Many uncertainties remain regarding how climate change will alter the structure and function of forest ecosystems. At the Aspen FACE experiment in northern Wisconsin, we are attempting to understand how an aspen/birch/maple forest ecosystem responds to long-term exposure to elevated carbon dioxide (CO2) and ozone (O3), alone and in combination, from establishment onward. We examine how O3 affects the flow of carbon through the ecosystem from the leaf level through to the roots and into the soil micro-organisms in present and future atmospheric CO2 conditions. We provide evidence of adverse effects of O3, with or without co-occurring elevated CO2, that cascade through the entire ecosystem impacting complex trophic interactions and food webs on all three species in the study: trembling aspen (Populus tremuloides Michx.), paper birch (Betula papyrifera Marsh), and sugar maple (Acer saccharum Marsh). Interestingly, the negative effect of O3 on the growth of sugar maple did not become evident until 3 years into the study. The negative effect of O3 effect was most noticeable on paper birch trees growing under elevated CO2. Our results demonstrate the importance of long-term studies to detect subtle effects of atmospheric change and of the need for studies of interacting stresses whose responses could not be predicted by studies of single factors. In biologically complex forest ecosystems, effects at one scale can be very different from those at another scale. For scaling purposes, then, linking process with canopy level models is essential if O3 impacts are to be accurately predicted. Finally, we describe how outputs from our long-term multispecies Aspen FACE experiment are being used to develop simple, coupled models to estimate productivity gain/loss from changing O3.
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an ecophysiological model to grow individual trees
Free-Air CO2 Exposure
leaf area index
photosynthetically active radiation
parts per billion
parts per billion hours
parts per million
soil organic matter
accumulated hourly exposure over 60 ppb.
Tropospheric ozone (O3), a secondary pollutant generated downwind of major metropolitan areas from nitrogen oxides and volatile organic compounds reacting in the presence of sunlight, was first identified as a problem in the 1950s (Dunn 1959) for plant communities downwind of the Los Angeles area. Among the first forest ecosystems found to be impacted by O3 was the pine-fir forest in the San Bernardino Mountains (Miller et al. 1963; Miller & Millecan 1971). Subsequently, O3 effects on forest trees also were identified in the Sierra Nevada Mountains of southern California (Miller, McCutcheon & Milligan 1972). About the same time, researchers in the eastern United States identified visible symptoms of O3 damage on sensitive genotypes of eastern white pine (Dochinger et al. 1970; Costonis 1970).
The Aspen FACE experiment was established in 1997 in northern Wisconsin to examine the impacts of tropospheric O3, alone and in combination with elevated atmospheric CO2, on the structure and function of a northern forest ecosystem dominated by the rapid-growing, pioneer species trembling aspen (Populus tremuloides Michx.) but including also another rapid-growing, pioneer species paper birch (Betula papyrifera Marsh) and the slower-growing, later-successional species sugar maple (Acer saccharum Marsh). Trembling aspen is the most widely distributed tree species in North America. Aspen forest types make up over 8.8 million ha in the USA and 17.8 million ha in Canada. In Wisconsin, alone, where this experiment is located, aspen, birch and maple stands comprise over 50% of the State's vast forest resource. Aspen and birch comprise some 70% of the pulpwood harvested in the states bordering the Great Lakes (Piva 1996).
The Aspen FACE experiment is unique in that it was established to examine the long-term effects of these two greenhouse gases on development of the ecosystem from seedling establishment onward. The experiment utilizes a state-of-the-art open-air fumigation system (Dickson et al. 2000) that is devoid of artifacts that often occur in chamber systems such as low-winds, higher-than-ambient temperature, altered hydrology, higher humidity, and reduced light levels (Hendrey et al. 1999; McLeod & Long 1999; Karnosky et al. 2001). Furthermore, the plot sizes (30-m-diameter rings) are large enough to examine effects that are difficult to detect in small chambers such as intraspecific and interspecific competition, carbon fluxes to soil and pest epidemiology. Trophic interactions are facilitated by the unencumbered movement of insects into and out of the rings.
In this paper, we present a synthesis of results from the first 7 years of this unique experiment including studies of above-ground physiology and growth, canopy development, stem wood quality, community dynamics, below ground growth, carbon flux and community structure, and pest interactions. Finally, we discuss ways to scale up our experimental data to landscape or regional levels via various modelling strategies and development of appropriate O3 dose–response functions to project impacts of O3. These could eventually be useful in determining O3 standards to protect forest vegetation.
