Declining Effect of Precipitation on the Normalized Difference Vegetation Index of Grasslands in the Inner Mongolian Plateau, 1982-2010

被引:9
作者
Li, Yanan [1 ,2 ,3 ,4 ,5 ]
Wu, Dan [1 ,2 ,3 ,4 ,5 ]
Yang, Liangyan [1 ,2 ,3 ,4 ,5 ]
Zhou, Tiancai [6 ]
机构
[1] Shaanxi Prov Land Engn Construct Grp Co Ltd, Xian 710075, Peoples R China
[2] Shaanxi Prov Land Engn Construct Grp Co Ltd, Inst Land Engn & Technol, Xian 710075, Peoples R China
[3] Shaanxi Land Engn Construct Grp Co Ltd, Technol Innovat Ctr Land Engn & Human Settlements, Xian 710075, Peoples R China
[4] Xi An Jiao Tong Univ, Xian 710075, Peoples R China
[5] Minist Nat Resources, Key Lab Degraded & Unused Land Consolidat Engn, Xian 710075, Peoples R China
[6] Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Ecosyst Network Observat & Modelling, Beijing 100101, Peoples R China
来源
APPLIED SCIENCES-BASEL | 2021年 / 11卷 / 18期
关键词
normalized difference vegetation index; temperature; precipitation; climate change; Inner Mongolian Plateau; TIBETAN PLATEAU; CLIMATE; NDVI; TEMPERATURE; VARIABILITY; SENSITIVITY; DIVERSITY; RESPONSES; PATTERNS; EXCHANGE;
D O I
10.3390/app11188766
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
Grasslands play an irreplaceable role in maintaining carbon balance and stabilizing the entire Earth's ecosystem. Although the grasslands in Inner Mongolia are sensitive and vulnerable to climate change, a generalized effect of climate change on the grasslands is still unavailable. In this study, we analyzed the effects of annual mean precipitation and annual mean temperature on the normalized difference vegetation index from 1982 to 2010 on the Inner Mongolia Plateau. Our results indicated that the normalized difference vegetation index was mostly affected by precipitation, followed by temperature. Spatially, temperature and precipitation had greater effects on normalized difference vegetation index in dry regions than in wet ones. In time series, the effect of precipitation on normalized difference vegetation index had significantly decreased from 1982 to 2010 (R-2 = 0.11, p > 0.05). However, the effect of temperature on normalized difference vegetation index remained stable. The high variation effect of precipitation on normalized difference vegetation index was due to the significant decrease in precipitation from 1980 to 2010. Thus, 35.47% and 0.56% of the dynamic of normalized difference vegetation index from 1982 to 2010 was accounted for by the precipitation and temperature, respectively. Our findings highlighted that grasslands are adaptable to the significant increase in temperature, but are sensitive to the decrease in precipitation on the Inner Mongolia Plateau.
引用
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页数:10
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