Understanding climate change-associated tree mortality is central to linking climate change impacts and forest structure and function. However, whether temporal increases in tree mortality are attributed to climate change or stand developmental processes remains uncertain. Furthermore, interpreting the climate change-associated tree mortality estimated from old forests for regional forests rests on an un-tested assumption that the effects of climate change are the same for young and old forests. Here we disentangle the effects of climate change and stand developmental processes on tree mortality. We show that both climate change and forest development processes influence temporal mortality increases, climate change-associated increases are significantly higher in young than old forests, and higher increases in younger forests are a result of their higher sensitivity to regional warming and drought. We anticipate our analysis to be a starting point for more comprehensive examinations of how forest ecosystems might respond to climate change.
Observational studies have relied on old forests to quantify temporal trends in background tree mortality, and have shown that tree mortality has increased with recent global warming, increasing atmospheric CO2 and decreasing water availability in tropical, temperate and boreal forests1,2,3,4,5. Old forests are assumed to be in an equilibrium state where tree mortality is matched by recruitment, and temporal changes in tree mortality at the forest level due to endogenous processes are assumed to be weak at this stage of stand development6,7. However, whether there is ever equilibrium is a contentious issue8. Although the effects of competition estimated by temporal changes of stand basal area (SBA) and stand density on tree mortality have been investigated in some previous studies4,5, conspecific negative density dependence and tree aging could also influence tree dynamics9,10. Furthermore, the temporal increase of tree mortality could be driven by stand development processes, but not necessarily climate change11,12. Unfortunately, previous studies have used unsuitable statistical methods that marginalize either climate or non-climate drivers for longitudinal data in which these drivers are highly correlated13. Therefore, the relative roles that climate change and stand development processes have on the temporal changes in tree mortality remain uncertain.
Furthermore, climate change-associated tree mortality increases in old forests have been used to represent the tree mortality response of regional forests to climate change14, based on the assumption that effects of climate change on tree mortality are same for young and old forests. However, this assumption has not been specifically tested. Verification of the assumption is essential for disturbance-driven ecosystems such as boreal forests. Because of high fire frequency, the boreal forests are a mosaic of stands at various developmental stages with old forests accounting for only a small portion of the landscape15,16. With a predicted increase of fire frequency associated with global warming, the mean age of the boreal forests is expected to decrease, as will the portion of old forests17. Thus, understanding how young forests respond to climate change is essential to predict how boreal forests will respond to future climate change. If tree mortality responses to climate change differ between young and old forests, increased tree mortality based on old forests will be biased for regional forest predictions.
Here we analyzed tree mortality patterns of boreal tree species in western Canada using 887 permanent sample plots measured between 1958 and 2007. To account for uncertainties in sampling, models and parameters, we used Bayesian models18,19 to disentangle endogenous (stand development) and exogenous (year, temperature anomaly or drought) effects on individual tree mortality for five major boreal tree species, Populus tremuloides Michx., Populus balsamifera L., Pinus banksiana Lamb., Picea mariana Mill. and Picea glauca (Moench) Voss. We tested the assumption that tree mortality increases associated with climate change do not differ with forest age. We also examined whether tree mortality increases are linked to recent regional warming and its negative consequence on water availability. We show that both climate change and forest development processes influence temporal mortality increases, climate change-associated increases are significantly higher in young than old forests, and higher increases in younger forests are a result of their higher sensitivity to regional warming and drought. Furthermore, climate change-associated mortality increases are stronger for moist-habitat-adapted Populus balsamifera and late-successional Picea mariana and Picea glauca than Populus tremuloides and Pinus banksiana.
Effects of year and stand development processes on tree mortality
With all data pooled, the effects of year, used to represent climate change drivers as a whole in both Model 1 (with only year as a predictor) and Model 2 (with year, endogenous processes and their interactions as predictors) were significantly positive for all study species (Table 1; Fig. 1), indicating significant increases of annual mortality probability during the study period (Fig. 2). The two models, however, produced different estimates for climate change-associated tree mortality: year effects estimated by Model 1 are bigger for Populus tremuloides, Pinus banksiana, Picea mariana and Picea glauca, but smaller for Populus balsamifera than those by Model 2 (Fig. 1a), resulting in different estimates of annual tree mortality probability from the two models (Fig. 2).
