PS 67-50 - Synthesis of four forest CO2 enrichment experiments demonstrates a strong decadal carbon sink in aggrading temperate forest biomass

Friday, August 11, 2017
Exhibit Hall, Oregon Convention Center
Anthony P. Walker1, Martin G. De Kauwe2, Belinda Medlyn3, Soenke Zaehle4, Colleen M. Iversen1, Bruce A. Hungate5, J. Patrick Megonigal6, Alan F. Talhelm7, Jeffrey M. Warren1, Donald R. Zak8 and Richard J. Norby1, (1)Environmental Sciences Division and Climate Change Science Institute, Oak Ridge National Laboratory, Oak Ridge, TN, (2)School of Biological Sciences, Macquarie University, Sydney, NSW, Australia, (3)Hawkesbury Institute for the Environment, University of Western Sydney, Australia, (4)Biogeochemical Integration Department, Max-Planck Institute for Biogeochemistry, Jena, Germany, (5)Department of Biological Sciences, Northern Arizona University, Flagstaff, AZ, (6)Smithsonian Environmental Research Center, Edgewater, MD, (7)Forest, Rangeland, and Fire Sciences, University of Idaho, Moscow, ID, (8)School of Natural Resources & Environment, University of Michigan, Ann Arbor, MI

Predictive understanding of the future terrestrial carbon sink remains elusive. Forest responses to increasing CO2 are a large contributor to uncertainty in this understanding. Synthesizing data from the only four, decade long, forest CO2 enrichment experiments replicated at the forest stand scale, we show a strong, decadal-scale CO2 sink in aggrading forest biomass.


Across ambient and elevated CO2 treatments, biomass increased over the decade of the experiments in a linear relationship with NPP, i.e. CO2 did not affect the relationship between biomass increment and cumulative NPP. However, because wood allocation increased as NPP increased, the retention of NPP as biomass was more efficient under increased CO2. Each forest showed strong within treatment variability in NPP suggesting that the factors governing the retention of NPP as biomass across a range of natural climatic and edaphic variability also govern the retention of CO2 stimulated NPP. At the two sites that were not confounded by uncertainty or adaptation to frequent fire disturbance, state-of-the-art ecosystem models under-predicted the biomass stimulation by CO2. This under-prediction was caused by an under-prediction of both the NPP response to CO2 and the increase in the wood allocation fraction in response to CO2. These data, synthesized as part of the Free Air CO2 Enrichment Model Data Synthesis (FACE-MDS) project, clearly demonstrate a sustained long-term stimulation of forest biomass in response to CO2 concentrations predicted for the middle of the century. Properly accounting for this CO2 stimulation of biomass in aggrading forests will be necessary for accurately projecting the future terrestrial carbon sink.