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Effect of interannual precipitation variability on dryland productivity: A global synthesis

机译:互连降水变异对旱地生产率的影响:全球合成

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Climate-change assessments project increasing precipitation variability through increased frequency of extreme events. However, the effects of interannual precipitation variance per se on ecosystem functioning have been largely understudied. Here, we report on the effects of interannual precipitation variability on the primary production of global drylands, which include deserts, steppes, shrublands, grasslands, and prairies and cover about 40% of the terrestrial earth surface. We used a global database that has 43 datasets, which are uniformly distributed in parameter space and each has at least 10 years of data. We found (a) that at the global scale, precipitation variability has a negative effect on aboveground net primary production. (b) Expected increases in interannual precipitation variability for the year 2,100 may result in a decrease of up to 12% of the global terrestrial carbon sink. (c) The effect of precipitation interannual variability on dryland productivity changes from positive to negative along a precipitation gradient. Arid sites with mean precipitation under 300 mm/year responded positively to increases in precipitation variability, whereas sites with mean precipitation over 300 mm/year responded negatively. We propose three complementary mechanisms to explain this result: (a) concave-up and concave-down precipitation-production relationships in arid vs. humid systems, (b) shift in the distribution of water in the soil profile, and (c) altered frequency of positive and negative legacies. Our results demonstrated that enhanced precipitation variability will have direct impacts on global drylands that can potentially affect the future terrestrial carbon sink.
机译:气候变化评估通过增加极端事件的频率提高降水变量。然而,在很大程度上被认为,本身对生态系统功能的依赖降水方差的影响已经大大。在这里,我们报告了持续降水变量对全球旱地主要生产的影响,包括沙漠,草原,灌木丛,草原和大草原,覆盖大约40%的陆地地面。我们使用了一个具有43个数据集的全局数据库,它均匀地分布在参数空间中,每个数据集都有至少10年的数据。我们发现(a)在全球范围内,降水可变性对地上净初级生产具有负面影响。 (b)预计2,100年持续降水变量的预期增加可能导致全球陆地碳汇的达到最多12%。 (c)降水续变性对旱地生产率的效果从沉淀梯度阳性变为负。在300毫米/年下的平均沉淀的干旱部位积极响应降水变异性,而具有超过300mm /年的平均沉淀的位点负面反应。我们提出了三种互补机制来解释这一结果:(a)干旱与湿度系统中的凹陷和凹陷的降水 - 生产关系,(b)在土壤轮廓中的水分布,(c)改变积极和负面遗产的频率。我们的结果表明,增强的降水可变性将对可能影响未来陆地碳汇的全球旱地产生直接影响。

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