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Cooley_et_al_data__Agg_Nov2024_dP.csv

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Figshare2024-11-28 更新2026-04-08 收录
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<b><i>A global 'climate opportunity benefit' of regeneration: meta-analysis shows warming from soil CH</i></b><sub><i><strong>4</strong></i></sub><b><i> and N</i></b><sub><i><strong>2</strong></i></sub><b><i>O is small in forests relative to agriculture</i></b>Savannah S. Cooley<sup>1*</sup>, Elisabeth Moore<sup>1</sup>, Jianna Martinez<sup>1</sup>, Jocelyn Fahlen<sup>1</sup>, Erin Maybach<sup>1</sup>, Maya Gollerkeri<sup>1</sup>, Anjali Rao Vasa<sup>1</sup>, Sian Kou-Giesbrecht<sup>2</sup>, Alexandra M. Huddell<sup>3</sup>, Linnea Norton<sup>1</sup>, Kerry Cawse-Nicholson<sup>4</sup>, Ruth DeFries<sup>1</sup>, Maria Uriarte<sup>1</sup>, Duncan N.L. Menge<sup>1</sup><sup>1</sup> Department of Ecology, Evolution and Environmental Biology, Columbia University<sup>2</sup> Department of Earth and Environmental Sciences, Dalhousie University<sup>3</sup> Department of Department of Plant and Soil Sciences, University of Delaware<sup>4</sup> NASA Jet Propulsion Laboratory, California Institute of Technology<br>* Corresponding author: sc4751@columbia.edu<b>Abstract</b>Global assessments of ecosystem regeneration as a climate mitigation strategy have traditionally focused on CO<sub>2</sub>, despite the acknowledgement that methane (CH<sub>4</sub>) and nitrous oxide (N<sub>2</sub>O) are also important greenhouse gasses (GHGs). We conducted a meta-analysis of studies that measured soil CH<sub>4</sub> and N<sub>2</sub>O fluxes in unmanaged regenerating forested and savanna ecosystems, with a focus on understanding biome-specific differences in these GHG fluxes compared to a counterfactual of agricultural land use. We expected most regenerating ecosystems to act as small CH<sub>4 </sub>sinks and relatively larger N<sub>2</sub>O sources, with a net warming combined CH<sub>4</sub>-N<sub>2</sub>O effect. Three of the five forested biomes we studied followed this pattern: subtropical/tropical forest, subtropical/tropical savanna and temperate conifer forest (0.98 ± 0.44, 0.23 ± 0.07, and 0.63 ± 0.37 Mg CO<sub>2</sub>e ha<sup>-1</sup> yr<sup>-1</sup>, respectively). Results suggest that even after 100 years of regeneration, the radiative cooling of the climate from CO<sub>2</sub> sequestration still exceeds the radiative warming driven by the net CH<sub>4</sub>-N<sub>2</sub>O effect among all ecosystems on average globally. We also found that the “climate opportunity benefit” of ecosystem regeneration—the difference of the net CH<sub>4</sub>-N<sub>2</sub>O effects of agriculture vs. regeneration—yields a net cooling effect for all biomes. However, our results underscore that it is unsound to use ecosystem regeneration as a justification for the continuation of fossil fuel emissions.
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Cooley, Savannah
创建时间:
2024-11-28
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