Tree mortality was strongly affected by stand development processes and their interactions with year (Fig. 1b, Supplementary Table S4). Year effect decreased significantly with stand age (SA) for all study species (Table 1). Year effect also increased with stand crowding as measured by SBA and in stands with more conspecific individuals for Picea mariana and Picea glauca (Table 1). Tree mortality increases associated with year differed among species with stronger year effects on late-successional Picea mariana and Picea glauca and moist-habitat-adapted Populus balsamifera than Populus tremuloides and Pinus banksiana (Fig. 1a).
When data were analyzed separately for young forests (initial SA ≤80 years) and old forests (initial SA >80 years, same as in Peng et al.5), year effect was consistently higher in young forests than old forests for all species (Fig. 1a), supporting the strong declining year effect with increasing SA (Table 1). Predicted annual mortality increased by 2.88%, 4.70%, 5.64% and 6.18% per year in young forests, but increased at the lower rates of 1.65%, 2.24%, 3.89% and 4.12% in old forests for Populus tremuloides, Populus balsamifera, Picea mariana and Picea glauca, respectively (Supplementary Fig. S3). For drought-tolerant Pinus banksiana, annual mortality increased by 2.09% per year in young forests, but year had no detectable effect on its mortality in old forests (Supplementary Fig. S3). In both young and old forests, endogenous factors were critical drivers of tree mortality for all study species (Fig. 1b; Supplementary Tables S6 and S7).
Warming and drought effects on tree mortality
For the study area, annual temperature anomaly (ATA) increased at 0.034 °C year−1, and annual climate moisture index anomaly (ACMIA) decreased at 0.088 year−1, whereas the growing season precipitation anomaly slightly increased at 0.761 mm year−1 between 1958 and 2007 (Supplementary Fig. S4; Supplementary Table S7). To examine whether increase of mortality could be attributed to regional warming and drought, we developed models that replaced year by these climatic variables (Models 3 and 4). The ATA models showed positive main ATA effects on mortality of all species and higher ATA effects in young than old forests of all species except Pinus banksiana (Table 2). The ACMIA models indicated negative main ACMIA effects on mortality of all species and greater effects for Populus balsamifera, Picea mariana and Picea glauca than the other two species. Furthermore, the ACMIA effects were stronger in young than old forests for all species except Pinus banksiana (Table 2).
Unlike previous attributions of temporal increases in tree mortality to either climate change1,2,3,4,5 or stand development processes10,12, by using Bayesian models, we show that both stand development processes and climate change have affected temporal increases in tree mortality. These findings are not likely a result of methodological problems because heterogeneity in sampling strategies had no effect on mortality (Supplementary Figs S5 and S6), though we note that we have not explicitly considered alternate exogenous factors here. Tree mortality associated with year decreased for all species except Populus balsamifera when stand development factors were included as predictors. The differences in year effect between the models provide support for the notion that studies excluding endogenous factors can potentially produce biased estimates of climate change effects in boreal forests13. The decreased year effect on tree mortality is attributable to stand development processes during the study period. For example, both SA and SBA increased (Supplementary Table S10), both of which positively affected tree mortality (Supplementary Table S4). Also, an increase in the conspecific density of shade-tolerant Picea mariana and Picea glauca (Supplementary Table S10), reflecting the nature of secondary succession in boreal forests6,20, intensified a negative density-dependence effect on these two species (Table 1). The increased year effect in moist-habitat-adapted Populus balsamifera suggests that reduced water availability might have overweighed endogenous effects.
Our results show that mortality increases associated with climate change were significantly higher in young than old forests, and the higher increase in younger forests appears to be due to higher mortality sensitivity to recent regional warming and the resulting negative consequence on water availability. This finding indicates that climate change-associated increases in tree mortality would be underestimated if only old forests are used to represent regional forests. Compared with old forests, even-aged young forests established after a stand-replacing disturbance may experience greater competition for space and nutrients among young trees that tend to occupy the same ecological niche6,7, resulting in them being more vulnerable to external stressors such as climate change-associated drought21,22. The positive effect of regional warming on mortality could also be attributed to the interdependencies among warming, drought and forest pests23,24,25. In our study area, outbreaks of forest pests could have a role in the temporal mortality increases26,27,28.