THE ASPEN FACE EXPERIMENT
The Aspen FACE experiment consists of a full factorial with 12 30-m-diameter treatment rings with three control rings, three rings with elevated O3, three rings with elevated CO2, and three rings with elevated O3 + elevated CO2(Fig. 2); 100 m is the minimum distance between any two FACE rings. The rings were planted in late 1997 and treatments ran from budbreak to the end of each growing season from 1998 to 2004. The eastern one-half of each ring was randomly planted in two-tree plots at 1 m × 1 m spacing with five aspen clones differing in O3 tolerance (8L, 216 and 271 = relatively tolerant; 42E and 259 = relatively sensitive). The north-western quadrant of each ring was planted at the same spacing with alternating aspen clone 216 and sugar maple seedlings, and the south-western quadrant of each ring was planted as above with aspen clone 216 and paper birch seedlings.
Carbon dioxide and O3 are delivered via a computer-controlled system modified from Hendrey et al. (1999) during the daylight hours with our target CO2 being 560 ppm, which is about 200 ppm above the daylight ambient CO2 concentration. Ozone was applied at a target of 1.5 × ambient and was not delivered during days when the maximum temperatures were projected to be less than 15 °C or when plants were wet from fog, dew, or rain events. Additional details of the experimental design and pollutant generation and monitoring can be found in Karnosky et al. (2003b). Actual treatment summaries for CO2 and O3 were published in Karnosky et al. (2003b). Hourly O3 values for one control and one O3 ring (Fig. 3) show that our O3 exposure levels matched our 1.5 × ambient target quite well. In addition, we monitored a number of micrometeorological parameters at our site including wind speed, wind direction, PAR, net radiation, relative humidity, rainfall, air temperature at five heights to 20.0 m and soil temperature at the soil surface and at five depths to 2.0 m and soil moisture. Relevant web sites for the Aspen FACE project include: (1) the general site for the Aspen FACE (http://aspenface.mtu.edu); (2) the micrometeorology data collected at the Aspen FACE site (http://climate.usfs.msu.edu/FACE/meteorology/); (3) the treatment gas concentrations are shown at the BNL web site (http://www.face.bnl.gov/FACE_Site_Data_Archive/FACESites/FACTSII.htm) and the CDIAC data depository web site (http://cdiac.ornl.gov/programs/FACE/facts-IIdata/factsIIdata.html).
EXAMINATION OF CARBON FLOWS
In order to prioritize research at the Aspen FACE project, our site's investigator team spent a considerable amount of time developing a conceptual model of carbon cycling in our ecosystem (Fig. 4). Our research team has focused attention on control points (red triangles) in an attempt to develop a comprehensive understanding of ecosystem carbon flow under elevated CO2 and O3. We hypothesized that ecosystem level responses to these two greenhouse gases would be driven by the responsiveness of the three keystone tree species (Karnosky 2005). In this paper, we will summarize the effects of O3 on carbon uptake, allocation, distribution, and release at background and elevated levels of CO2. Finally, we discuss our progress scaling our results to regional levels and we present our results in terms of O3 metrics as best predictors of O3 effects.
All carbon flows into trees through leaves via the process of photosynthesis. Thus, the impacts of greenhouse gases on leaf morphology, chlorophyll content, Rubisco content, stomatal density, stomatal conductance, leaf area in the canopy, and phenology of leaf display play critical roles in carbon budgets of forest trees. In Fig. 5, it is shown that there is interspecific variability in the effects of elevated O3 and/or CO2 on maximal photosynthesis as the rapid-growing pioneer species, trembling aspen and paper birch, are both quite responsive to these two greenhouse gases but the slower-growing, later-successional species sugar maple is not very responsive to either gas (Noormets et al. 2001a,b; Karnosky et al. 2003b; Sharma et al. 2003).
The effects of O3 on photosynthesis have generally been negative for aspen at either CO2 concentration (Karnosky et al. 2003b), whereas birch photosynthesis was most affected at the elevated CO2. The depression of photosynthesis under elevated CO2 + O3 suggests co-occurring elevation of O3 could decrease the projected stimulation of photosynthesis under future CO2 concentrations (Kull et al. 1996).
