Peter E. Thornton
September 21, 2016
Low-cost experiment provides first robust test of alternative hypotheses regarding short-term vegetation response to chronic nutrient limitation.
An innovative and low-cost field experiment provided new results regarding the fundamental process of photosynthetic carbon uptake in the face of varying levels of nutrient limitation. Experimental results refute current modeling approach for instantaneous downregulation of carbon uptake and support new hypothesis for long-term storage and release of excess carbon.
This new hypothesis has significant impact on the seasonal cycle of atmospheric carbon dioxide (CO2), an important performance metric for global carbon cycle models. The fate of excess carbon can have significant impact on other ecosystem processes.
Models predicting ecosystem CO2 exchange under future climate change rely on relatively few real-world tests of their assumptions and outputs. This work demonstrated a rapid and cost-effective method to estimate CO2 exchange from intact vegetation patches under varying atmospheric CO2 concentrations. Findings showed that net ecosystem CO2 uptake (NEE) in a boreal forest rose linearly by 4.7% ± 0.2% of the current ambient rate for every 10 ppm CO2 increase, with no detectable influence of foliar biomass, season, or nitrogen fertilization. The lack of any clear short-term NEE response to fertilization in such a nitrogen-limited system is inconsistent with the instantaneous downregulation of photosynthesis formalized in many global models. Incorporating an alternative mechanism with considerable empirical support—diversion of excess carbon to storage compounds—into an existing Earth system model brings the model output into closer agreement with the team's field measurements. A global simulation incorporating this modified model reduced a long-standing mismatch between the modeled and observed seasonal amplitude of atmospheric CO2. Wider application of this chamber approach would provide critical data needed to further improve modeled projections of biosphere-atmosphere CO2 exchange in a changing climate.
BER Program Managers
Dorothy Koch, Daniel Stover, and Jared DeForest
Dorothy.Koch@science.doe.gov (301-903-0105), Daniel.Stover@science.doe.gov (301-903-0289), and Jared.DeForest@science.doe.gov (301-903-1678)
Peter E. Thornton
Environmental Sciences Division and Climate Change Science Institute
Oak Ridge National Laboratory
Oak Ridge, TN 37831
This work was supported by the Earth System Modeling (ACME project) and Terrestrial Ecosystem Science program (ORNL TES SFA) of the Office of Biological and Environmental Research, within the U.S. Department of Energy (DOE) Office of Science.
Metcalfe, D. B., D. Ricciuto, S. Palmroth, C. Campbell, V. Hurry, J. Mao, S. G. Keel, S. Linder, X. Shi, T. Näsholm, K. E. A. Ohlsson, M. Blackburn, P. E. Thornton and R. Oren. "Informing climate models with rapid chamber measurements of forest carbon uptake." Global Change Biology 23(5), 2130–2139 (2016). [DOI:10.1111/gcb.13451].
ORNL TES SFA, ACME, OLCF