Forest Sensitivity to Elevated Atmospheric CO 2 and its Relevance to Carbon Management Richard J. Norby Oak Ridge National Laboratory Aspen Global Change.

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Presentation transcript:

Forest Sensitivity to Elevated Atmospheric CO 2 and its Relevance to Carbon Management Richard J. Norby Oak Ridge National Laboratory Aspen Global Change Institute October 19, 2001

Trees that are planted today will be growing in a higher CO 2 concentration tomorrow

Forests play an important role in the global C cycle Increased rate of CO 2 uptake as atmospheric [CO 2 ] rises could slow the rate of [CO 2 ] increase

Forestry Issues with Rising Atmospheric CO 2 Global Carbon Cycle flux storage Net primary productivity Vegetation Response “CO 2 fertilization ” Forest composition and biomass Deforestation, reforestation Climatic Change “greenhouse effect ”

We cannot make reliable predictions concerning the global effects of increasing CO 2 concentration until we have information based on long-term measurements of plant growth from experiments in which high CO 2 concentration is combined with water and nitrogen stress on a wide range of species. - Paul Kramer, 1981

The initial effect of elevated CO 2 will be to increase NPP in most plant communities... A critical question is the extent to which the increase in NPP will lead to a substantial increase in plant biomass. Alternatively, increased NPP could simply increase the rate of turnover of leaves or roots without changing plant biomass. - Boyd Strain & Fakhri Bazzaz, 1983

Will increased [CO 2 ] boost profits on tree farms? What trees should be planted to take advantage of rising [CO 2 ]? Will trees prevent global warming? Can high CO 2 be used to sequester more C in trees? Alternative Research Questions

Mature Forests Not Necessarily CO 2 Sinks Madison, Wisconsin – Some scientists and policy-makers claim forests can absorb enough carbon dioxide to cut the risk of further global warming. But at least some forests may not be up to the job. --ScienceNow, 10 August 2001 Role of Trees in Curbing Greenhouse Gases Is Challenged Two new studies challenge the idea that planting forests could be an effective way to absorb emissions of carbon dioxide, heat-trapping gas that many scientists believe is causing global warming. --New York Times, 24 May 2001 Trees Aren’t a ‘Magic Answer’ on Warming Studies suggest forests won’t soak up excess CO 2. --New York Times, 2 June 1992

We know how trees respond to elevated CO 2 Elevated CO 2 stimulates photosynthesis and photosynthetic enhancement is sustained in the field Trees in elevated CO 2 are bigger at the end of the experiment N concentrations are reduced No large changes in structure Stomatal responses are inconsistent

Response of tree productivity is likely to be less for mature trees in a closed forest How can data from relatively short-term experiments be used to address the long- term responses of a forest?

Hypotheses for new experiments Maximum stand leaf area will increase with increasing CO 2 Growth per unit leaf area will increase after canopy closure Fine root standing crop will not change but turnover will increase Downregulation of growth will occur through N cycle Stand water use will be decoupled from effects on stomata

Oak Ridge Experiment on CO 2 Enrichment of Sweetgum To understand how the eastern deciduous forest will be affected by CO 2 enrichment of the atmosphere, and what are the feedbacks from the forest to the atmosphere. This goal will be approached by measuring the integrated response of an intact forest ecosystem, with a focus on stand-level mechanisms. Goal

Each plot is 25 m diameter (20 m diameter inside buffer) Full year of pre-treatment measurement in 1997 CO 2 exposure (560 ppm) started spring, 1998 Exposure is 24 hours per day, April through October Brookhaven exposure system CO 2 Enrichment of a Deciduous Forest: The Oak Ridge Sweetgum Experiment Liquidambar styraciflua plantation started in elevated, 3 control plots (2 with blowers)

Calculation of NPP Oak Ridge Experiment on CO 2 Enrichment of Sweetgum Stem Allometry : DM = f(BA, H, taper, density) Fine root Minirhizotrons and in-growth cores Coarse root Allometry: DM = f(BA) Understory Harvest Leaf Litter traps

