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Changes in satellite-derived vegetation growth trend in temperate and boreal Eurasia from 1982 to 2006

机译:1982年至2006年温带和北方欧亚大陆卫星衍生的植被生长趋势的变化

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Monitoring changes in vegetation growth has been the subject of considerable research during the past several decades, because of the important role of vegetation in regulating the terrestrial carbon cycle and the climate system. In this study, we combined datasets of satellite-derived Normalized Difference Vegetation Index (NDVI) and climatic factors to analyze spatio-temporal patterns of changes in vegetation growth and their linkage with changes in temperature and precipitation in temperate and boreal regions of Eurasia (>23.5 degrees N) from 1982 to 2006. At the continental scale, although a statistically significant positive trend of average growing season NDVI is observed (0.5 x 10(-3) year (1), P = 0.03) during the entire study period, there are two distinct periods with opposite trends in growing season NDVI. Growing season NDVI has first significantly increased from 1982 to 1997 (1.8 x 10(-3) year(-1), P < 0.001), and then decreased from 1997 to 2006 (-1.3 x 10(-3) year(-1), P = 0.055). This reversal in the growing season NDVI trends over Eurasia are largely contributed by spring and summer NDVI changes. Both spring and summer NDVI significantly increased from 1982 to 1997 (2.1 x 10(-3) year(-1), P = 0.01; 1.6 x 10(-3) year(-1) P < 0.001, respectively), but then decreased from 1997 to 2006, particularly summer NDVI which may be related to the remarkable decrease in summer precipitation ( 2.7mm yr(-1), P = 0.009). Further spatial analyses supports the idea that the vegetation greening trend in spring and summer that occurred during the earlier study period 1982-1997 was either stalled or reversed during the following study period 1997-2006. But the turning point of vegetation NDVI is found to vary across different regions.
机译:在过去的几十年中,由于植被在调节陆地碳循环和气候系统中的重要作用,监测植被生长的变化已成为大量研究的主题。在这项研究中,我们结合了源自卫星的归一化差异植被指数(NDVI)和气候因素的数据集,分析了欧亚大陆温带和寒带地区植被生长变化的时空格局及其与温度和降水变化的联系(>从1982年到2006年是23.5度N。)在整个大陆范围内,尽管在整个研究期间平均观察到NDVI的平均生长季节呈积极趋势(0.5 x 10(-3)年(1),P = 0.03),生长季NDVI有两个截然相反的时期。 NDVI的生长期从1982年到1997年首先显着增加(1.8 x 10(-3)年(-1),P <0.001),然后从1997年到2006年下降(-1.3 x 10(-3)年(-1) ),P = 0.055)。欧亚大陆生长季NDVI趋势的这种逆转很大程度上是由春季和夏季NDVI的变化引起的。从1982年到1997年,春季和夏季NDVI均显着增加(分别为2.1 x 10(-3)year(-1),P = 0.01; 1.6 x 10(-3)year(-1)P <0.001),但是从1997年到2006年下降,特别是夏季NDVI,这可能与夏季降水的显着下降有关(2.7mm yr(-1),P = 0.009)。进一步的空间分析支持了这样一个观点,即在较早的研究期1982-1997年发生的春季和夏季植被绿化趋势在随后的1997-2006年的研究期中被停止或逆转。但是,发现植被NDVI的转折点在不同地区之间有所不同。

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