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Pervasive drought legacies in forest ecosystems and their implications for carbon cycle models

机译:森林生态系统普遍存在的干旱遗产及其对碳循环模型的影响

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摘要

The impacts of climate extremes on terrestrial ecosystems are poorly understood but important for predicting carbon cycle feedbacks to climate change. Coupled climate-carbon cycle models typically assume that vegetation recovery from extreme drought is immediate and complete, which conflicts with the understanding of basic plant physiology. We examined the recovery of stem growth in trees after severe drought at 1338 forest sites across the globe, comprising 49,339 site-years, and compared the results with simulated recovery in climate-vegetation models.We found pervasive and substantial >legacy effects> of reduced growth and incomplete recovery for 1 to 4 years after severe drought. Legacy effects were most prevalent in dry ecosystems, among Pinaceae, and among species with low hydraulic safety margins. In contrast, limited or no legacy effects after drought were simulated by current climate-vegetation models. Our results highlight hysteresis in ecosystem-level carbon cycling and delayed recovery from climate extremes.
机译:人们很少了解极端气候对陆地生态系统的影响,但对于预测碳循环对气候变化的反馈至关重要。耦合的气候-碳循环模型通常假定从极端干旱中恢复植被是即时且完整的,这与对基本植物生理学的理解相矛盾。我们检查了全球1338个森林站点(包括49339个站点-年)遭受严重干旱后树木茎秆生长的恢复情况,并将结果与​​气候-植被模型中的模拟恢复结果进行了比较。严重干旱后1至4年生长和恢复不完全。在干旱生态系统,松科和水力安全系数低的物种中,遗留效应最为普遍。相反,目前的气候-植被模型模拟了干旱后有限或没有遗留影响。我们的结果突出了生态系统级碳循环的滞后现象以及从极端气候中恢复的延迟。

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