Articles | Volume 14, issue 4
https://doi.org/10.5194/bg-14-861-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/bg-14-861-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Attaining whole-ecosystem warming using air and deep-soil heating methods with an elevated CO2 atmosphere
Climate Change Science Institute, Oak Ridge National Laboratory, Oak
Ridge, Tennessee, USA
Jeffery S. Riggs
Integrated Operations Support Division, Oak Ridge National Laboratory,
Oak Ridge, Tennessee, USA
W. Robert Nettles
Climate Change Science Institute, Oak Ridge National Laboratory, Oak
Ridge, Tennessee, USA
Jana R. Phillips
Climate Change Science Institute, Oak Ridge National Laboratory, Oak
Ridge, Tennessee, USA
Misha B. Krassovski
Climate Change Science Institute, Oak Ridge National Laboratory, Oak
Ridge, Tennessee, USA
Leslie A. Hook
Climate Change Science Institute, Oak Ridge National Laboratory, Oak
Ridge, Tennessee, USA
Lianhong Gu
Climate Change Science Institute, Oak Ridge National Laboratory, Oak
Ridge, Tennessee, USA
Andrew D. Richardson
Department of Organismic and Evolutionary Biology, Harvard University, Cambridge, Massachusetts, USA
Donald M. Aubrecht
Department of Organismic and Evolutionary Biology, Harvard University, Cambridge, Massachusetts, USA
Daniel M. Ricciuto
Climate Change Science Institute, Oak Ridge National Laboratory, Oak
Ridge, Tennessee, USA
Jeffrey M. Warren
Climate Change Science Institute, Oak Ridge National Laboratory, Oak
Ridge, Tennessee, USA
Charlotte Barbier
Instrument and Source Division, Oak Ridge National Laboratory, Oak
Ridge, Tennessee, USA
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- Large-scale experimental warming reduces soil faunal biodiversity through peatland drying C. Barreto et al. 10.3389/fenvs.2023.1153683
- Temperature and CO2 interactively drive shifts in the compositional and functional structure of peatland protist communities C. Kilner et al. 10.1111/gcb.17203
- Comparing stem growth of strip-bark and whole-bark growth morphologies in a subarctic conifer (Pinus banksiana), Yellowknife, Northwest Territories M. Pisaric et al. 10.1016/j.dendro.2023.126148
- Whole-Ecosystem Warming Increases Plant-Available Nitrogen and Phosphorus in an Ombrotrophic Bog C. Iversen et al. 10.1007/s10021-022-00744-x
- Elevated temperature alters microbial communities, but not decomposition rates, during 3 years of in situ peat decomposition S. Roth et al. 10.1128/msystems.00337-23
- Hydrological feedbacks on peatland CH4 emission under warming and elevated CO2: A modeling study F. Yuan et al. 10.1016/j.jhydrol.2021.127137
- Ecological responses to forest age, habitat, and host vary by mycorrhizal type in boreal peatlands P. Kennedy et al. 10.1007/s00572-018-0821-4
- Hydrological and meteorological data from research catchments at the Marcell Experimental Forest, Minnesota, USA S. Sebestyen et al. 10.1002/hyp.14092
- Photosynthetic and Respiratory Responses of Two Bog Shrub Species to Whole Ecosystem Warming and Elevated CO2 at the Boreal-Temperate Ecotone E. Ward et al. 10.3389/ffgc.2019.00054
- Springtime Drought Shifts Carbon Partitioning of Recent Photosynthates in 10-Year Old Picea mariana Trees, Causing Restricted Canopy Development A. Jensen et al. 10.3389/ffgc.2020.601046
- Design and Assessment of a Novel Approach for Ecosystem Warming Experiments in High‐Energy Tidal Wetlands R. Rich et al. 10.1029/2023JG007550
- Deep peat warming increases surface methane and carbon dioxide emissions in a black spruce‐dominated ombrotrophic bog A. Gill et al. 10.1111/gcb.13806
- Advancing global change biology through experimental manipulations: Where have we been and where might we go? P. Hanson & A. Walker 10.1111/gcb.14894
- Diversity of Active Viral Infections within the Sphagnum Microbiome J. Stough et al. 10.1128/AEM.01124-18
- Warming and elevated CO2 promote rapid incorporation and degradation of plant‐derived organic matter in an ombrotrophic peatland N. Ofiti et al. 10.1111/gcb.15955
- Acclimation of Fine Root Systems to Soil Warming: Comparison of an Experimental Setup and a Natural Soil Temperature Gradient K. Parts et al. 10.1007/s10021-018-0280-y
- Differential responses of carbon‐degrading enzyme activities to warming: Implications for soil respiration J. Chen et al. 10.1111/gcb.14394
- Climate change impacts plant carbon balance, increasing mean future carbon use efficiency but decreasing total forest extent at dry range edges J. Mathias et al. 10.1111/ele.13945
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Discussed (final revised paper)
Latest update: 20 Nov 2024
Short summary
This paper describes operational methods to achieve whole-ecosystem warming (WEW) for tall-stature, high-carbon, boreal forest peatlands. The methods enable scientists to study immediate and longer-term (1 decade) responses of organisms (microbes to trees) and ecosystem functions (carbon, water and nutrient cycles). The WEW technology allows researchers to have a plausible glimpse of future environmental conditions for study that are not available in the current observational record.
This paper describes operational methods to achieve whole-ecosystem warming (WEW) for...
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Final-revised paper
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