Spatial scale effects of water erosion dynamics: Complexities, variabilities, and uncertainties

被引:32
作者
Wei Wei [1 ]
Chen Liding [1 ]
Yang Lei [1 ]
Fu Bojie [1 ]
Sun Ranhao [1 ]
机构
[1] Chinese Acad Sci, State Key Lab Urban & Reg Ecol, Res Ctr Ecoenvironm Sci, Beijing 100085, Peoples R China
基金
中国国家自然科学基金;
关键词
water erosion; spatial variation; scale effect; driving force; uncertainty; complexity; ROCK FRAGMENT COVER; SOIL-EROSION; SEDIMENT YIELD; REGIONAL SCALES; LAND-USE; TERRESTRIAL ECOSYSTEMS; CARBON SEQUESTRATION; EXPERIMENTAL AREA; CLIMATE-CHANGE; RUNOFF;
D O I
10.1007/s11769-012-0524-2
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Severe water erosion is notorious for its harmful effects on land-water resources as well as local societies. The scale effects of water erosion, however, greatly exacerbate the difficulties of accurate erosion evaluation and hazard control in the real world. Analyzing the related scale issues is thus urgent for a better understanding of erosion variations as well as reducing such erosion. In this review article, water erosion dynamics across three spatial scales including plot, watershed, and regional scales were selected and discussed. For the study purposes and objectives, the advantages and disadvantages of these scales all demonstrate clear spatial-scale dependence. Plot scale studies are primarily focused on abundant data collection and mechanism discrimination of erosion generation, while watershed scale studies provide valuable information for watershed management and hazard control as well as the development of quantitatively distributed models. Regional studies concentrate more on large-scale erosion assessment, and serve policymakers and stakeholders in achieving the basis for regulatory policy for comprehensive land uses. The results of this study show that the driving forces and mechanisms of water erosion variations among the scales are quite different. As a result, several major aspects contributing to variations in water erosion across the scales are stressed: differences in the methodologies across various scales, different sink-source roles on water erosion processes, and diverse climatic zones and morphological regions. This variability becomes more complex in the context of accelerated global change. The changing climatic factors and earth surface features are considered the fourth key reason responsible for the increased variability of water erosion across spatial scales.
引用
收藏
页码:127 / 143
页数:17
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