Satellite-Observed Hydrothermal Conditions Control the Effects of Soil and Atmospheric Drought on Peak Vegetation Growth on the Tibetan Plateau
文献类型：期刊论文
| 作者 | Qiu, Zhengliang1; Tang, Longxiang1; Wang, Xiaoyue2; Zhang, Yunfei1; Tan, Jianbo1; Yue, Jun3; Xia, Shaobo1 |
| 刊名 | REMOTE SENSING
 |
| 出版日期 | 2024-11-01 |
| 卷号 | 16期号:22页码:4163 |
| 关键词 | peak vegetation growth drought soil moisture vapor pressure deficit Tibetan Plateau |
| DOI | 10.3390/rs16224163 |
| 产权排序 | 2 |
| 文献子类 | Article |
| 英文摘要 | Recent research has demonstrated that global warming significantly enhances peak vegetation growth on the Tibetan Plateau (TP), underscoring the influence of climatic factors on vegetation dynamics. Nevertheless, the effects of different drought types on peak vegetation growth remain underexplored. This study utilized satellite-derived gross primary productivity (GPP) and the normalized difference vegetation index (NDVI) to assess the impacts of soil moisture (SM) and vapor pressure deficit (VPD) on peak vegetation growth (GPPmax and NDVImax) across the TP from 2001 to 2022. Our findings indicate that NDVImax and GPPmax exhibited increasing trends in most regions, displaying similar spatial patterns, with 65.28% of pixels showing an increase in NDVImax and 72.98% in GPPmax. In contrast, the trend for SM primarily showed a decrease (80.86%), while VPD showed an increasing trend (74.75%). Through partial correlation analysis and ridge regression, we found that peak vegetation growth was significantly affected by SM or VPD in nearly 20% of the study areas, although the magnitude of these effects varied considerably. Furthermore, we revealed that hydrothermal conditions modulated the responses of peak vegetation growth to SM and VPD. In regions with annual precipitation less than 650 mm and an annual mean temperature below 10 degrees C, decreased SM and increased VPD generally inhibited peak vegetation growth. Conversely, in warm and humid areas, lower SM and higher VPD promoted peak vegetation growth. These findings are crucial for deepening our understanding of vegetation phenology and its future responses to climate change. |
| WOS关键词 | NET PRIMARY PRODUCTIVITY ; CLIMATE-CHANGE ; ALPINE ECOSYSTEM ; SPRING PHENOLOGY ; CO2 EXCHANGE ; RESPONSES ; IMPACTS ; VARIABILITY ; MEADOW ; TRENDS |
| WOS研究方向 | Environmental Sciences & Ecology ; Geology ; Remote Sensing ; Imaging Science & Photographic Technology |
| WOS记录号 | WOS:001366490300001 |
| 源URL | [http://ir.igsnrr.ac.cn/handle/311030/210477]  |
| 专题 | 陆地表层格局与模拟院重点实验室_外文论文 |
| 通讯作者 | Wang, Xiaoyue |
| 作者单位 | 1.Changsha Univ Sci & Technol, Sch Traff & Transportat Engn, Changsha 410114, Peoples R China 2.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Land Surface Pattern & Simulat, Beijing 100101, Peoples R China 3.Cent South Univ, Sch Automat, Changsha 410083, Peoples R China |
| 推荐引用方式 GB/T 7714 | Qiu, Zhengliang,Tang, Longxiang,Wang, Xiaoyue,et al. Satellite-Observed Hydrothermal Conditions Control the Effects of Soil and Atmospheric Drought on Peak Vegetation Growth on the Tibetan Plateau[J]. REMOTE SENSING,2024,16(22):4163. |
| APA | Qiu, Zhengliang.,Tang, Longxiang.,Wang, Xiaoyue.,Zhang, Yunfei.,Tan, Jianbo.,...&Xia, Shaobo.(2024).Satellite-Observed Hydrothermal Conditions Control the Effects of Soil and Atmospheric Drought on Peak Vegetation Growth on the Tibetan Plateau.REMOTE SENSING,16(22),4163. |
| MLA | Qiu, Zhengliang,et al."Satellite-Observed Hydrothermal Conditions Control the Effects of Soil and Atmospheric Drought on Peak Vegetation Growth on the Tibetan Plateau".REMOTE SENSING 16.22(2024):4163. |
入库方式： OAI收割
来源：地理科学与资源研究所
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