人类对全球地表水储量的变化
Sarah W Cooley1,2, Jonathan C Ryan3,4, Laurence C Smith4,5
1Department of Earth System Science, Stanford University, Stanford, CA, USA. scooley@stanford.edu.
Nature
|March 4, 2021
概括
人类管理的水库导致全球季节性地表水储量的57%变化. 卫星数据显示水库的波动为0.86米, 而自然水体的波动仅为0.22米,
科学领域:
- 水文学
- 环境科学
- 遥感技术
背景情况:
- 了解人类对全球水文循环的影响对于淡水可持续性至关重要.
- 对自然水体的水位数据有限,这阻碍了人类对地表水储量变化的影响.
研究的目的:
- 量化人类对全球地表水储量变化的影响程度.
- 评估人类管理的水库对季节性地表水储量变化的贡献.
- 通过卫星数据建立跟踪人类对全球水文循环的基线.
主要方法:
- 使用NASA的ICESat-2卫星激光高度计数据进行全球水位测量.
- 收集了2018年10月至2020年7月227,386个水体的水位变化数据集.
- 人类管理的水库和自然水体之间的季节性变化.
主要成果:
- 人类管理的水库占地球季节性地表水储量的57%.
- 水库的季节性变化平均为0.86米,明显高于自然水体 (0.22米).
- 人类影响导致全球45°N以南67%的地表水变化,在干旱地区达到近100%.
结论:
- 人类活动,主要是通过水库,显著改变了全球地表水储存的变化.
- 卫星遥感为监测人类对水文循环的影响提供了强大的工具.
- 这些发现凸显出人类发展和气候变化对全球水资源的压力越来越大.
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