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首页> 外文期刊>Remote Sensing >Effects of Precipitation Intensity and Temperature on NDVI-Based Grass Change over Northern China during the Period from 1982 to 2011
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Effects of Precipitation Intensity and Temperature on NDVI-Based Grass Change over Northern China during the Period from 1982 to 2011

机译:1982-2011年降水强度和温度对中国北方基于NDVI的草地变化的影响

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摘要

The knowledge about impacts of changes in precipitation regimes on terrestrial ecosystems is fundamental to improve our understanding of global environment change, particularly in the context that heavy precipitation is expected to increase according to the 5th Intergovernmental Panel on Climate Change (IPCC) assessment. Based on observed climate data and the Advanced Very High Resolution Radiometer (AVHRR) Global Inventory Modeling and Mapping Studies (GIMMS) satellite-derived normalized difference vegetation index (NDVI), here we analyzed the spatio-temporal changes in grassland NDVI, covering 1.64 × 106 km2, in northern China and their linkages to changes in precipitation and temperature during the period 1982–2011. We found that mean growing season (April–October) grass NDVI is more sensitive to heavy precipitation than to moderate or light precipitation in both relatively arid areas (RAA) and relatively humid areas (RHA), whereas the sensitivities of grass NDVI to temperature are comparable to total precipitation in RHA. Heavy precipitation showed the strongest impacts in more than half of northern China (56%), whereas impacts of light precipitation on grass NDVI were stronger in some areas (21%), mainly distributed in northwestern China, a typical arid and semi-arid area. Our findings suggest that responses of grasslands are divergent with respect to changes in precipitation intensities.
机译:了解降水状况变化对陆地生态系统的影响,对于增进我们对全球环境变化的理解至关重要,尤其是根据第五届政府间气候变化专门委员会(IPCC)的评估,预计大雨将增加。基于观测到的气候数据和先进的超高分辨率辐射计(AVHRR)全球清单建模与制图研究(GIMMS)卫星衍生的归一化差异植被指数(NDVI),我们在此分析了草地NDVI的时空变化,覆盖1.64× 1982-2011年期间,中国北部10 6 km 2 及其与降水和温度变化的联系。我们发现,相对干旱地区(RAA)和相对潮湿地区(RHA)的平均生长期(4月至10月)草NDVI对中等降水量或轻度降水更为敏感,而草NDVI对温度的敏感性为与RHA中的总降水量相当。强降水在华北一半以上地区(56%)表现出最强烈的影响,而轻降水对草地NDVI的影响在某些地区(21%)较强,主要分布在中国西北部,一个典型的干旱和半干旱地区。我们的发现表明,草原对降水强度变化的反应是不同的。

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