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树木因干旱而死亡的暴露程度是由不同植被类型共有的气候阈值来定义的。

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

机构信息

CSIRO Ecosystem Sciences and Climate Adaptation Flagship College Rd, Sandy Bay, TAS, Australia.

CSIRO Computational Informatics, Castray Esplanade Hobart, TAS, Australia.

出版信息

Ecol Evol. 2014 Apr;4(7):1088-101. doi: 10.1002/ece3.1008. Epub 2014 Mar 6.

Abstract

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.

摘要

森林和林地生态系统中的干旱和温度压力增加被认为是导致全球范围内间歇性死亡事件增加的原因。然而,与死亡率事件共同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尚未得到评估。在这里,我们使用标准化气候指数来描述澳大利亚各地有记录的树木死亡事件的气候驱动因素,这些指数代表了各种植被类型干旱压力的关键维度。我们确定了一个与所有研究地点的死亡风险增加相关的共同概率阈值。我们表明,当水分亏缺和最高温度较高时,就会发生观测到的树木死亡事件,而且这种情况超出了干旱强度观测范围的 98%;无论植被类型和气候如何,这个阈值在所有地点都很明显。观察到的死亡事件也与至少一次热浪(连续三天最高温度超过第 90 个百分位数)同时发生,这强调了热应力在放大树木死亡和死亡过程中的关键作用。为了描述炎热和干燥条件的同时发生情况,并评估与死亡事件相关的未来气候阈值变化,我们对每个地点的干旱强度和最高温度分布进行了建模。在相对干燥和中度变暖的情景下,澳大利亚发生严重树木死亡的干旱频率可能会从每 24 年一次增加到每 15 年一次,而相关热浪的发生频率也会增加一倍。通过定义能够导致树木死亡的干旱条件的共性,我们展示了水和高温压力的强烈相互作用,并提供了一种评估生态系统暴露于极端干旱事件的变化的一致方法。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e328/3997324/2577c0afe755/ece30004-1088-f1.jpg

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