[1]WANG Jialu,LI Weijie,WANG Yong,et al.Spatial-Temporal Variation of NDVI and Its Responses to Hydrothermal Condition in Rocky Desertification Area of Chongqing City from 2005 to 2014[J].Research of Soil and Water Conservation,2021,28(02):217-223.
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Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume:
28
Number of periods:
2021 02
Page number:
217-223
Column:
Public date:
2021-02-06
- Title:
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Spatial-Temporal Variation of NDVI and Its Responses to Hydrothermal Condition in Rocky Desertification Area of Chongqing City from 2005 to 2014
- Author(s):
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WANG Jialu1,2, LI Weijie2, WANG Yong2, REN Juan2, GAO Min
2
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(1.School of Resources and Environmental Engineering, Anshun University, Anshun, Guizhou 561000, China; 2.Chongqing Key Laboratory of Karst Environment/School of Geographical Sciences, Southwest University, Chongqing 400715, China)
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- Keywords:
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spatial temporal variation of NDVI; climate data; in rocky desertification area; Chongqing City
- CLC:
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P951
- DOI:
-
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- Abstract:
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In order to understand the restoration of vegetation and the treatment of ecological environment in rocky desertification areas of Chongqing City, NDVI and meteorological data from 2005 to 2014 in rocky desertification areas of Chongqing City were selected, and trend analysis, variation coefficient analysis, partial correlation analysis and other methods to focus on the spatial-temporal variation of NDVI in the rocky desertification areas of Chongqing City over the past 10 years were used, and the correlations between the NDVI and climatic factors were analyzed. The results show that:(1)the interannual variation of NDVI shows an overall increasing trend in rocky desertification areas of Chongqing City, with an increasing rate of 0.08/10 a. Among them, the growth rate in northeast Chongqing City is relatively high, up to 0.09/10 a, and the seasonal variation of NDVI has some differences, and the spring growth is the most significant, mainly distributed in the northeast, central and western regions of Chongqing City;(2)the area with increasing NDVI in the northeastern Chongqing has a large area, which plays a crucial role in improving the ecological environment and soil and water conservation in the Three Gorges reservoir area; the NDVI in the rocky desertification regions of southeastern and midwest Chongqing City remained as a whole, but the areas with decreasing NDVI were mainly distributed in the Wujiang River Basin;(3)the coefficient of variation of NDVI in rock desertification of Chongqing City from 2005 to 2014 was relatively low, and the degree of variation was mainly stable;(4)the positive correlation between precipitation and NDVI in rocky desertification areas of Chongqing City is larger than that of negative correlation, the same to the positive correlation between temperature and NDVI. In general, high-humidity environment promoted the growth of vegetation in the Three Gorges reservoir area to a certain extent, while the low-temperature environment has inhibited the growth of vegetation in the Wujiang River Basin.