Ozone effects on photosynthesis vary by aspen genotype, leaf age (Noormets et al. 2001a,b) and crown position (Sharma et al. 2003). Average maximal photosynthesis was depressed by 29–40%, depending on the aspen clone at ambient CO2 and by 19–31% under elevated CO2, compared with photosynthesis at elevated CO2 alone. Older leaves tended to be more severely affected by O3 at either CO2 concentration (Noormets et al. 2001a,b). The limitations to maximal photosynthesis were primarily driven by altered mesophyll processes, primarily by impacts on Rubisco (Noormets et al. 2001b). In addition, O3 decreased chloroplast size, starch content, and altered foliar ultrastructure (Oksanen, Sober & Karnosky 2001) in aspen but not in birch leaves. More recently, O3-induced decreases in mesophyll cell wall thickness and starch grain size were detected for both aspen and birch trees (Oksanen et al. 2003).
While no effects of elevated CO2 have been found in foliar respiration at our site (Davey et al. 2004), increased levels of foliar respiration have been detected in O3-damaged aspen leaves, particularly later in the growing season (Noormets et al. 2001a,b).
Since we have shown decreased maximal photosynthesis for aspen (see above), it is not surprising that we have documented a relatively consistent and statistically significant, O3-induced 10–15% decrease in both height and diameter growth in aspen from O3 at both ambient and elevated CO2 (Isebrands et al. 2001; Percy et al. 2002; Fig. 6). In contrast, birch has not shown adverse effects of O3 in ambient CO2. However, consistent and significant 14–18% decreases in growth of birch have been seen for elevated O3 in the elevated CO2 environment compared to birch in elevated CO2 alone.
The most interesting growth response we have found was that of sugar maple in that no significant O3 effects were detected for the first few years but growth has been significantly decreased since year four. After age 5, O3 had significantly decreased both height and diameter growth of sugar maple, regardless of the CO2 treatment. While we have not yet determined the cause for either the stronger O3 response in birch in the CO2 + O3 combination treatment or the significant long-term decrease in sugar maple growth under elevated O3. These two findings show the importance of long-term studies of interacting stresses in decreasing uncertainties about the impacts of O3 on forest ecosystems and the need to examine interacting stresses as the responses found were not predicted from the single-factor treatments.
Shifts in carbon allocation under elevated O3 are expected in our experiment because O3 often decreases carbon allocation to root systems (Andersen 2003). Our previous open-top chamber research with aspen suggested that O3 may alter C14 distribution to roots (Coleman et al. 1995) and that O3 differentially impacts root growth (Karnosky et al. 1996; Coleman et al. 1996). While a trend was seen in decreased soil respiration under elevated O3 suggesting possible adverse effects on root growth for our site (King et al. 2001), we did not detect any shifts in carbon allocation in sample whole-tree biomass harvests in 2000 (Pregitzer, unpublished) and 2002.
Canopy dynamics and phenology
In addition to photosynthetic rates, leaf area and leaf display duration contribute to carbon gain potential in forest trees. In our study, we have shown that O3 can have major negative impacts on both LAI (Fig. 7) and leaf display duration. LAI was significantly decreased under elevated O3 throughout the growing season and this is due to several factors. First, bud break is delayed so that leaf out is later in the spring, as has been previously reported by Oksanen (2003). Second, leaf senescence and leaf abscission are accelerated under elevated O3, regardless of CO2 concentration, as can be seen in late-season aerial photos (Fig. 8). Accelerated leaf aging is a well-documented phenomenon with O3 (Pell et al. 1990; Bielenberg, Lynch & Pell 2002) and we have previously reported on it in aspen (Karnosky et al. 1996). Third, the reduced LAI may have been partially due to decreased tree sizes (Isebrands et al. 2001; Percy et al. 2002), reduced branch and leaf sizes (Oksanen et al. 2001), or changes in crown architecture (Dickson et al. 2001).
