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气候和人类对埃尔多斯高原最近湖泊面积变化的影响
Muhammad Naeem1, Yongqiang Zhang2, Vahid Nourani3
1Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China; University of Chinese Academy of Sciences, Beijing 100049, China.
Journal of environmental management
|November 28, 2024
概括
由于气候和人类活动,中国埃尔多斯高原的湖泊面积大幅下降,但在政策变化后恢复. 有效的水资源管理和法规对于长期湖泊生态系统的可持续性至关重要.
科学领域:
- 水文学的水文学
- 环境科学 环境科学
- 生态生态学 生态生态学
背景情况:
- 湖泊生态系统在理解变化方面面临挑战,特别是人类对其造成的重大影响.
- 埃尔多斯高原的地表水体是环境健康的关键指标.
研究的目的:
- 分析2000年至2022年埃尔多斯高原湖面面积变化.
- 研究气候和人类因素对这些湖泊动态的影响.
- 量化各种因素对观测到的湖面变化的贡献.
主要方法:
- 远程传感数据分析,绘制湖面面积变化图.
- 统计分析以将湖区动态与气候变量 (降水,温度,蒸发) 和人为活动 (采矿,灌,放牧) 相关联.
- 对每个因素独立影响的定量评估.
主要成果:
- 2000年至2011年间,湖面总面积减少了18.23% (35平方公里),主要原因是降雨量减少,蒸发转化增加和人类活动.
- 到2022年出现了显著的复苏,湖面面积增加了75.8% (119平方公里),归因于更严格的政策法规.
- 降水和采矿是主要的驱动因素,对变化贡献了分别约25.47%和22.22%.
结论:
- 埃尔多斯高原的湖泊动态复杂,受到气候变化和人类干预的影响.
- 政策干预和改善水资源管理在恢复湖泊生态系统方面是有效的.
- 可持续的土地利用和严格的环境法规对于长期保护埃尔多斯高原的湖泊至关重要.
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