be a difficult task in the Nordic working conditions. Although planting machines and combinations of base machine and...
Decreased Carbon Accumulation Feedback Driven by Climate‐Induced Drying of Two Southern Boreal Bogs over Recent Centuries
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This resource is available on an external database and may require a paid subscription to access it. It is included on the CCLM to support our goal of capturing and sharing the breadth of all...
Large Stocks of Peatland Carbon and Nitrogen are Vulnerable to Permafrost Thaw
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Northern peatlands have accumulated large stocks of organic carbon (C) and nitrogen (N), but their spatial distribution and vulnerability to climate warming remain uncertain. Here, we used machine...
Mechanized Tree Planting in Sweden and Finland: Current State and Key Factors for Future Growth
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In Fennoscandia, mechanized tree planting is time-efficient and produces high-quality regeneration. However, because of low cost-efficiency, the mechanization of Fennoscandian tree planting has been...
Peatland Restoration Increases Water Storage and Attenuates Downstream Stormflow but Does Not Guarantee an Immediate Reversal of Long-term Ecohydrological Degradation
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Peatland restoration is experiencing a global upsurge as a tool to protect and provide various ecosystem services. As the range of peatland types being restored diversifies, do previous findings...
Potential for Using Remote Sensing to Estimate Carbon Fluxes Across Northern Peatlands – A Review
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Peatlands store large amounts of terrestrial carbon and any changes to their carbon balance could cause large changes in the greenhouse gas (GHG) balance of the Earth's atmosphere. There is still much...
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...
Soil and Water Nutrients in Stem‐only and Whole‐tree Harvest Treatments in Restored Boreal Peatlands
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This resource is available on an external database and may require a paid subscription to access it. It is included on the CCLM to support our goal of capturing and sharing the breadth of all...
Soil Deformation and its Recovery in Logging Trails of Drained Boreal Peatlands
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This resource is available on an external database and may require a paid subscription to access it. It is included on the CCLM to support our goal of capturing and sharing the breadth of all...
The Biophysical Climate Mitigation Potential of Boreal Peatlands During the Growing Season
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Peatlands and forests cover large areas of the boreal biome and are critical for global climate regulation. They also regulate regional climate through heat and water vapour exchange with the...
Warming Impacts on Boreal Fen CO2 Exchange Under Wet and Dry Conditions
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This resource is available on an external database and may require a paid subscription to access it. It is included on the CCLM to support our goal of capturing and sharing the breadth of all...
Warming Response of Peatland CO2 Sink is Sensitive to Seasonality in Warming Trends
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This resource is available on an external database and may require a paid subscription to access it. It is included on the CCLM to support our goal of capturing and sharing the breadth of all...
Water Level Drawdown Makes Boreal Peatland Vegetation More Responsive to Weather Conditions
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Abstract Climate warming and projected increase in summer droughts puts northern peatlands under pressure by subjecting them to a combination of gradual drying and extreme weather events. The combined...