Journal of Geographical Sciences >
Investigating the spatially heterogeneous relationships between climate factors and NDVI in China during 1982 to 2013
Gao Jiangbo, PhD, specialized in climate change risk and adaptation. E-mail: gaojiangbo@igsnrr.ac.cn |
Received date: 2019-01-10
Accepted date: 2019-03-20
Online published: 2019-12-09
Supported by
National Key R&D Program of China(No.2018YFC1508900)
National Key R&D Program of China(No.2018YFC1509003)
National Key R&D Program of China(No.2018YFC1508801)
National Natural Science Foundation of China(No.41671098)
Strategic Priority Research Program of the Chinese Academy of Sciences(No.XDA19040304)
Strategic Priority Research Program of the Chinese Academy of Sciences(No.XDA20020202)
Copyright
Climate change is a major driver of vegetation activity, and thus their complex processes become a frontier and difficulty in global change research. To understand this relationship between climate change and vegetation activity, the spatial distribution and dynamic characteristics of the response of NDVI to climate change were investigated by the geographically weighted regression (GWR) model during 1982 to 2013 in China. This model was run based on the combined datasets of satellite vegetation index (NDVI) and climate observation (temperature and moisture) from meteorological stations nationwide. The results showed that the spatial non-stationary relationship between NDVI and surface temperature has appeared in China: the significant negative temperature-vegetation relationship was located in Northeast, Northwest and Southeast China, while the positive correlation was more concentrated from southwest to northeast. By comparing the normalized regression coefficients from GWR model for different climate factors, it presented the regions with moisture dominants for NDVI were in North China and the Tibetan Plateau, and the areas of temperature dominants were distributed in East, Central and Southwest China, where the annual mean maximum temperature accounted for the largest areas. In addition, regression coefficients from GWR model between NDVI dynamics and climate variability indicated that the higher warming rate could result in the weakened vegetation activity through some mechanisms such as enhanced drought, while the moisture variability could mediate the hydrothermal conditions for the variation of vegetation activity. When the increasing rate of photosynthesis exceeded that of respiration, the positive correlation between vegetation dynamics and climate variability was reflected. However, the continuous and dynamic process of vegetation activity response to climate change will be determined by spatially heterogeneous conditions in climate change and vegetation cover. Furthermore, the dynamic description of climate-induced vegetation activity from its rise to decline in different regions is expected to provide a scientific basis for initiating ecosystem-based adaptation strategies in response to global climate change.
Key words: NDVI; climate change; spatial heterogeneity; GWR; China
GAO Jiangbo , JIAO Kewei , WU Shaohong . Investigating the spatially heterogeneous relationships between climate factors and NDVI in China during 1982 to 2013[J]. Journal of Geographical Sciences, 2019 , 29(10) : 1597 -1609 . DOI: 10.1007/s11442-019-1682-2
Table 1 Moran’s I and Z scores of regression coefficients for each factor in GWR model |
Regression coefficients | Average temperature | Maximum temperature | Minimum temperature | Precipitation | Relative humidity | |
---|---|---|---|---|---|---|
Moran’s I | Mean | 0.75 | 0.75 | 0.74 | 0.76 | 0.76 |
Variability | 0.68 | 0.73 | 0.70 | 0.70 | 0.63 | |
Z | Mean | 41.58 | 42.03 | 41.22 | 42.07 | 41.99 |
Variability | 34.18 | 39.72 | 36.64 | 37.28 | 30.54 |
Figure 1 Spatial pattern of NDVI (a) and spatial regression coefficients between NDVI and temperature (b: average; c: maximum; d: minimum) in GWR model from 1982 to 2013 |
Figure 2 Affected regions of climatic factors to vegetation activity during 1982-2013 from GWR model |
Table 2 The distribution proportion of affected regions of climatic factors in China |
Average temperature | Maximum temperature | Minimum temperature | Precipitation | Relative humidity | Other factors | |
---|---|---|---|---|---|---|
Number of grids | 187 | 743 | 131 | 1278 | 454 | 202 |
Proportion (%) | 6.24 | 24.81 | 4.37 | 42.67 | 15.16 | 6.74 |
Figure 3 Spatial distribution of NDVI (a), precipitation (b) and relative humidity trends (c) from 1982 to 2013 |
Figure 4 Spatial regression coefficients between NDVI variability and temperature variability (a. average; b. maximum; c. minimum) from GWR model from 1982 to 2013 |
Figure 5 Spatial regression coefficients between NDVI variability and moisture variability (a. precipitation; b. relative humidity) from GWR model from 1982 to 2013 |
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