Investigating the spatially heterogeneous relationships between climate factors and NDVI in China during 1982 to 2013

doi:10.1007/s11442-019-1682-2

Abstract

Abstract:

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.

Figures/Tables 7

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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
Moran’s I	Variability	0.68	0.73	0.70	0.70	0.63
Z	Mean	41.58	42.03	41.22	42.07	41.99
Z	Variability	34.18	39.72	36.64	37.28	30.54

	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