史无前例的大陆干旱,淡水供应减少,土地对海平面上升的贡献增加
Hrishikesh A Chandanpurkar1,2, James S Famiglietti2, Kaushik Gopalan1
1FLAME University, Pune, India.
Science advances
|July 25, 2025
概括
全球陆地储水 (TWS) 正在迅速下降,而巨型干燥地区正在扩大. 地下水的枯竭推动了大陆的干旱,影响了淡水的供应,并导致海平面上升.
科学领域:
- 地球科学 地球科学 地球科学
- 水文学的水文学
- 气候科学 气候科学
背景情况:
- 陆地储水 (TWS) 变化是全球淡水供应的关键指标.
- 监测TWS对于了解气候变化影响和水资源管理至关重要.
研究的目的:
- 使用NASA GRACE/GRACE-FO数据量化自2002年以来的大陆TWS变化.
- 确定TWS损失的驱动因素,并评估大陆干燥的全球影响.
主要方法:
- 从2002年到现在的NASA GRACE和GRACE-FO卫星重力数据的分析.
- 量化整个大陆地区的TWS变化.
- 将TWS变化归因于各种驱动因素,包括地下水枯竭.
主要成果:
- 自2002年以来,在全球范围内观察到重大的和前所未有的TWS损失.
- "超级干燥"地区的扩张速度每年是加利福尼亚州的两倍.
- 在非冰化大陆地区,地下水枯竭占TWS损失的68%.
- 干燥区域正在扩大,干燥的速度比湿地区的湿速度快.
- 大陆的干燥对海平面上升作出了重大贡献,超过了冰盖和陆地冰川的贡献.
结论:
- 大陆的干燥是一个广泛和加速的现象,具有深刻的全球影响.
- 需要采取紧急行动,以应对淡水供应量下降和相关海平面上升的影响.
- 调查结果强调了对可持续水资源管理和气候变化缓解战略的关键需求.
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