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Mountain vegetation change quantification using surface landscape metrics in Lancang watershed, China

机译:利用澜沧江流域的地表景观度量量化山地植被变化

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Land cover and vegetation change are among the most important aspects of environmental change. Vegetation change can be quantified by landscape pattern indices (LPI). Landscape indices are routinely calculated using planar land use/land cover (LU/LC) maps, obtained by the projection of a non-flat landscape surface into a two-dimensional Cartesian space. Especially in mountainous areas, quantification on planar maps can lead to underestimation of vegetation and land cover changes. Hoechstetter et al. (2008) developed a method to compute LPIs in a surface structure by calculating landscape patch surface area and surface perimeter from digital elevation models (DEM). As yet there have been no applications of these surface landscape indices on land use/land cover and vegetation change quantification. The objectives of this study are to (1) choose a LPI method (surface metrics pattern analysis or common planimetric metrics pattern analysis) for vegetation change quantification; and (2) employ the selected surface LPI method to assess vegetation pattern change in two mountainous areas of the Lancang watershed, Yunnan Province, China. The results show that the surface approach to estimate changes of class area (CA), mean patch area (MPA), and mean Euclidean Near-Neighbor distance (MENN) may obtain more accurate results for quantifying vegetation change in steep mountain areas. Forest fragmentation increased significantly over time in the two different mountainous study areas. The patches of two land cover classes, (i) agricultural land and (ii) low density forest and tall shrubs, became more aggregated in the northern (temperate) study area. In the southern (tropical) study area, rubber plantations increased considerably in size and became more aggregated.
机译:土地覆盖和植被变化是环境变化最重要的方面。植被变化可以通过景观格局指数(LPI)进行量化。通常使用平面土地利用/土地覆盖(LU / LC)图来计算景观指数,该图是通过将非平面景观表面投影到二维笛卡尔空间中而获得的。特别是在山区,对平面地图的量化可能会低估植被和土地覆盖的变化。 Hoechstetter等。 (2008年)开发了一种通过从数字高程模型(DEM)计算景观斑块的表面积和表面周长来计算表面结构中LPI的方法。迄今为止,尚未将这些地表景观指数应用于土地利用/土地覆盖和植被变化量化。这项研究的目的是(1)选择LPI方法(表面度量模式分析或普通平面度量模式分析)进行植被变化量化; (2)采用选定的地面LPI方法来评估中国云南省澜沧江流域两个山区的植被格局变化。结果表明,采用表面方法估算类别面积(CA),平均斑块面积(MPA)和平均欧几里得近邻距离(MENN)的变化可能获得更准确的结果,以量化陡峭山区的植被变化。随着时间的推移,在两个不同的山区研究区域中森林破碎化现象显着增加。在北部(温带)研究区,(i)农业用地和(ii)低密度森林和高矮灌木丛这两种土地覆盖类别的斑块变得更加聚集。在南部(热带)研究区,橡胶种植园的规模大大增加,并且变得更加聚集。

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