Abstract
Climate change has dramatically altered the frequency and intensity of droughts, thereby altering tree growth. Understanding whether tree growth in semiarid areas in response to long-term drought and the post-drought recovery rate of tree growth vary along moisture gradients is crucial for predicting future forest change. Here, we assessed the spatial variation in both the growth resistance of Qinghai spruce (Picea crassifolia Kom.) to long-term drought and its post-drought recovery using a stand-total sampling strategy along a moisture gradient that covered three sites (with an annual precipitation of 330.4, 394.2, and 515.9 mm for the western, middle, and eastern sites, respectively) with six plots. Resistance and recovery were evaluated by analyzing the tree growth trends during a long-term drought period (1980–2001) and the subsequent post-drought period (2001–2013), respectively. Our results indicate that the trees with the highest temporal stability were those at the wetter eastern site; specifically, during the long-term drought period, the trees at the wetter eastern site showed the highest resistance (−0.015) and the lowest recovery (0.002). The trees in moderately arid conditions were much more sensitive to climate change than those at the relatively arid western site, showing the lowest resistance (−0.050) and highest recovery (0.020). Climate change had the strongest impact on tree growth at the moderately arid site, contributing 60.6% to the tree growth decreasing trend during the long-term drought period and 65.4% to the tree recovery during the post-drought period, respectively. Climate change had a lower impact on tree growth at the wet and dry sites, contributing less than 50% to the tree growth trends at these sites. The results indicate that a trade-off relationship exists between resistance and recovery at the different sites; that is, the highly resistant trees at the wetter eastern site tend to have lower recovery, whereas the weakly resistant trees at the moderately arid site tend to have higher recovery. These results have implications for predicting tree growth in response to future climate change.
Highlights
Licensee MDPI, Basel, Switzerland.Drought exerts a strong suppressive effect on tree growth through water deficit or carbon starvation and has important effects on forest structure and biomass [1,2], terrestrial carbon stocks [3,4], and ecosystem functioning [5]
We investigated the response of stand-level biomass growth to long-term drought in different regions based on a stand-total sampling strategy along a moisture gradient in the Qilian Mountains
Treesand exhibited the for the middle and western sites, respectively), and their recovery was not significant in resistance to long-term drought (−0.015) but the weakest recovery after drought any of the sites. These findings indicate a trade-off between resistance and recovery at the the eastern easternQilian site Mountains, exhibited trees the exhibited highest temporal stability to dro different sites.trees
Summary
Drought exerts a strong suppressive effect on tree growth through water deficit or carbon starvation and has important effects on forest structure and biomass [1,2], terrestrial carbon stocks [3,4], and ecosystem functioning [5]. The frequency and intensity of droughts have been altered dramatically by climate change, and their effects on tree growth are a research hotspot. Many studies have assessed the impact of drought on tree growth, identifying it as an important factor affecting the growth and death of trees [6,7,8]. The effects of single extreme droughts on tree growth have been widely studied in many parts of the world [9,10,11,12]
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