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Vegetation response to climatic variation and human activities on the Ordos Plateau from 2000 to 2016

机译:2000年至2016年鄂尔多斯高原植被对气候变化和人类活动的响应

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Determination and analysis of the effects of climatic variation and human activities on vegetation changes since the implementation of intensive ecological projects in 2000 are critically important for the restoration of vegetation on the Ordos Plateau, one of the areas that suffer from the worst vegetation degradation, the most concentrated coal and gas exploitation, and the highest ecological risks in China. This study was performed to establish and validate a nonlinear regression model to express the relationships between the normalized difference vegetation index (NDVI), precipitation, and air temperature in areas with scarce human activities, as identified from the Global Human Influence Index Datasets. This model was then applied to the whole plateau with data on cumulative precipitation and average air temperature with the consideration of the delayed effects to simulate temporal NDVI changes induced by climatic variation. The residual trend was then computed as the slope of the difference between the actual NDVI and the simulated value to analyze the human impact on vegetation. The results show that the plateau's vegetation had experienced a significant greening trend from 2000 to 2016 under a warmer and wetter climate and with the impact of human activities; compared to air temperature, precipitation played a leading role in vegetation greening in most parts of the plateau, and human activities had a significant positive impact in 22.0% of the plateau and a significant negative impact in 0.66% of the plateau (p < 0.1). More effective programs of ecological protection and restoration must still be conducted by the government and other organizations.
机译:自2000年实施密集的生态项目以来,确定和分析气候变化和人类活动对植被变化的影响对于恢复鄂尔多斯高原的植被至关重要。鄂尔多斯高原是遭受最严重植被退化的地区之一。中国煤炭和天然气开采最集中,生态风险最高。进行这项研究是为了建立和验证非线性回归模型,以表达人类活动稀少地区的归一化差异植被指数(NDVI),降水和气温之间的关系,这已从全球人类影响指数数据集中确定。然后将此模型应用于累积高原和平均气温的数据,并考虑到延迟效应,以模拟气候变化引起的时间NDVI变化,将其应用于整个高原。然后,将剩余趋势计算为实际NDVI与模拟值之间的差异的斜率,以分析人类对植被的影响。结果表明,在温暖湿润的气候以及人类活动的影响下,高原植被在2000年至2016年间经历了明显的绿化趋势。与气温相比,降水在高原大部分地区的植被绿化中起主要作用,人类活动对高原的22.0%具有显着的正向影响,对高原的0.66%具有显着的负向影响(p <0.1) 。政府和其他组织仍必须执行更有效的生态保护和恢复计划。

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