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NDVI-based vegetation changes and their responses to climate change from 1982 to 2011: A case study in the Koshi River Basin in the middle Himalayas

机译:1982年至2011年基于NDVI的植被变化及其对气候变化的响应:以喜马拉雅中部科希河流域为例

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Considerable researches during the past several decades have focused on monitoring changes in vegetation growth due to its important role in regulating the terrestrial carbon cycle and the climate system. In this study, we combined datasets of the satellite-derived Normalized Difference Vegetation Index (NDVI) and climatic factors to analyze spatio-temporal patterns of vegetation growth in 1982-2006 in the Koshi River Basin (KRB) in the middle Himalayas. In addition, the dataset from the global land surface satellite sensor from SPOT-4's Vegetation instrument in 1998-2011 was used to further verify the results of this study. At the regional scale, although a statistically significant increase in average growing season NDVI was observed (0.0008 yr~(-1) P = 0.03) during the entire study period, there existed three distinct periods with opposing trends. Growing season NDVI significantly increased in 1982-1994 (0.0019 yr~(-1) P = 0.03), and then decreased in 1994-2000 ( - 0.0058 yr~(-1), P< 0.001), while increased again in 2000-2006 (0.0049 yr~(-1) P < 0.001) and in 2000-2011 (0.0034 yr~(-1) P < 0.001). A sudden drop in NDVI in 1994-2000 largely contributed to these fluctuations in growing season NDVI over the KRB. Spring, summer and autumn NDVI significantly decreased in 1994-2000 (-0.0077 yr~(-1), P< 0.001; -0.0067 yr~(-1), P< 0.001; and -0.0155 yr~(-1), P < 0.001; respectively). Our further spatial analyses supported the existence of the sudden decrease in spring, summer and autumn NDVI in 1994-2000.
机译:在过去的几十年中,由于其在调节陆地碳循环和气候系统中的重要作用,因此大量研究集中在监测植被生长的变化。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)和气候因子的数据集,以分析1982-2006年喜马拉雅中部科希河流域(KRB)的植被生长时空格局。此外,还使用了1998-2011年SPOT-4的Vegetation仪器中的全球地面卫星传感器数据集来进一步验证这项研究的结果。在区域范围内,尽管在整个研究期间平均生长期NDVI出现了统计上的显着增长(0.0008 yr〜(-1)P = 0.03),但存在三个截然相反的时期。生长季NDVI在1982-1994年显着增加(0.0019 yr〜(-1)P = 0.03),然后在1994-2000年下降(-0.0058 yr〜(-1),P <0.001),而在2000-2000年再次增加2006年(0.0049年〜(-1)P <0.001)和2000-2011年(0.0034年〜(-1)P <0.001)。 1994-2000年NDVI的突然下降很大程度上是导致KRB上NDVI生长季节出现这些波动的原因。 1994-2000年春,夏,秋季NDVI显着下降(-0.0077 yr〜(-1),P <0.001; -0.0067 yr〜(-1),P <0.001;和-0.0155 yr〜(-1),P <0.001;分别)。我们进一步的空间分析支持在1994-2000年春季,夏季和秋季NDVI突然下降。

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