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Rainfall intensity switches ecohydrological runoff/runon redistribution patterns in dryland vegetation patches

机译:降雨强度改变了旱地植被斑块的生态水文径流/径流再分配模式

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摘要

Effectively managing net primary productivity in drylands for grazing and other uses depends on understanding how limited rainfall input is redistributed by runoff and runon among vegetation patches, particularly for patches that contrast between lesser and greater amounts of vegetation cover. Due in part to data limitations, ecohydrologists generally have focused on rainfall event size to characterize water redistribution processes. Here we use soil moisture data from a semiarid woodland to highlight how, when event size is controlled and runoff and interception are negligible at the stand scale, rainfall intensity drives the relationship between water redistribution and canopy and soil patch attributes. Horizontal water redistribution variability increased with rainfall intensity and differed between patches with contrasting vegetation cover. Sparsely vegetated patches gained relatively more water during lower intensity events, whereas densely vegetated ones gained relatively more water during higher intensity events. Consequently, range managers need to account for the distribution of rainfall event intensity, as well as event size, to assess the consequences of climate variability and change on net primary productivity. More generally; our results suggest that rainfall intensity needs to be considered in addition to event size to understand vegetation patch dynamics in drylands.
机译:有效管理旱地放牧和其他用途的净初级生产力取决于了解植被斑块中径流和径流如何重新分配有限的降雨输入,尤其是对于植被覆盖量较少和较大的斑块而言。部分由于数据限制,生态水文学家通常将注意力集中在降雨事件的大小上,以表征水的重新分配过程。在这里,我们使用半干旱林地的土壤湿度数据来突出显示,当控制事件大小并且在林分尺度上径流和截距可忽略不计时,降雨强度驱动着水的重新分配与冠层和土壤斑块属性之间的关系。水平的水再分配变异性随降雨强度的增加而增加,并且在不同植被覆盖的斑块之间有所不同。植被稀疏的补丁在强度较低的事件中获得相对更多的水分,而植被茂密的补丁在强度较高的事件中获得相对更多的水分。因此,范围管理员需要考虑降雨事件强度的分布以及事件规模,以评估气候变化和变化对净初级生产力的影响。更普遍;我们的结果表明,除了事件大小以外,还需要考虑降雨强度,以了解干旱地区的植被斑块动态。

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