Mortality responses to climate change differed among species, suggesting that the regional forest may be undergoing forest compositional shift that is independent of endogenous forest succession. The highest mortality increase in Populus balsamifera among pioneer species indicates that reduced water availability by regional warming has the greatest influence on species adapted to moist habitats. The higher mortality increases of late-successional Picea mariana and Picea glauca than those of early-successional Populus tremuloides and Pinus banksiana in both young and old forests (Figs 1 and 2) suggest that the regional forest will likely become further dominated by early-successional species if current warming trends continue. The different responses of tree mortality among species, coupled with those by climate change-associated fire activities15,16,17,29 that promote early-successional species30, may pose a significant conservation challenge for the region under further global warming.
We show evidence that long-term tree mortality trends are influenced by both stand development processes and long-term climate trends, that is, regional warming and drought. Note that the strength of these drivers on tree mortality differs among species, and their influences interact both among endogenous factors and between endogenous and exogenous factors. Because of the higher sensitivity to recent climate change in young than old forests, climate change-associated tree mortality could be underestimated if mortality estimates from old forests are used to represent regional forests. Tree mortality responses to climate change differed among species, and these different responses can have strong implications for future forest composition in the western boreal forest.
Study area and the forest inventory data
We analyzed longitudinal data from 887 permanent sampling plots established in Alberta and Saskatchewan (Supplementary Data 1 and Supplementary Fig. S1). Details for plot establishment, measurements and selection criteria are described in Supplementary Methods.
To examine whether long-term tree mortality trends are affected by long-term climate change trends, similar to previous studies1,2,3,4,5,12, we used the middle calendar year of a census period, during which tree mortality measurements were made between two successive censuses, to represent climate change drivers as a whole. To account for the effects of endogenous factors including asymmetric competition, stand crowding, tree ageing and inter-specific interaction on tree mortality, we used the tree’s relative basal area (RBA; ratio of subject tree basal area to the mean tree basal area of the stand), SBA, SA and the ratio of focal species’ basal area to SBA, calculated using the preceding measurement of each census period10.
Climate anomalies were defined as the departure from the long-term climate means31. Because our dependent variable, tree status, was observed at the end of a census period, the departure from the long-term mean for each climate variable was defined as the difference between its mean value during the census period and its long-term mean. Long-term climate means were calculated based on the 1950–2007 time period, during which plot measurements were taken. Three sets of climate anomalies were calculated: ATA, growing season precipitation anomaly and ACMIA. We derived temperature and precipitation data using scale-free ClimateWNA32,33 and climate moisture index (CMI) using BioSIM34 from latitude, longitude and elevation of each sample plot. Annual CMI was the sum of monthly CMIs over 12-month periods from last 1 August to 31 July of the current year, where monthly CMI was the quantity of monthly precipitation minus monthly potential evapotranspiration, which was computed using a simplified form of the Penman–Monteith equation35. A smaller CMI value indicated a drier condition. The summary statistics for explanatory variables were presented in Supplementary Table S2.
Annual mortality probability calculations
We used individual tree mortality analyses rather than plot-level mortality analyses to accommodate the individual tree-level variable, RBA, because (1) RBA is the strongest predictor of tree mortality in non-equilibrium boreal forests and (2) its control on tree mortality can change with SBA and ratio of focal species’ basal area to SBA10. Similar to previous studies36,37, we were interested in estimating annual tree mortality probability where measurement intervals varied (Supplementary Fig. S2e). We derived annual mortality probability from tree status as follows.
The survival probability, S, of tree i, for census period j of t years, in plot k is expressed as a function of annual survival probability, s:
Lastly, we related a tree’s status at the end of the census period (Mijk, alive or dead) to annual mortality probability using Bernoulli likelihood:
For each species, we developed individual tree mortality models using Hierarchical Bayesian logistic regression with plot identity as a random effect to account for uncertainties potentially affected by different forest characteristics or in different climatic and/or edaphic conditions18,19.
where α and β are the intercept and estimated coefficients, respectively; Xijk represents explanatory variables corresponding to tree i for census period j in plot k; and the model included a term πk to describe the random effect of sampling plots. As a rule of thumb, πk is in normal distribution with a mean of 0.
