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Exposure of trees to drought-induced die-off is defined by a common climatic threshold across different vegetation types

机译:树木因干旱而死亡的风险是由不同植被类型的共同气候阈值确定的

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摘要

Increases in drought and temperature stress in forest and woodland ecosystems are thought to be responsible for the rise in episodic mortality events observed globally. However, key climatic drivers common to mortality events and the impacts of future extreme droughts on tree survival have not been evaluated. Here, we characterize climatic drivers associated with documented tree die-off events across Australia using standardized climatic indices to represent the key dimensions of drought stress for a range of vegetation types. We identify a common probabilistic threshold associated with an increased risk of die-off across all the sites that we examined. We show that observed die-off events occur when water deficits and maximum temperatures are high and exist outside 98% of the observed range in drought intensity; this threshold was evident at all sites regardless of vegetation type and climate. The observed die-off events also coincided with at least one heat wave (three consecutive days above the 90th percentile for maximum temperature), emphasizing a pivotal role of heat stress in amplifying tree die-off and mortality processes. The joint drought intensity and maximum temperature distributions were modeled for each site to describe the co-occurrence of both hot and dry conditions and evaluate future shifts in climatic thresholds associated with the die-off events. Under a relatively dry and moderate warming scenario, the frequency of droughts capable of inducing significant tree die-off across Australia could increase from 1 in 24 years to 1 in 15 years by 2050, accompanied by a doubling in the occurrence of associated heat waves. By defining commonalities in drought conditions capable of inducing tree die-off, we show a strong interactive effect of water and high temperature stress and provide a consistent approach for assessing changes in the exposure of ecosystems to extreme drought events.
机译:人们认为,森林和林地生态系统中干旱和温度胁迫的增加是全球观察到的突发性死亡事件增加的原因。但是,尚未评估死亡事件共有的关键气候驱动因素以及未来极端干旱对树木生存的影响。在这里,我们使用标准化的气候指数来表征澳大利亚各地与文献记载的树木死亡事件相关的气候驱动因素,以代表一系列植被类型的干旱胁迫的关键尺度。我们确定了一个共同的概率阈值,该阈值与我们检查的所有站点中的死亡风险均增加相关。我们发现,当水分亏缺和最高温度很高并且出现在干旱强度所观测范围的98%之外时,就会发生死亡现象。无论植被类型和气候如何,该阈值在所有地点都很明显。观察到的死亡事件还与至少一个热浪同时发生(最高温度超过90%的连续三天),强调了热应激在扩大树木死亡和死亡过程中的关键作用。对每个地点的联合干旱强度和最高温度分布进行建模,以描述炎热和干旱条件的共同发生,并评估与死亡事件相关的气候阈值的未来变化。在相对干燥和中度变暖的情况下,到2050年,能够在澳大利亚引起重大树木死亡的干旱频率可能从24年中的1年增加到15年中的1年,并伴随着相关热浪的发生增加一倍。通过定义能够诱发树木死亡的干旱条件下的共性,我们展示了水与高温胁迫的强烈相互作用,并提供了一致的方法来评估生态系统暴露于极端干旱事件中的变化。

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