全球水循环的永久性变化
1Department of Computational Hydrosystems, UFZHelmholtz Centre for Environmental Research, Leipzig, Germany.
概括
几十年来陆地储水数据显示土壤水分明显且不可逆转地下降. 这一长期趋势凸显了全球水资源的重大变化.
科学领域:
- 地球科学
- 环境科学
- 水文学
背景情况:
- 陆地水储存是地球水循环的关键组成部分.
- 了解TWS的长期趋势对于水资源管理和气候变化影响评估至关重要.
研究的目的:
- 分析几十年来陆地水库的变化.
- 确定土壤水分水平的长期趋势.
主要方法:
- 使用了跨越数十年的卫星重力测量数据 (例如,GRACE/GRACE-FO).
- 应用先进的时间序列分析技术对TWS数据.
主要成果:
- 在过去的几十年中,全球土壤湿度出现了显著且不可逆转的下降.
- 确定了土壤湿度下降的速度和程度的区域变化.
结论:
- 这些发现表明陆地生态系统持续干燥.
- 这种不可逆转的土壤湿度下降对农业,水资源和生态系统稳定性产生了深远的影响.
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