To examine whether inclusion of endogenous factors alters climate change-associated tree mortality, we compared the year effect between models with and without inclusion of endogenous factors as predictors, that is, Model 1 and Model 2, respectively.
where f(En) in Model 2 was developed based on our previous work10 to account for the endogenous effects on tree mortality:
where βs are the coefficients. We modelled the mortality probability as an exponential function of RBA because our previous results showed that mortality probability decreases exponentially with RBA10. The Akaike information criterion also indicated that the exponential transformation of RBA gave better fits for all species (Supplementary Table S3). Furthermore, our previous work10 showed near-linear mortality trends with tree aging and with SBA after taking account of competition and species interaction. Consequently, we modelled mortality probability as a linear function of SA and SBA.
Both Models 1 and 2 were developed for all plots, young forest plots and old forest plots, respectively, to examine how the inclusion of endogenous factors affect year effect in these three scenarios. Following Peng et al.5, we defined that young forests were ≤80 years of age and old forests >80 years of age at the first census.
To examine whether increases of mortality could be attributed to regional warming and its negative consequence on water availability, we developed models that replaced year with the climatic variables in Model 2, resulting in Models 3 and 4.
To examine the temporal trends of endogenous and exogenous factors at the plot level, Y, we used the Hierarchical Bayesian linear (HBL) model.
where Yjk is dependent variable, that is, endogenous factors and exogenous factors; α and β are intercept and estimated coefficients, respectively; Yearjk represents middle calendar year at for census period j in plot k; and the model included a term πk to describe the random effect of sampling plots.
For all analyses, the Bayesian Markov Chain Monte Carlo methods were implemented using JAGS38 called from R39 with rjags package40. All coefficients were assigned non-informative priors. All independent variables were centred to reduce their correlations and speed up convergence. For each model, we evaluated convergence by running two independent chains with different initial values and monitoring the Gelman–Rubin statistic41. When convergence was confirmed, an additional 10,000 iterations with thinning of half were used to calculate the mean, s.d. and 95% credible interval for each coefficient from the posterior distribution.
We developed full models and sequentially removed dimensionless explanatory variables whose posterior 95% credible interval covered 0. The reduced models, assessed by Deviance Information Criterion, were better than or similar to full models (Supplementary Table S11). Consequently, we selected the reduced models as our final models. To assess the adequacy of the final models, we calculated the area under the receiver operating characteristic curve (AUC) based on the mean of each coefficient using ROCR package42. A value of AUC >0.8 indicates that a model has excellent discriminatory power, and a value >0.7 indicates good discriminatory power43.
Finally, we calculated the mortality sensitivity scores to endogenous factors, exogenous factors and their interactions as a measure of the influences of these factors on mortality. Similar to Dietze and Moorcroft37, we defined sensitivity score on annual mortality probability as the s.d. of the predicted annual mortality probability for each of the above three groups of factors, holding the other two groups of variables at their mean.
To present how annual mortality probability changes over the study period, we summarized posterior distribution of annual mortality probability (mean and 95% credible interval) using mean of each parameter (β) from the final models. We also calculated the annual fractional change of mortality probability associated with year over the study period using the equation exp(β)−1, in which β is fitted coefficient for Year.
Assessing possible methodological problems
We first examined the spatial auto-correlation and heterogeneity in sampling strategies following the method described by van Mantgem et al.4. For all study species, Mantel tests showed no evidence of spatial auto-correlation among the plots for annual mortality probability, annual fractional change of mortality probability or the effect of plot identity on annual mortality probability (Supplementary Table S12). The selected permanent sampling plots were located in ecologically heterogeneous regions, and close geographic configuration does not imply similarity in forest characteristics. Our result that mortality probability increased more so in young forests than old forests could also be mistaken if the young forest plots were spatially clustered. Thus, we also examined the spatial auto-correlation for initial SAs. For all study species, the mantel tests showed no evidence of spatial auto-correlation among the plots for initial SA (Supplementary Table S12).
The linear regressions that related annual mortality fractional change to plot size and average census interval showed that neither plot size nor average census interval was significantly related to annual mortality fractional change (Supplementary Figs S5 and S6). These results indicate that the variation of mortality changes could not be attributed to plot size heterogeneity or the variation in census intervals.
