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Ecogeomorphic coevolution of semiarid hillslopes: emergence of banded and striped vegetation patterns through interaction of biotic and abiotic processes

机译:半干旱山坡的生态地貌共同演化:通过生物过程和非生物过程的相互作用出现带状和带状植被格局

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摘要

Nonlinear interactions between physical and biological factors give rise to the emergence of remarkable landform-vegetation patterns. Patterns of vegetation and resource redistribution are linked to productivity and carrying capacity of the land. As a consequence, growing concern over ecosystem resilience to perturbations that could lead to irreversible land degradation imposes a pressing need for understanding the processes, nonlinear interactions, and feedbacks, leading to the coevolution of these patterns. For arid and semiarid regions, causes for concern have increased at a rapid pace during the last few decades due to growing anthropic and climatic pressures that have resulted in the degradation of numerous areas worldwide. This paper aims at improving our understanding of the ecogeomorphic evolution of landscape patterns in semiarid areas with a sparse biomass cover through a modeling approach. A coupled vegetation-pattern formation and landform evolution model is used to study the coevolution of vegetation and topography over centennial timescales. Results show that self-organized vegetation patterns strongly depend on feedbacks with coevolving landforms. The resulting patterns depend on the erosion rate and mechanism (dominance of either fluvial or diffusive processes), which are affected by biotic factors. Moreover, results show that ecohydrologic processes leading to banded pattern formation, when coupled with landform processes, can also lead to completely different patterns (stripes of vegetation along drainage lines) that are equally common in semiarid areas. These findings reinforce the importance of analyzing the coevolution of landforms and vegetation to improve our understanding of the patterns and structures found in nature.
机译:物理和生物因素之间的非线性相互作用引起了显着的地貌-植被格局的出现。植被和资源再分配的模式与土地的生产力和承载能力有关。结果,人们越来越关注生态系统对扰动的适应能力,这种干扰可能导致土地不可逆转的退化,因此迫切需要了解过程,非线性相互作用和反馈,从而导致这些模式的共同发展。在干旱和半干旱地区,由于日益增加的人类和气候压力导致全世界许多地区的退化,在过去几十年中,引起关注的原因迅速增加。本文旨在通过建模方法,提高对稀疏生物量覆盖的半干旱地区景观格局生态地貌演变的理解。耦合的植被格局形成和地貌演化模型用于研究百年时间尺度上植被和地形的协同演化。结果表明,自组织的植被格局在很大程度上取决于具有共同演化地貌的反馈。所产生的模式取决于受生物因素影响的侵蚀速率和机理(河流或扩散过程的主导)。此外,结果表明,导致带状格局形成的生态水文过程,与地形过程相结合,也可能导致完全不同的格局(沿排水线的植被条纹),在半干旱地区同样普遍。这些发现加强了分析地貌和植被共同进化的重要性,以增进我们对自然界中的格局和结构的理解。

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