Net Primary Productivity CO 2 effect on NPP was: 27% in 1998, 17% in 1999, 19% in GPP was 27% higher in elevated CO 2. Allocation of the extra C changed from stem to fine root. Oak Ridge Experiment on CO 2 Enrichment of Sweetgum

Aboveground Woody Increment No difference in growth prior to treatment (1997). CO 2 significantly increased growth in 1st year of treatment (35%), but not in 2nd (15%) or 3 rd (7%). The CO 2 effect on stem growth also has disappeared in the Duke prototype FACE ring. Oak Ridge Experiment on CO 2 Enrichment of Sweetgum

Fine Root Productivity Delay in fine root response may be related to accumulation of CHO in coarse roots. Fine roots C turns over faster than wood C through soil processes. Analyze soil heterotrophic respiration: - integrate CO 2 efflux - subtract root respiration - add litter decomposition Oak Ridge Experiment on CO 2 Enrichment of Sweetgum

Net Ecosystem Productivity NEP was positive each year. CO 2 effect on heterotrophic respiration was less than effect on NPP. Oak Ridge Experiment on CO 2 Enrichment of Sweetgum

NPPe NPPa NEPe NEPa NEP gain wood gain NPP gain Short-term C sequestration (NEP) was enhanced by CO 2 enrichment With an increasing fraction of the additional C storage allocated to short-term pools rather than to wood, the gains are likely to be short-lived Dynamics of Carbon Storage

Additional carbon entering the soil through root systems has the potential to add to long-lived soil organic matter pools, but most analyses suggest this is unlikely.

Regardless of the fate of the extra C taken up in the Oak Ridge and Duke FACE experiments, both of these rapidly- growing tree plantations are sequestering substantial amounts of C under current conditions.

Common assumption is that this will confer increased drought resistance, but evidence generally is lacking CO 2 effects on leaf-level transpiration are mitigated as the scale increases to a whole canopy, stand, and region Interactions between CO 2 and Water Elevated CO 2 often reduces stomatal conductance and leaf- level transpiration and increases water-use efficiency

Temperature affects all biological processes Effects are non-linear, time-dependent, and highly dependent on initial conditions Warming can stimulate productivity through increased photosynthesis and longer growing season Warming can decrease productivity through increased stress Elevated CO 2 is likely to ameliorate negative effects of warming Interactions between CO 2 and Warming

Prediction of NPP with Three Biogeochemical Models Predictions are for (425 ppmv CO 2 ) All three models predict increased NPP with climate change and increased CO 2 for both climate simulations Increases are smaller (or become decreases) when CO 2 is not included Increases are less with the Canadian climate simulation

CO 2 x Temperature Interactions Elevated CO 2 increased growth of maples trees by 73%

CO 2 x Temperature Interactions Elevated temperature reduced growth by 35% because of increased stress

CO 2 x Temperature Interactions Positive effects of CO 2 and negative effects of temperature were additive

Plant most responsive species? A factor in evaluation of sequestration projects? Should the certainty of rising atmospheric CO 2 influence forest management decisions?

Wide range in response to high CO 2 ? Is variation due to species or experiment? Dry matter increase is confounded by increasing leaf area and exponential growth These results do not predict the response of a forest

Species may be fundamentally similar Expressing annual growth per unit leaf area adjusts for exponential growth pattern Response is uniform across species and conditions: 29% increase at ~650 ppm CO 2 Growth per unit leaf area separates the functional response from the structural response

NPPe NPPa NEPe NEPa NEP gain wood gain NPP gain CO 2 effect on NEP must be discounted somewhat because of lack of permanence and because increase in [CO 2 ] will be gradual Any remaining effect is small compared to the substantial measurement errors CO 2 Effect on Sequestration is Relatively Small CO 2 fertilization need not be considered part of the evaluation of a C sequestration project

Heavily instrumented tree plantations Full C budgets New instrumentation Increasing focus on belowground C accounting FACE experiments are a useful testbed for sequestration projects

Acknowledgements Research funded by U.S. Department of Energy Artwork provided by Vincent van Gogh (