近20年塔里木河流域植被变化及与气候因子的关系

岳胜如; 王伦澈; 曹茜; 孙嘉; 崔利芳

doi:10.3799/dqkx.2024.047

Volume 50 Issue 1

Jan. 2025

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Yue Shengru, Wang Lunche, Cao Qian, Sun Jia, Cui Lifang, 2025. Vegetation Changes in Tarim River Basin over Past 20 Years and Their Relationship with Climate Factors. Earth Science, 50(1): 33-45. doi: 10.3799/dqkx.2024.047

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Yue Shengru, Wang Lunche, Cao Qian, Sun Jia, Cui Lifang, 2025. Vegetation Changes in Tarim River Basin over Past 20 Years and Their Relationship with Climate Factors. Earth Science, 50(1): 33-45. doi: 10.3799/dqkx.2024.047

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Vegetation Changes in Tarim River Basin over Past 20 Years and Their Relationship with Climate Factors

doi: 10.3799/dqkx.2024.047

Yue Shengru^{1, 2
,
,},
Wang Lunche^{1
,
,},
Cao Qian¹,
Sun Jia¹,
Cui Lifang³

1.
School of Geography and Information Engineering, China University of Geosciences, Wuhan 430078, China
2.
College of Water Resources and Architecture Engineering, Tarim University, Alaer 843300, China
3.
School of Geography and Tourism, Huanggang Normal University, Huanggang 438000, China

Received Date: 2023-12-11
Available Online: 2025-02-10
Publish Date: 2025-01-25

Abstract

Abstract

To understand the role of climatic factors in driving vegetation changes in the Tarim River Basin during the "warming and humidification" process in Northwest China, based on the linear regression, coefficient of variation, Person correlation coefficient, Hurst index and partial derivative methods, the climate-driven mechanism of vegetation change in the Tarim River Basin was quantitatively evaluated using MODIS satellite remote sensing data and meteorological data. It is found that the optimal vegetation growth and productivity levels in the basin showed a fluctuating upward trend, and the index NDVI, EVI, and NPP growth rates were 0.036 4/10a, 0.023 8/10a, and 12.606 1 gC/(m²∙10a), respectively. The Hurst index shows that the study area had the problem of uncertainty of continuous change in vegetation, and the areas of continuous improvement accounted for 19.7%, 18.7%, and 6.1% of the watershed area, respectively. At the watershed scale, the contributions of climatic factors to NDVI, EVI, and NPP were 0.001 6/10a, 0.001 0/10a, and 2.801 9 gC/(m²∙10a), respectively. Precipitation was the main climatic factor affecting vegetation change compared to air temperature; radiation had an inhibitory effect on vegetation change. Climate change contributed limitedly to the changes in optimal vegetation growth, but promoted significant improvements in vegetation productivity. The results reveal the spatial characteristics of vegetation change and climate-driven changes in the Tarim River Basin.
- Tarim River Basin,
- vegetation change,
- driving mechanism,
- quantitative evaluation,
- climate change

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References(49)

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Vegetation Changes in Tarim River Basin over Past 20 Years and Their Relationship with Climate Factors

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