How to cite this article: Luo, Y. and Chen, H.Y.H. Observations from old forests underestimate climate change effects on tree mortality. Nat. Commun. 4:1655 doi: 10.1038/ncomms2681 (2013).
Phillips O. L., Gentry A. H. Increasing turnover through time in tropical forests. Science 263, 954–958 (1994).
Phillips O. L. et al. Pattern and process in Amazon tree turnover, 1976-2001. Philos. Trans. R. Soc. Lond. B, Biol. Sci. 359, 381–407 (2004).
van Mantgem P. J., Stephenson N. L. Apparent climatically induced increase of tree mortality rates in a temperate forest. Ecol. Lett. 10, 909–916 (2007).
van Mantgem P. J. et al. Widespread increase of tree mortality rates in the western United States. Science 323, 521–524 (2009).
Peng C. H. et al. A drought-induced pervasive increase in tree mortality across Canada's boreal forests. Nat. Clim. Change 1, 467–471 (2011).
Chen H. Y. H., Popadiouk R. V. Dynamics of North American boreal mixedwoods. Environ. Rev. 10, 137–166 (2002).
Franklin J. F. et al. Disturbances and structural development of natural forest ecosystems with silvicultural implications, using Douglas-fir forests as an example. For. Ecol. Manage. 155, 399–423 (2002).
Connell J. H., Slatyer R. O. Mechanisms of succession in natural communities and their role in community stability and organization. Am. Nat. 111, 1119–1144 (1977).
Johnson D. J., Beaulieu W. T., Bever J. D., Clay K. Conspecific negative density dependence and forest diversity. Science 336, 904–907 (2012).
Luo Y., Chen H. Y. H. Competition, species interaction and ageing control tree mortality in boreal forests. J. Ecol. 99, 1470–1480 (2011).
Lutz J. A., Halpern C. B. Tree mortality during early forest development: a long-term study of rates, causes, and consequences. Ecol. Monogr. 76, 257–275 (2006).
Thorpe H. C., Daniels L. D. Long-term trends in tree mortality rates in the Alberta foothills are driven by stand development. Can. J. For. Res. 42, 1687–1696 (2012).
Brown C. J. et al. Quantitative approaches in climate change ecology. Global Change Biol. 17, 3697–3713 (2011).
Birdsey R., Pan Y. D. Ecology drought and dead trees. Nat. Clim. Change 1, 444–445 (2011).
Weir J. M. H., Johnson E. A., Miyanishi K. Fire frequency and the spatial age mosaic of the mixed-wood boreal forest in western Canada. Ecol. Appl. 10, 1162–1177 (2000).
Pan Y. et al. Age structure and disturbance legacy of North American forests. Biogeosciences 8, 715–732 (2011).
Fauria M. M., Johnson E. A. Climate and wildfires in the North American boreal forest. Philos. Trans. R. Soc. Lond. B, Biol. Sci. 363, 2317–2329 (2008).
Clark J. S. Uncertainty and variability in demography and population growth: A hierarchical approach. Ecology 84, 1370–1381 (2003).
Wikle C. K. Hierarchical Bayesian models for predicting the spread of ecological processes. Ecology 84, 1382–1394 (2003).
Chen H. Y. H., Taylor A. R. A test of ecological succession hypotheses using 55-year time-series data for 361 boreal forest stands. Global Ecol. Biogeogr. 21, 441–454 (2012).
Linares J. C., Camarero J. J., Carreira J. A. Competition modulates the adaptation capacity of forests to climatic stress: insights from recent growth decline and death in relict stands of the Mediterranean fir Abies pinsapo. J. Ecol. 98, 592–603 (2010).
Moreno-Gutierrez C. et al. Stand structure modulates the long-term vulnerability of Pinus halepensis to climatic drought in a semiarid Mediterranean ecosystem. Plant Cell Environ. 35, 1026–1039 (2012).
Allen C. D. et al. A global overview of drought and heat-induced tree mortality reveals emerging climate change risks for forests. For. Ecol. Manage. 259, 660–684 (2010).
McDowell N. G. et al. The interdependence of mechanisms underlying climate-driven vegetation mortality. Trends Ecol. Evol. 26, 523–532 (2011).