Competition for light, nutrients, and water in a forest environment can have major impacts on the responses of trees to elevated levels of O3 and CO2 (Matyssek & Sandermann 2003). At the Aspen FACE experiment, we are testing both the effects of interspecific as well as intraspecific competition. Clear evidence has been presented from our project that the magnitude of the O3 effects on growth depended on the particular aspen genotype and its competitive status (McDonald et al. 2002). After 6 years of treatments, we can readily see the effects of CO2 and O3 on the competitive ability of aspen clones (Fig. 9). Clone 259 is not a good competitor in our experiment as seen by its poor growth in all treatments, but we have evidence that its fitness is particularly decreased under elevated O3 as evidenced by its decreased survival and inability to produce seed (Karnosky et al. 2003c). Interestingly, clone 8L appears to thrive in elevated O3 as it is growing at faster rates under high O3, regardless of CO2 treatment. We have previously seen enhanced growth in low levels of O3 (i.e. in 0.5 × ambient versus ‘O3-free air’ produced by charcoal filtering) (Karnosky et al. 1996) that was attributed to adaptation to elevated background O3 exposures at the location from which the clone originated. In general, however, the lowest growth rate of aspen is in the elevated O3 treatment and the CO2 + O3 treatment is nearly identical to growth under control conditions (Isebrands et al. 2001; Fig. 9).
Stem wood properties
Ozone significantly decreased volume of xylem as shown by decreased distance from the pith to the bark in our juvenile aspen stems but did not affect birch or maple stems (Kaakinen et al. 2004). Gravimetric lignin concentration increased under elevated O3 in four of five aspen clones and in birch (Kaakinen et al. 2004). This suggests a possible change in carbon allocation leading to enhanced activity of the phenylpropanoid biosynthetic pathway as we previously documented in our Aspen FACE project with increased PAL transcripts under elevated O3 (Wustman et al. 2001).
Another wood structure change illicited by O3 was that vessel lumen diameter decreased, which could decrease water transport efficiency in the xylem (Kaakinen et al. 2004). In birch, hemicellulose increased under elevated O3. Elevated CO2 largely offset adverse effects of O3 on both aspen and birch wood structure and chemistry (Kaakinen et al. 2004).
While the role of tropospheric O3 in altering plant growth and development has been thoroughly studied over the recent decades, there is still limited understanding regarding the effects of O3 on tree roots and soil processes (Andersen 2003). From our open-top chamber research with aspen, we knew that carbon allocation and partitioning to roots could be dramatically altered by O3 (Coleman et al. 1995). This, in turn, could lead to decreased root growth of aspen (Coleman et al. 1996) and altered root/shoot ratios (Karnosky et al. 1996). Thus, we expected going into the Aspen FACE experiment that we would likely be able to detect effects of O3 on root growth in aspen but did not know if birch or maple would be adversely affected. Furthermore, we were uncertain as to how interacting elevated CO2 and O3 would affect root growth and soil processes of any of the three species.
Early in our Aspen FACE experiment, we found that live fine-root biomass (< 1.0 mm) averaged over community types was 263 g−2, of which 81% was composed of roots < 0.5 mm in diameter (King et al. 2001). Elevated O3 resulted in a decrease in fine root biomass, which was marginally significant after three growing seasons (King et al. 2001). Elevated O3 has increased fine root turnover (Pregitzer, unpublished), as was previously found from our open-top chamber studies of O3 effects on aspen fine root dynamics (Coleman et al. 1996). As with our above-ground studies, elevated CO2 alleviated the negative effects of O3 on aspen roots. Conversely, elevated O3 offset increases in soil respiration caused by elevated CO2 when the two gases were applied in combination (King et al. 2001). Taken together, root studies at Aspen FACE suggest that elevated CO2 increases the flux of carbon from root systems to the soil, while elevated O3 alters whole plant source–sink relationships, resulting in more rapid root turnover and a smaller crop of standing fine root biomass (Karnosky & Pregitzer 2005).
Carbon inputs to the Aspen FACE soils were increased under elevated CO2 as seen by the increase in soil respiration (King et al. 2001, 2004). However, under the combination of elevated CO2 + O3, stable soil carbon formation was decreased by 50% compared to that under elevated CO2 alone (Loya et al. 2003; Fig. 10). This suggests that NPP-induced changes in the atmosphere may have a significant impact on the formation of stable soil carbon. These findings have begun to influence air pollution control strategies in Europe (see Grennfelt 2004).
Decomposition of leaf litter is another important part of carbon input into the forest ecosystem. Elevated CO2 altered birch litterfall chemistry at Aspen FACE, decreasing nitrogen content, and increasing condensed tannins, regardless of O3 concentration (Parsons, Lindroth & Bockheim 2004). Nitrogen content in decomposing litter from elevated CO2 treatments remained consistently lower up to 350 d. Ozone alone did not affect birch leaf litter quality or litter decompositon (Parsons et al. 2004).
