珠江流域贵州段地形特征及其对植被覆盖度空间分布的影响研究

Topographic Characteristics and Their Influence on the Spatial Distribution of Fractional Vegetation Cover in the Guizhou Section of the Pearl River Basin

  • 摘要: 作为珠江上游重要的生态屏障,贵州省显著的山地地形特征与生态环境对流域生态安全具有关键作用。本文基于12.5 m分辨率DEM数据提取地形因子,结合GF-6高分辨率遥感影像,采用像元二分法反演植被覆盖度(Fractional Vegetation Cover,FVC),系统量化了珠江流域贵州段植被覆盖与地形因子的空间耦合关系。结果表明:(1)地形空间分异特征显著,整体呈现西北高、东南低的地势格局,坡度由中心向外围递增,主导坡向为北坡、西北坡、南坡和东南坡,地形起伏度表现为"U"型的空间分布模式;(2)FVC空间异质性凸显,高植被覆盖等级占研究区总面积的45.66%,其中2000~3000 m海拔带高覆盖度面积比例超50%,主要分布于陡坡(15°~<20°)、急坡(20°~<25°)及中等地形起伏度(300~900 m)区域;(3)地形因子对FVC的解释力依次为坡度(q=0.0342)>海拔(q=0.0071)>地形起伏度(q=0.0058)>坡向(q=0.0014),各因子交互作用均表现为非线性增强。

     

    Abstract: As a critical ecological barrier in the upper reaches of the Pearl River, Guizhou Province has distinctive mountainous topographic features and ecological environments, both of which play a vital role in sustaining the ecological security of the river basin. This study derived topographic factors from 12.5 m resolution DEM data, combined GF-6 high-resolution remote sensing images with the pixel dichotomy model to retrieve fractional vegetation cover (FVC), and systematically quantified the spatial coupling relationship between FVC and topographic factors in the Guizhou section of the Pearl River Basin. The results indicate that: (1) The terrain features showed remarkable spatial differentiation, with an overall terrain pattern of high northwest and low southeast. Slope gradient increased gradually from the central region to the periphery zones, and the dominant slope aspects were north, northwest, south, and southeast. Terrain relief exhibited a U-shaped spatial distribution pattern. (2) FVC displayed notable spatial heterogeneity, and high-FVC zones accounted for 45.66% of the total study area. The proportion of high-FVC areas exceeded 50% within the elevation zone of 2000–3000 m, which were mainly distributed on steep slopes (15°~<20°), abrupt slopes (20°~<25°) and areas with moderate terrain relief (300~900 m). (3) The explanatory power of topographic factors for FVC followed the order: slope (q=0.0342) > elevation (q=0.0071) > terrain relief (q=0.0058) >slope aspect (q=0.0014). All pairwise interactions between factors exhibited nonlinear enhancement effects.

     

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