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并非所有干旱都是一样的:年际干旱模式和强度对草地碳循环的影响。

Not all droughts are created equal: the impacts of interannual drought pattern and magnitude on grassland carbon cycling.

作者信息

Hoover David L, Rogers Brendan M

机构信息

US Geological Survey, Southwest Biological Center, 2290 SW Resource Blvd., Moab, UT, USA.

Woods Hole Research Center, 149 Woods Hole Road, Falmouth, MA, USA.

出版信息

Glob Chang Biol. 2016 May;22(5):1809-20. doi: 10.1111/gcb.13161. Epub 2016 Feb 25.

Abstract

Climate extremes, such as drought, may have immediate and potentially prolonged effects on carbon cycling. Grasslands store approximately one-third of all terrestrial carbon and may become carbon sources during droughts. However, the magnitude and duration of drought-induced disruptions to the carbon cycle, as well as the mechanisms responsible, remain poorly understood. Over the next century, global climate models predict an increase in two types of drought: chronic but subtle 'press-droughts', and shorter term but extreme 'pulse-droughts'. Much of our current understanding of the ecological impacts of drought comes from experimental rainfall manipulations. These studies have been highly valuable, but are often short term and rarely quantify carbon feedbacks. To address this knowledge gap, we used the Community Land Model 4.0 to examine the individual and interactive effects of pulse- and press-droughts on carbon cycling in a mesic grassland of the US Great Plains. A series of modeling experiments were imposed by varying drought magnitude (precipitation amount) and interannual pattern (press- vs. pulse-droughts) to examine the effects on carbon storage and cycling at annual to century timescales. We present three main findings. First, a single-year pulse-drought had immediate and prolonged effects on carbon storage due to differential sensitivities of ecosystem respiration and gross primary production. Second, short-term pulse-droughts caused greater carbon loss than chronic press-droughts when total precipitation reductions over a 20-year period were equivalent. Third, combining pulse- and press-droughts had intermediate effects on carbon loss compared to the independent drought types, except at high drought levels. Overall, these results suggest that interannual drought pattern may be as important for carbon dynamics as drought magnitude and that extreme droughts may have long-lasting carbon feedbacks in grassland ecosystems.

摘要

极端气候,如干旱,可能对碳循环产生直接且可能持续较长时间的影响。草原储存了大约三分之一的陆地碳,在干旱期间可能会成为碳源。然而,干旱对碳循环造成干扰的程度和持续时间,以及其背后的机制,仍鲜为人知。在接下来的一个世纪里,全球气候模型预测两种干旱类型将会增加:长期但不明显的“持续干旱”,以及短期但极端的“脉冲干旱”。我们目前对干旱生态影响的大部分认识来自于实验性降雨控制。这些研究非常有价值,但往往是短期的,而且很少量化碳反馈。为了填补这一知识空白,我们使用了社区土地模型4.0来研究脉冲干旱和持续干旱对美国大平原中部草原碳循环的单独和交互影响。通过改变干旱程度(降水量)和年际模式(持续干旱与脉冲干旱)进行了一系列模拟实验,以研究在年度到世纪时间尺度上对碳储存和循环的影响。我们呈现了三个主要发现。第一,由于生态系统呼吸和总初级生产的敏感性不同,单一年度的脉冲干旱对碳储存有直接且持久的影响。第二,当20年期间的总降水量减少量相当时,短期脉冲干旱比长期持续干旱导致的碳损失更大。第三,与单独的干旱类型相比,脉冲干旱和持续干旱相结合对碳损失有中间影响,但在高干旱水平下除外。总体而言,这些结果表明年际干旱模式对碳动态的重要性可能与干旱程度相当,并且极端干旱可能在草原生态系统中产生持久 的碳反馈。

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