Soil fauna and micro-organisms
Since O3 adversely affected aspen growth at Aspen FACE and since O3 impacts litter quality in aspen (Lindroth et al. 2001), Loranger, Pregitzer & King (2004) hypothesized that O3 could impact the abundance of soil fauna. They found significant decreases in Acari (−47%) under elevated O3, but these responses were alleviated by elevated CO2 (Loranger et al. 2004).
Phillips, Zak & Holmes (2002) presented evidence from Aspen FACE that O3 may be impacting microbial community composition at Aspen FACE. While microbial respiration was increased under elevated CO2, this increase was negated by the presence of co-occurring O3 (Phillips et al. 2002; Fig. 11). Fungal abundance declined under elevated O3 in both the aspen and aspen-birch communities but not in the aspen-maple community (Phillips et al. 2002).
Holmes et al. (2003) found that soil nitrogen transformations were impacted by O3(Fig. 12). Elevated O3 significantly decreased gross N mineralization and microbial biomass N. Effects were consistent across all three communities (Holmes et al. 2003). The authors suggested that by decreasing plant litter inputs, O3 appeared to be decreasing microbial biomass and activity.
SCALING ASPEN FACE RESPONSES WITH MODELS
Scaling responses from 30 m plots studied over 7 years at Aspen FACE to the landscape or regional levels over decades or centuries requires making a series of assumptions to bridge these gaps in scale. Through simulation modelling we can extrapolate the consequences of these assumptions over space and time (Laurence & Andersen 2003). Since the direct effects of O3 and CO2 occur as physiological effects on photosynthesis in individual leaves (Chappelka & Samuelson 1998), using a leaf-level model is a logical starting point for scaling. The ways that changes in leaf physiology can in turn affect growth of trees and their ability to compete within forest canopies can then be evaluated by using forest community or forest productivity models.
Two alternative models have been used at Aspen FACE to take leaf-level responses and predict their significance for whole-tree health. First, Martin et al. (2001) have developed a process-based model that predicts the relative effects of O3 on the photosynthetic rate and growth of an O3-sensitive aspen clone. Modifying the model ecophys, developed by Rausher et al. (1990), Host et al. (1996), and Isebrands et al. 2000, Martin et al. (2001) estimate seasonal growth, biomass accumulation, and leaf drop under various O3 profiles. Further adaptations enable the simulation of root growth and below-ground water redistribution (Theseira et al. 2003).
A second model is tregro (Weinstein, Beloin & Yanai 1991), which simulates carbon, water, and nutrient flows of an individual plant in response to changes in temperature, drought, nutrient deficiency, and exposure to pollutants and CO2 levels. The tregro model evaluates whether a reduction in the rate of photosynthesis in direct proportion to the cumulative O3 uptake would prevent an individual tree from meeting its carbon demands for growth. tregro then calculates how the plant is likely to shift its carbon allocation as a result of the lowered supply of carbon and mobilize stored carbon reserves to continue tissue growth.
The zelig model was applied to extrapolate the results from the Aspen FACE studies to regional forests of Wisconsin over 100 years of simulated stand development. Ozone was predicted to cause P. tremuloides basal area in the approximately 1.4 million hectares of aspen-birch stands throughout Wisconsin to decrease by over 1 million m2 cross-sectional area or 12% of the abundance expected in the absence of O3(Fig. 13). This level of reduction was expected because of the physiological sensitivity of P. tremuloides to O3. However, predictions for B. papyrifera demonstrate that scaling is not a simple matter of extrapolating directly from experimental results. Betula papyrifera was predicted to increase in abundance despite the absence of sensitivity to O3. The scaling methodology clearly must be capable of considering changes in the competitive opportunities among species, since in this case B. papyrifera thrived (11% increase) despite O3 because P. tremuloides was injured more severely. Betula papyrifera was then able to compete for resources in situations where previously it had not been able.
Elevated levels of CO2 caused 20% growth increases in B. papyrifera and 30% increases in P. tremuloides (Fig. 13). For P. tremuloides, this amounted to an increase of over 1 million m2, similar in size but opposite in direction to the effect of O3. Simultaneous exposure to O3 and CO2 had offsetting effects in B. papyrifera and P. tremuloides. Unpredictably, the competitive advantages B. papyrifera was simulated to have under O3 exposure disappeared when CO2 was also present. In another result from the landscape level that would not have been predictable from the physiological effects, the presence of CO2 exacerbated the negative effect of O3 on Acer saccharum abundance, causing it to decrease by over 30%.
