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Drought and Carbon Cycling of Grassland Ecosystems under Global Change: A Review

机译:全球变化下的草地生态系统干旱与碳循环研究进展

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In recent years, the increased intensity and duration of droughts have dramatically altered the structure and function of grassland ecosystems, which have been forced to adapt to this change in climate. Combinations of global change drivers such as elevated atmospheric CO 2 concentration, warming, nitrogen ( N ) deposition, grazing, and land-use change have influenced the impact that droughts have on grassland C cycling. This influence, to some extent, can modify the relationship between droughts and grassland carbon ( C ) cycling in the multi-factor world. Unfortunately, prior reviews have been primarily anecdotal from the 1930s to the 2010s. We investigated the current state of the study on the interactive impacts of multiple factors under drought scenarios in grassland C cycling and provided scientific advice for dealing with droughts and managing grassland C cycling in a multi-factor world. Currently, adequate information is not available on the interaction between droughts and global change drivers, which would advance our understanding of grassland C cycling responses. It was determined that future experiments and models should specifically test how droughts regulate grassland C cycling under global changes. Previous multi-factor experiments of current and future global change conditions have studied various drought scenarios poorly, including changes in precipitation frequency and amplitude, timing, and interactions with other global change drivers. Multi-factor experiments have contributed to quantifying these potential changes and have provided important information on how water affects ecosystem processes under global change. There is an urgent need to establish a systematic framework that can assess ecosystem dynamic responses to droughts under current and future global change and human activity, with a focus on the combined effects of droughts, global change drivers, and the corresponding hierarchical responses of an ecosystem.
机译:近年来,干旱的加剧和持续时间的增加大大改变了草原生态系统的结构和功能,迫使它们适应这种气候变化。全球变化驱动因素的组合,例如大气中CO 2浓度升高,变暖,氮(N)沉积,放牧和土地利用变化,都影响了干旱对草原碳循环的影响。这种影响在一定程度上可以改变干旱与多因素世界中草地碳(C)循环之间的关系。不幸的是,从1930年代到2010年代,以前的评论主要是轶事。我们调查了干旱条件下草地C循环中多种因素相互作用的研究现状,并为应对干旱和管理多因素世界中的草地C循环提供了科学建议。当前,关于干旱与全球变化驱动因素之间的相互作用尚无足够的信息,这将加深我们对草地碳循环响应的理解。确定未来的实验和模型应专门测试干旱如何调节全球变化下的草地碳循环。先前对当前和将来的全球变化条件进行的多因素实验对各种干旱情景的研究较差,包括降水频率和振幅,时间的变化以及与其他全球变化驱动因素的相互作用。多因素实验有助于量化这些潜在变化,并提供了有关水如何影响全球变化下的生态系统过程的重要信息。迫切需要建立一个系统的框架,以评估当前和未来全球变化和人类活动下生态系统对干旱的动态响应,重点是干旱,全球变化驱动因素和生态系统相应的分层响应的综合影响。

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