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首页> 外文期刊>Water resources research >An ecohydrological approach to predicting hillslope-scale vegetation patterns in dryland ecosystems
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An ecohydrological approach to predicting hillslope-scale vegetation patterns in dryland ecosystems

机译:预测旱地生态系统中坡面植被格局的生态水文学方法

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摘要

Drylands are an important ecosystem, as they cover over 40% of the Earth's land surface and are believed to be sensitive to climate change. Where dryland vegetation supports pastoralist livestock production, catastrophic ecological shifts present a grave concern because of the direct coupling between the quality of available forage and human livelihoods. In this research we investigate the organization of vegetation on hillslopes by developing a relatively simple spatially explicit daily stochastic ecohydrological model. Using a 2 year observational study in central Kenya, we present an empirical patch water balance of three representative patch types, bare soil, grass, and tree. Given the recent expansion of bare areas, the system is dominated by Hortonian runoff and overland flow. By incorporating concepts of simple local interactions from complex systems we are able to simulate a range of surface flowpath convergence states across the hillslope during a rain event. The model also allows the root to canopy radius of the tree patches to vary affecting the length scale of water competition. By changing the length scales of facilitation and competition, the model demonstrates a range of most efficient hillslope water-use patterns from random to highly organized static vegetation patterns. The findings of this work support the mechanism of symmetry-breaking instabilities for pattern formation in drylands.
机译:干旱地区是重要的生态系统,因为它们覆盖了地球40%以上的陆地表面,并且据信对气候变化敏感。在旱地植被支持牧民畜牧生产的地方,由于可用牧草质量与人类生计之间存在直接联系,灾难性的生态变化引起了人们的严重关切。在这项研究中,我们通过开发相对简单的空间明晰的每日随机生态水文模型,研究了山坡上的植被组织。通过在肯尼亚中部进行的为期2年的观察研究,我们提出了三种代表性斑块类型(裸露的土壤,草和树)的经验斑块水平衡。考虑到最近裸露面积的扩大,该系统以霍顿径流和陆上水流为主。通过结合来自复杂系统的简单局部相互作用的概念,我们能够模拟降雨事件期间整个山坡上的一系列表面流径收敛状态。该模型还允许树木斑块的根部到冠层半径发生变化,从而影响水竞争的长度尺度。通过改变促进和竞争的规模,该模型展示了一系列最有效的山坡用水模式,从随机到高度组织化的静态植被模式。这项工作的发现支持干旱地区格局形成的对称性破坏不稳定性机制。

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  • 来源
    《Water resources research 》 |2012年第1期| p.W01515.1-W01515.18| 共18页
  • 作者单位

    Department of Hydrology and Water Resources, University of Arizona, 1133 E James E Rogers Way, Room 122, Tucson, AZ 85721,USA;

    Department of Civil and Environmental Engineering, Princeton University, E205 Engineering Quad, Princeton, NJ 08544, USA;

    Department of Ecology and Evolutionary Biology, Princeton University, 106 Guyot Hall, Princeton, NJ 08544, USA;

    Department of Civil and Environmental Engineering, Princeton University, E205 Engineering Quad, Princeton, NJ 08544, USA;

    Department of Civil and Environmental Engineering, Princeton University, E205 Engineering Quad, Princeton, NJ 08544, USA;

    Department of Civil and Environmental Engineering, Princeton University, E205 Engineering Quad, Princeton, NJ 08544, USA;

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