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Multi-scale controls on and consequences of aeolian processes in landscape change in arid and semi-arid environments

机译:干旱和半干旱环境中风沙过程在景观变化中的多尺度控制和后果

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Aeolian processes are tightly linked to soil and vegetation change in arid and semi-arid systems at multiple spatial and temporal scales. Wind influences patterns of vegetation and soil within the landscape, and these patterns control wind erosion at patch to landscape scales. Aggregated at larger scales, patterns in soil and vegetation distributions influence global distributions of dust and its biogeochemical impacts. Understanding the controls on aeolian processes is therefore important not only in understanding the biogeochemistry and land cover patterns in dryland environments, but also in understanding global land cover, climate, and biogeochemistry. Although the microscopic physics that control aeolian processes are well understood, the controls on these processes in real landscapes are poorly constrained, particularly for structurally complex plant communities such as shrub-invaded grasslands. This paper reviews the controls on aeolian processes and their consequences at plant-interspace, patch-landscape, and regional-global scales. Based on this review, we define the requirements for a cross-scale model of wind erosion in structurally complex arid and semi-arid ecosystems.
机译:风沙过程与干旱和半干旱系统在多个时空尺度上的土壤和植被变化紧密相关。风影响景观中植被和土壤的模式,这些模式控制着风蚀对景观尺度的影响。土壤和植被分布的模式在更大范围内聚集,影响着尘埃的全球分布及其生物地球化学影响。因此,了解风成过程的控制方法不仅对了解干旱地区环境中的生物地球化学和土地覆盖格局非常重要,而且对理解全球土地覆盖,气候和生物地球化学也很重要。尽管控制风沙过程的微观物理学已广为人知,但在实际景观中对这些过程的控制却受到了严格的限制,特别是对于结构复杂的植物群落(例如灌木丛生的草原)而言。本文回顾了对风沙过程的控制及其在植物间距,斑块景观和区域全球范围内的后果。在此基础上,我们定义了结构复杂的干旱和半干旱生态系统中风蚀跨尺度模型的要求。

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