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Biogeosciences An interactive open-access journal of the European Geosciences Union
Biogeosciences, 14, 861-883, 2017
https://doi.org/10.5194/bg-14-861-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
Research article
24 Feb 2017
Attaining whole-ecosystem warming using air and deep-soil heating methods with an elevated CO2 atmosphere
Paul J. Hanson1, Jeffery S. Riggs2, W. Robert Nettles1, Jana R. Phillips1, Misha B. Krassovski1, Leslie A. Hook1, Lianhong Gu1, Andrew D. Richardson3, Donald M. Aubrecht3, Daniel M. Ricciuto1, Jeffrey M. Warren1, and Charlotte Barbier4 1Climate Change Science Institute, Oak Ridge National Laboratory, Oak Ridge, Tennessee, USA
2Integrated Operations Support Division, Oak Ridge National Laboratory, Oak Ridge, Tennessee, USA
3Department of Organismic and Evolutionary Biology, Harvard University, Cambridge, Massachusetts, USA
4Instrument and Source Division, Oak Ridge National Laboratory, Oak Ridge, Tennessee, USA
Abstract. This paper describes the operational methods to achieve and measure both deep-soil heating (0–3 m) and whole-ecosystem warming (WEW) appropriate to the scale of tall-stature, high-carbon, boreal forest peatlands. The methods were developed to allow scientists to provide a plausible set of ecosystem-warming scenarios within which immediate and longer-term (1 decade) responses of organisms (microbes to trees) and ecosystem functions (carbon, water and nutrient cycles) could be measured. Elevated CO2 was also incorporated to test how temperature responses may be modified by atmospheric CO2 effects on carbon cycle processes. The WEW approach was successful in sustaining a wide range of aboveground and belowground temperature treatments (+0, +2.25, +4.5, +6.75 and +9 °C) in large 115 m2 open-topped enclosures with elevated CO2 treatments (+0 to +500 ppm). Air warming across the entire 10 enclosure study required  ∼  90 % of the total energy for WEW ranging from 64 283 mega Joules (MJ) d−1 during the warm season to 80 102 MJ d−1 during cold months. Soil warming across the study required only 1.3 to 1.9 % of the energy used ranging from 954 to 1782 MJ d−1 of energy in the warm and cold seasons, respectively. The residual energy was consumed by measurement and communication systems. Sustained temperature and elevated CO2 treatments were only constrained by occasional high external winds. This paper contrasts the in situ WEW method with closely related field-warming approaches using both aboveground (air or infrared heating) and belowground-warming methods. It also includes a full discussion of confounding factors that need to be considered carefully in the interpretation of experimental results. The WEW method combining aboveground and deep-soil heating approaches enables observations of future temperature conditions not available in the current observational record, and therefore provides a plausible glimpse of future environmental conditions.

Citation: Hanson, P. J., Riggs, J. S., Nettles, W. R., Phillips, J. R., Krassovski, M. B., Hook, L. A., Gu, L., Richardson, A. D., Aubrecht, D. M., Ricciuto, D. M., Warren, J. M., and Barbier, C.: Attaining whole-ecosystem warming using air and deep-soil heating methods with an elevated CO2 atmosphere, Biogeosciences, 14, 861-883, https://doi.org/10.5194/bg-14-861-2017, 2017.
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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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