首页> 外文期刊>International journal of applied earth observation and geoinformation >High positive correlation between soil temperature and NDVI from 1982 to 2006 in alpine meadow of the Three-River Source Region on the Qinghai-Tibetan Plateau
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High positive correlation between soil temperature and NDVI from 1982 to 2006 in alpine meadow of the Three-River Source Region on the Qinghai-Tibetan Plateau

机译:青藏高原三河源区1982年至2006年高寒草甸土壤温度与NDVI的高正相关

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摘要

Using satellite-observed Normalized Difference Vegetation Index (NDVI) data and Rotated Empirical Orthogonal Function (REOF) method, we analyzed the spatio-temporal variation of vegetation during growing seasons from May to September in the Three-River Source Region, alpine meadow in the Qinghai-Tibetan Plateau from 1982 to 2006. We found that NDVI in the centre and east of the region, where the vegetation cover is low, showed a consistent but slight increase before 2003 and remarkable increase in 2004 and 2005. Impact factors analysis indicted that among air temperature, precipitation, humid index, soil surface temperature, and soil temperature at 10 cm and 20 cm depth, annual variation of NDVI was highly positive correlated with the soil surface temperature of the period from March to July. Further analysis revealed that the correlation between the vegetation and temperature was insignificant before 1995, but statistically significant from 1995. The study indicates that temperature is the major controlling factor of vegetation change in the Three-River Source Region, and the currently increase of temperature may increase vegetation coverage and/or density in the area. In addition, ecological restoration project started from 2005 in Three-River Source Region has a certain role in promoting the recovery of vegetation.
机译:利用卫星观测的归一化植被指数(NDVI)数据和旋转经验正交函数(REOF)方法,我们分析了三河源区高寒草甸5月至9月生长季节植被的时空变化。 1982年至2006年是青藏高原。我们发现该地区中部和东部植被覆盖度较低的NDVI在2003年前呈现出稳定但略有增加的趋势,而在2004和2005年则显着增加。影响因素分析表明:在气温,降水量,湿度指数,土壤表面温度和10 cm和20 cm深度的土壤温度之间,NDVI的年变化与3月至7月期间的土壤表面温度高度正相关。进一步的分析表明,植被与温度之间的相关性在1995年之前微不足道,但从1995年开始具有统计学意义。研究表明,温度是三河源区植被变化的主要控制因素,目前温度的升高可能增加该地区的植被覆盖率和/或密度。此外,三河源区2005年启动的生态修复工程对促进植被恢复具有一定作用。

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