Vegetation Changes along the Qinghai-Tibet Plateau Engineering Corridor Since 2000 Induced by Climate Change and Human Activities
文献类型：期刊论文
| 作者 | Wang, Haibo1; Jin, Long2; Song, Yi3 |
| 刊名 | REMOTE SENSING
 |
| 出版日期 | 2018 |
| 卷号 | 10期号:1 |
| 关键词 | Permafrost Degradation Human Activities Vegetation Change Scale Effect Qinghai-tibet Plateau Engineering Corridor |
| DOI | 10.3390/rs10010095 |
| 文献子类 | Article |
| 英文摘要 | The Qinghai-Tibet (QT) Plateau Engineering Corridor is located in the hinterland of the QT Plateau, which is highly sensitive to global climate change. Climate change causes permafrost degradation, which subsequently affects vegetation growth. This study focused on the vegetation dynamics and their relationships with climate change and human activities in the region surrounding the QT Plateau Engineering Corridor. The vegetation changes were inferred by applying trend analysis, the Mann-Kendall trend test and abrupt change analysis. Six key regions, each containing 40 nested quadrats that ranged in size from 500 x 500 m to 20 x 20 km, were selected to determine the spatial scales of the impacts from different factors. Cumulative growing season integrated enhanced vegetation index (CGSIEVI) values were calculated for each of the nested quadrats of different sizes to indicate the overall vegetation state over the entire year at different spatial scales. The impacts from human activities, a sudden increase in precipitation and permafrost degradation were quantified at different spatial scales using the CGSIEVI values and meteorological data based on the double mass curve method. Three conclusions were derived. First, the vegetation displayed a significant increasing trend over 23.6% of the study area. The areas displaying increases were mainly distributed in the Hoh Xil. Of the area where the vegetation displayed a significant decreasing trend, 72.4% was made up of alpine meadows. Second, more vegetation, especially the alpine meadows, has begun to degenerate or experience more rapid degradation since 2007 due to permafrost degradation and overgrazing. Finally, an active layer depth of 3 m to 3.2 m represents a limiting depth for alpine meadows. |
| WOS关键词 | PERMAFROST CHANGES ; CHINA ; DYNAMICS ; DESERTIFICATION ; VARIABILITY ; ECOSYSTEMS ; PARAMETERS ; QUALITY ; MODEL ; SCALE |
| WOS研究方向 | Remote Sensing |
| 语种 | 英语 |
| WOS记录号 | WOS:000424092300094 |
| 源URL | [http://ir.ieecas.cn/handle/361006/5184]  |
| 专题 | 地球环境研究所_生态环境研究室 |
| 作者单位 | 1.Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, Lanzhou 730000, Peoples R China 2.CCCC First Highway Consultants Co Ltd, Minist Transport, Key Lab Highway Construct & Maintenance Technol P, Xian 710065, Shaanxi, Peoples R China 3.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710061, Shaanxi, Peoples R China |
| 推荐引用方式 GB/T 7714 | Wang, Haibo,Jin, Long,Song, Yi. Vegetation Changes along the Qinghai-Tibet Plateau Engineering Corridor Since 2000 Induced by Climate Change and Human Activities[J]. REMOTE SENSING,2018,10(1). |
| APA | Wang, Haibo,Jin, Long,&Song, Yi.(2018).Vegetation Changes along the Qinghai-Tibet Plateau Engineering Corridor Since 2000 Induced by Climate Change and Human Activities.REMOTE SENSING,10(1). |
| MLA | Wang, Haibo,et al."Vegetation Changes along the Qinghai-Tibet Plateau Engineering Corridor Since 2000 Induced by Climate Change and Human Activities".REMOTE SENSING 10.1(2018). |
入库方式： OAI收割
来源：地球环境研究所
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