How predictable were these landscape level effects from the individual plot responses? While it is somewhat difficult to compare 5 years of tree plot results to 100 years of landscape predictions, the changes in the landscape abundance of species were generally a reflection of responses that had been noted in average growth in the experimental plots (Table 1). For example, P. tremuloides decreased by 14% in the experimental plots but only by 12% in abundance by year 2100 in the simulation. In no case did the competitive dynamics among species on the landscape predicted in the simulation result in the opposite response to that observed in the plots. However, P. tremuloides was predicted to have twice the response to CO2 on the landscape as the plots suggested, and B. papyrifera had twice the response to O3.
Table 1. Comparison of responses at the scale of physiology, plot, and predicted landscape
FACE Amax reductions
O3 + CO2
Face plot effects measured
O3 + CO2
ZELIG landscape effects predicted in 2100
O3 + CO2
SCALING FOR RISK ANALYSIS
North America and Europe have adopted different approaches to ambient O3 standard setting, with the latter opting for an approach to specifically protect vegetation. In North America, ambient air quality standards (AAQS) are used for compliance purposes and are balanced against social, economic and political considerations (see Ashmore 2005). AAQS do not implicitly assume the existence of a concentration threshold for receptor (i.e. tree) response (Percy et al. 2003a), and therefore, target values are often substituted for regulatory purposes. In North America, the current primary O3 National AAQS is set at 0.08 ppm (80 ppb) and 0.065 (65 ppb) calculated as the 3-year average of the annual fourth highest daily maximum 8-h O3 concentrations for the US (Federal Register 1997) and Canada (CCME 2000), respectively.
In contrast, Europe has adopted critical levels (CLs) that assume a threshold concentration for receptor (tree) response exists (UN-ECE 1988; Tema Nord 1994). The CL concept implicitly requires that all adverse effects should be prevented regardless of the economic costs of reducing primary pollutant emissions. The current European CL, based upon the accumulated mean hourly exposure over time above an O3 concentration threshold of 40 ppb (AOT40), for forests is 10 000 ppbh (10 ppmh) and is calculated for daylight hours with global clear-sky radiation during a 6-month (April–September) period (Kärenlampi & Skärby 1996). The continuously evolving UN-ECE process recently concluded that the CL for forest trees should be based upon stomatal uptake (Karlsson, Selldén & Pleijel 2003; see Ashmore 2005).
Independent of the various experimental methods used, however, there remain a number of uncertainties. First of all, hourly ambient O3 concentrations follow a rather complex, three-parameter Weibull distribution (Nosal, Legge & Krupa 2000). Secondly, weekly or bi-weekly O3 concentration means or seasonal concentration summation methods cannot capture the dynamic changes of the atmosphere and plant biology (Krupa & Kickert 1997). Thirdly, cause–effect relationships that have been established have used empirical/statistical, and mechanistic/process models, the former relying heavily on correlations and multivariate linear regression models. However, even a statistically significant correlation does not necessarily mean causality. The effect of O3 on tree growth is a complex phenomenon and its quantitative characterization will require more complex, non-linear regression models. Fourthly, in most investigations saplings rather than mature tree responses have been examined (Samuelson & Kelly 2001; Kolb & Matyssek 2001). Finally, even though O3 may have a statistically significant effect on tree growth, it is usually not the ecologically dominant factor. There are meteorological (e.g. precipitation, soil moisture, solar radiation, temperature, etc.) factors, co-occurring air pollutants, and many other variables that exert large effects on tree growth.
In order to meaningfully assess the risk of increasing O3 concentrations, it is vital to build a predictive model comprising all important predictors. Krupa et al. (2003) have recently developed a multivariate statistical model including meteorological variables (global radiation, air temperature, relative humidity and wind speed, variables that influence plant O3 uptake through stomata). With the addition of soil moisture data to the main meteorological variables listed, an approximation of first-order atmospheric O3 flux can be achieved. After verification of validity and significance of such a model, it is then necessary to factor out the effect of O3 itself, while controlling all other predictors. This is a complicated procedure requiring integrated experiments such as Aspen FACE, which provide systematic and reliable monitoring of pertinent predictors.
