1992年至2020年在西伯利亚的土地覆盖面变化及其驱动因素
Lin Wang1,2, Guimin Liu3, Xiaodong Wu2
1School of Environmental and Municipal Engineering, Ministry of Education Engineering Research Center of Water Resource Comprehensive Utilization in Cold and Arid Regions, Lanzhou Jiaotong University, Lanzhou, 730070, China.
Environmental monitoring and assessment
|December 6, 2024
概括
由于气候变暖和永久土退化,西伯利亚的土地覆盖面正在发生变化. 森林正在缩小,而草原,灌木,特别是耕地和建筑面积正在扩大,这是由温度和降水变化所驱动的.
科学领域:
- 环境科学环境科学
- 气候变化研究研究 气候变化研究
- 生态生态学 生态生态学
背景情况:
- 西伯利亚广的永久土地区对气候变暖很敏感.
- 了解土地覆盖的动态对于这些地区的生态保护至关重要.
研究的目的:
- 分析 1992 年至 2020 年西伯利亚的土地覆盖变化.
- 确定这些土地覆盖变化的主要驱动因素.
主要方法:
- 对土地覆盖面和气候数据集的分析.
- 追踪植被类型和建筑区域的变化.
- 研究温度,降水和活性层厚度的影响.
主要成果:
- 常青树和落叶针叶树的显著减少.
- 草原,灌木,耕地和建筑用地面积显著增加.
- 农田和建筑用地分别在永久和非永久区扩张最快.
- 农业和建筑用地地理中心的变化.
- 温度和降水被确定为主要驱动因素,活性层厚度影响特定的土地覆盖类型.
结论:
- 气候变化和永久土退化正在显著改变西伯利亚的土地覆盖面.
- 这些发现有助于更好地了解永久土地区的土地覆盖面变化机制.
- 提供了对永久土融化的生态反应的新见解.
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