Anderegg W. R. et al. The roles of hydraulic and carbon stress in a widespread climate-induced forest die-off. Proc. Natl Acad. Sci. USA 109, 233–237 (2012).
Michaelian M., Hogg E. H., Hall R. J., Arsenault E. Massive mortality of aspen following severe drought along the southern edge of the Canadian boreal forest. Global Change Biol. 17, 2084–2094 (2011).
Cullingham C. I. et al. Mountain pine beetle host-range expansion threatens the boreal forest. Mol. Ecol. 20, 2157–2171 (2011).
Hogg E. H., Brandt J. P., Kochtubajda B. Growth and dieback of aspen forests in northwestern Alberta, Canada, in relation to climate and insects. Can. J. For. Res. 32, 823–832 (2002).
Larsen C. P. S. Spatial and temporal variations in boreal forest fire frequency in northern Alberta. J. Biogeogr. 24, 663–673 (1997).
Ilisson T., Chen H. Y. H. Response of six boreal tree species to stand replacing fire and clearcutting. Ecosystems 12, 820–829 (2009).
Clark J. S., Bell D. M., Hersh M. H., Nichols L. Climate change vulnerability of forest biodiversity: climate and competition tracking of demographic rates. Global Change Biol. 17, 1834–1849 (2011).
Wang T., Hamann A., Spittlehouse D. L., Aitken S. N. Development of scale-free climate data for western Canada for use in resource management. Int. J. Climatol. 26, 383–397 (2006).
Mbogga M. S., Hamann A., Wang T. L. Historical and projected climate data for natural resource management in western Canada. Agri. For. Meteor. 149, 881–890 (2009).
Réginère J., Saint-Amant R., Béchard A. BioSIM 10 User’s Manual Natural Resources Canada, Canadian Forest Service, Laurentian Forestry Centre: Sainte-Foy, Quebec, Canada, (2012).
Hogg E. H., Brandt J. P., Michaellian M. Impacts of a regional drought on the productivity, dieback, and biomass of western Canadian aspen forests. Can. J. For. Res. 38, 1373–1384 (2008).
Hurst J. M., Allen R. B., Coomes D. A., Duncan R. P. Size-specific tree mortality varies with neighbourhood crowding and disturbance in a Montane Nothofagus forest. PLoS One 6, e26670 (2011).
Dietze M. C., Moorcroft P. R. Tree mortality in the eastern and central United States: patterns and drivers. Global Change Biol. 17, 3312–3326 (2011).
Plummer M. JAGS: Just another Gibbs sampler <http://sourceforge.net/projects/mcmc-jags/> (2011).
R Development Core Team. R: A Language and Environment for for Statstical Computing <http://www.R-project.org/> (2011).
Plummer M. rjags: Bayesian graphical models using MCMC <http://CRAN.R-project.org/package=rjags> (2011).
Gelman A., Rubin D. B. Inference from iterative simulation using multiple sequences. Stat. Sci. 7, 457–472 (1992).
Sing T., Sander O., Beerenwinkel N., Lengauer T. ROCR: Visualizing the performance of scoring classifiers <http://CRAN.R-project.org/package=ROCR> (2009).
Hosmer D. W., Lemeshow S. Applied Logistic Regression 2nd edn John Wiley & Sons, Inc.: New York, NY, USA, (2000).
We thank the Forest Management Branch of Alberta Ministry of Sustainable Resource Development and the Forestry Branch of Saskatchewan Renewable Resources for providing detailed data; Michael Dietze for his help with JAGS; and Samuel Bartels, Brian Brassard, Gordon Kayahara, Joan Keene, Anthony Taylor and Jian Wang for their comments. This study was supported by the Natural Sciences and Engineering Research Council of Canada (DG 283336-09), the Early Researcher Award Program of Ontario Ministry of Research and Innovation, and Northern Ontario Heritage Foundation. Y.L. acknowledges Ontario Forest Ecosystem Science Co-operative Inc. and the Natural Sciences and Engineering Research Council of Canada for a doctoral research scholarship.
The authors declare no competing financial interests.
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Luo, Y., Chen, H. Observations from old forests underestimate climate change effects on tree mortality. Nat Commun 4, 1655 (2013). https://doi.org/10.1038/ncomms2681
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