Coincidentally, evidence from our Aspen FACE experiment is pointing to the multitropic nature of forest ecosystem responses to long-term, low-level O3 exposures. Feedbacks to growth have included a large reduction in both aspen height (−12%) and diameter (−13%) growth at the stand level (Percy et al. 2002). We have now taken the initial steps towards linking a multivariate statistical model (Krupa et al. 2003) with multipoint plant response data. After computing O3 exposure within each of the three replicate FACE rings using established AAQS, CL, and related descriptors, O3 dose–response functions relevant to regulatory processes have been calculated.
Initial analysis using The Best Subsets Regression Algorithm (Percy et al. unpublished) suggests the best predictor of aspen growth was the 4th highest daily maximum 8 h O3 concentration (Table 2) followed by tree age. As a second step in the process, meteorological data (T, RH, PAR, precipitation) are being combined with soil moisture data at the stand level to develop an approximation of first-order atmospheric O3 flux and aspen stomatal uptake. If such efforts are coupled to multipoint plant response measurements, meaningful cause–effect relationships can be derived regarding the nature of the so-called background O3 concentrations and their significance in more remote forested areas (Krupa et al. 2003). The future development of new flux-based critical levels in Europe and biologically based dose–response functions in North America will allow policy makers and regulators for the first time to more accurately predict O3 risk to the world's forests in the future.
Table 2. Best subsets regression analysis of dependence of aspen clone growth on a variety of ozone exposure indexes and tree age for trees growing in the Aspen FACE projecta
Best single predictor
Adj. R-Sq %
Adj. R-Sq % single predictor
Maximum 1 h O3 concentration; maximum 8 h O3 concentration; SUM60; 4th highest daily maximum 8 h O3 concentration; AOT40 (various 3-month sums); AOT40 (6 month); and tree age (1–5 years).
4th, 3-year average of the annual fourth highest daily maximum 8-h O3 concentrations; from used to calculate US EPA and CWS AAQS.
We have examined over 7 years the effects of elevated levels of O3 at two atmospheric CO2 levels, current ambient (360 ppm) and 560 ppm (projected for about year 2050), on northern Wisconsin aspen, aspen-birch, and aspen-maple forest communities. In this paper, we elucidate how O3 affects the flow of C from the leaf and canopy level through tree roots to soil and soil micro-organisms, under ambient and elevated CO2. Our long-term, multidisciplinary research project has consistently shown adverse effects of O3 on the above-ground growth and physiology of all three species. These impacts on above-ground biochemistry, physiology and morphology with feedbacks to growth and pest occurrence have cascaded through the ecosystem via multiple food webs and trophic levels ultimately affecting ecosystem C cycling. While CO2 generally moderated the detrimental responses of O3, there were some noticeable exceptions, including the long-term growth suppression of sugar maple and paper birch, which could not have been predicted by studies of these two important greenhouse gases applied singly or for a short-term.
Our results suggest that fine roots are key mediators of ecosystem response to these greenhouse gases, regardless of forest community type. Secondly, they highlight the importance of bottom-up changes caused by the combined effects of CO2 and O3 on food quality and the long-term population dynamics of forest pests. Futhermore, they suggest establishing links between net primary productivity, the biochemical constituents of plant litter, and the metabolic responses of microbial communities which are crucial to a mechanistic understanding of how these greenhouse gases will alter soil C and N cycling, as well as the long-term forest ecosystem productivity.
We are attempting to scale up our results to project O3 responses of forest regions using various process-based models linked to canopy gap models. In addition, we are using a regression approach to find the best policy-relevant predictors of our observed O3 effects on growth.
This research was partially supported by the Office of Science (BER), US Department of Energy, Grant No. DE-FG02–95ER62125, DE-FG02–93ER6166, DE-FG02–98ER62680, USDA Forest Service Northern Global Change Program, the National Science Foundation (DBI-9601942, IBN-9652674), the USDA NRI Competitive Grants Programs (000–2982, 001–00796, 001–01193), the National Council of the Paper Industry for Air and Stream Improvement (NCASI), Michigan Technological University, the Praxair Foundation, the McIntire-Stennis Program, the Brookhaven National Laboratories/US Department of Energy (725–079), Canadian Federal Panel on Energy Research and Development, and Natural Resources Canada–Canadian Forest Service. The authors would like to thank C.E. Johnson and David Fowler for providing the 2050 STOCHEM model O3 output map.