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首页> 外文期刊>Plant and Soil >Spatiotemporal variability of grassland vegetation cover in a catchment in Inner Mongolia, China, derived from MODIS data products
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Spatiotemporal variability of grassland vegetation cover in a catchment in Inner Mongolia, China, derived from MODIS data products

机译:基于MODIS数据产品的中国内蒙古流域草地植被覆盖时空变异。

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摘要

Conditions, distribution and development of vegetation in semi arid regions are highly variable. In this study we detected the temporal and spatial variability of vegetation in the Xilin river catchment from 2000 to 2008 by analysis of Moderate Resolution Imaging Spectroradiometer (MODIS) data products of that period. The study is based on LAI (Leaf area index) and supported by NDVI (Normalized difference vegetation index) and LST (Land surface temperature) data with a spatial resolution of 1km. The mean LAI of the catchment from 2000 to 2008 is 0.59. Precipitation data of the study period governs the conditions and distribution of vegetation in the catchment. In dry years, e.g. 2001 and 2005, LAI was clearly lower (0.52) compared to 2003 (LAI=0.72) which was a wet year. As precipitation generally decreases from south-east to north-west, LAI values decrease according to this gradient. The influence of heavy grazing in the vicinity of the Xilin river is obvious as LAI is low (0.4) in these areas. The high temporal variability of the LAI is displayed by its high mean CV (coefficient of variation) which is 48% for the observed years. The analysis of sample areas illustrates temporal and spatial differences in vegetation development within the catchment and shows a generally delayed growth start in the north-west of the catchment.
机译:半干旱地区植被的条件,分布和发育变化很大。在这项研究中,我们通过分析那个时期的中分辨率成像光谱仪(MODIS)数据产品,检测了2000年至2008年锡林河流域植被的时空变化。这项研究基于LAI(叶面积指数),并得到NDVI(归一化植被指数)和LST(土地表面温度)数据的支持,其空间分辨率为1km。从2000年到2008年,流域的平均LAI为0.59。研究期的降水数据决定着流域植被的状况和分布。在干旱的年份,例如2001和2005年的LAI明显低于雨季的2003年(LAI = 0.72)(0.52)。由于降水量通常从东南向西北减少,因此LAI值会根据此梯度降低。由于这些地区的LAI较低(0.4),因此在锡林河附近的重度放牧影响很明显。 LAI的高时间变异性由其较高的平均CV(变异系数)显示,在所观察的年份为48%。对样本区域的分析说明了流域内植被发展的时间和空间差异,并显示了在流域西北方向普遍开始延迟的生长。

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