Abstract

Both increases in temperature and changes in precipitation may limit future tree growth, but rising atmospheric CO2 could offset some of these stressors through increased plant Water Use Efficiency (WUE). The net balance between the negative impacts of climate change and positive effects of CO2 on tree growth is crucial for ecotones, where increased climate stress could drive mortality and shifts in range. Here, we quantify the effects of climate, stand structure, and rising CO2 on both annual tree-ring growth increment and intrinsic WUE (iWUE) at a savanna-forest boundary in the Upper Midwest United States. Taking a Bayesian hierarchical modelling approach, we find that plant iWUE increased by ~ 16–23% over the course of the twentieth century, but on average, tree-ring growth increments do not significantly increase. Consistent with higher iWUE under increased CO2 and recent wetting, we observe a decrease in sensitivity of tree growth to annual precipitation, leading to ~ 35–41% higher growth under dry conditions compared to trees of similar size in the past. However, an emerging interaction between summer maximum temperatures and annual precipitation diminishes the water-savings benefit under hot and dry conditions. This decrease in precipitation sensitivity, and the interaction between temperature and precipitation are strongest in open canopy microclimates, suggesting that stand structure may modulate response to future changes. Overall, while higher iWUE may provide some water savings benefits to growth under normal drought conditions, near-term future temperature increases combined with drought events could drive growth declines of about 50%.

Highlights

  • Future increases in temperature, changes in precipitation regimes, and elevated atmospheric C­ O2 have the potential to drive large shifts in tree growth and distribution (Allen and Breshears 1998; Scheller and Mladenoff 2008; Reinmann and Hutyra 2017; Nolan et al 2018)

  • Using a Bayesian hierarchical framework, we model both tree growth and intrinsic Water Use Efficiency (WUE) of Quercus spp. trees of two different cohorts: those that experienced either low ­CO2 or high C­ O2 levels, that are similar in most other aspects

  • We document increases in intrinsic WUE (iWUE) and decreases in drought sensitivity that are consistent with a positive effect of C­ O2 on tree function in the Upper Midwest, but these changes do not result in detectable increases in tree growth

Read more

Summary

Introduction

Changes in precipitation regimes, and elevated atmospheric C­ O2 have the potential to drive large shifts in tree growth and distribution (Allen and Breshears 1998; Scheller and Mladenoff 2008; Reinmann and Hutyra 2017; Nolan et al 2018). The net effects of divergent environmental changes on trees are critical at ecotone or biome boundaries, where drought stress, amplified by microclimatic feedbacks could drive severe tree growth declines and a shifts in distribution (Breshears et al 2005; Adams et al 2009; Allen et al 2015; Clark et al 2016; Charney et al 2016; Druckenbrod et al 2019). Quantifying long term responses of tree growth to joint changes in temperature, precipitation, and ­CO2 is critical to forecast future function at biome boundaries

Methods
Results
Discussion
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call