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王鑫, 薛飞阳, 苏子昕, 等. 基于MODIS-NDVI的岷江流域植被时空演变及地形分异研究[J]. 四川林业科技, 2024, 45(1): 33−40. DOI: 10.12172/202306020001
引用本文: 王鑫, 薛飞阳, 苏子昕, 等. 基于MODIS-NDVI的岷江流域植被时空演变及地形分异研究[J]. 四川林业科技, 2024, 45(1): 33−40. DOI: 10.12172/202306020001
WANG X, XUE F Y, SU Z X, et al. Spatial and temporal evolution of vegetation and topographic differentiation in Minjiang River basin based on MODIS-NDVI[J]. Journal of Sichuan Forestry Science and Technology, 2024, 45(1): 33−40. DOI: 10.12172/202306020001
Citation: WANG X, XUE F Y, SU Z X, et al. Spatial and temporal evolution of vegetation and topographic differentiation in Minjiang River basin based on MODIS-NDVI[J]. Journal of Sichuan Forestry Science and Technology, 2024, 45(1): 33−40. DOI: 10.12172/202306020001

基于MODIS-NDVI的岷江流域植被时空演变及地形分异研究

Spatial and temporal evolution of vegetation and topographic differentiation in Minjiang River basin based on MODIS-NDVI

  • 摘要: 岷江是长江水系的重要分支之一,流经川西高原以及四川盆地地区。植被作为重要的生态指标之一,通过研究岷江流域的植被时空变化特征将有助于了解该流域的生态环境情况并为后续的生态治理提供参考依据。基于2003年~2021年岷江流域的MODIS-NDVI数据集以及DEM数据,借助于空间分析技术、Hurst指数、线性趋势分析、变异系数等方法多方面分析了岷江流域植被覆盖的时空演变特征以及地形因子对其变化趋势的影响性。结果表明:(1)研究时段内的NDVI均值介于0~0.9之间。其流域的NDVI值上中游偏高,下游偏低,岷江流域植被整体呈现波动上升的趋势,增长速率为2.4%/10a。(2)岷江流域植被覆盖呈增加趋势和减少趋势的面积分别占84.49%和15.51%。川西高原的河谷地区以及四川盆地的非城镇区域呈现显著增长趋势。呈减少趋势的主要分布在成都市向外扩张的新城区、眉山市和德阳市。(3)波动性较强的区域主要分布在川西高原的高海拔山地以及成都市,而低波动主要出现在川西高原的相对低海拔区域,植被较为稳定。(4)植被未来变化趋势呈现持续性减少的主要是成都市向外扩张的新城区。而呈现持续性增加的主要分布在四川盆地的非城镇地区以及川西高原的河谷地区。(5)海拔和坡度作为影响植被变化的主要因素,坡向与植被变化的相关性并未显示出明显的规律。

     

    Abstract: Minjiang River is one of the important branches of the Yangtze River system, which flows through the western Sichuan Plateau and the Sichuan Basin. As one of the important ecological indicators, studying the spatial and temporal variation of vegetation in Minjiang River basin will help to understand the ecological environment of the basin and provide reference for subsequent ecological management. Based on the MODIS-NDVI dataset and DEM data of Minjiang River basin from 2003 to 2021, the spatial and temporal evolution of vegetation cover in the Minjiang River basin and the influence of topographic factors on its change trend by means of spatial analysis techniques, Hurst index, linear trend analysis and coefficient of variation were analyzed. The results showed that: (1) The average NDVI value ranged from 0 to 0.9 during the study period. The NDVI value in the upper and middle reaches of the river basin were higher than that in the lower reaches, and the overall vegetation cover of the Minjiang River basin showed a fluctuating upward trend with a growth rate of 2.4%/10 a. (2) The areas with increasing and decreasing vegetation cover in the Minjiang River basin accounted for 84.49% and 15.51%, respectively. The valley areas of the western Sichuan Plateau and the non-urban areas of the Sichuan basin showed a significant increasing trend. Those with decreasing trends were mainly located in the new urban areas of Chengdu city expanding outward, Meishan city and Deyang city. (3) The areas with high volatility were mainly distributed in the high-elevation mountains of the western Sichuan Plateau and in Chengdu city, while low volatility mainly occured in the relatively low-elevation areas of the western Sichuan Plateau, where the vegetation was more stable. (4) Future changes in vegetation cover showed a continuous decrease mainly in the new urban areas of Chengdu city, which were expanding outward. Those with persistent increases were mainly in the non-urban areas of the Sichuan basin and the river valley areas of the western Sichuan Plateau. (5) Elevation and slope were the main factors affecting vegetation change, and the correlation between slope direction and vegetation change did not show a clear pattern.

     

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