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降雨雪的全球模式及其对过去到未来预测的冲水的影响
Fadji Z Maina1,2, Sujay V Kumar3
1NASA Goddard Space Flight Center, Hydrological Sciences Laboratory, Greenbelt, MD, USA. fadjizaouna.maina@nasa.gov.
Nature communications
|May 21, 2025
概括
全球变暖增加了降雨与降雪 (ROS) 事件,特别是在寒冷的地区. 尽管ROS频率上升,但由于降雨量增加和积雪量减少,其对流水的贡献将会减少.
科学领域:
- 气候学 气候学 气候学
- 水文学的水文学
- 环境科学 环境科学
背景情况:
- 全球变暖正在改变寒冷地区的降雨模式.
- 降雨降雪 (ROS) 事件对生态和社会经济有重大影响.
- 为了有效管理,需要对历史和未来的ROS趋势进行全面的全球分析.
研究的目的:
- 分析降雨雪事件 (ROS) 的全球变化.
- 评估ROS对流水供应水的影响.
- 在不同的排放场景下 (SSP245和SSP585) 预测未来的ROS趋势.
主要方法:
- 分析自1950年以来的历史ROS数据.
- 使用气候模型预测未来的ROS趋势.
- 在不同的排放场景下评估ROS对流水的影响.
主要成果:
- 预计到2100年,ROS事件将在高度和高海拔地区显著增加.
- 尽管频率增加,但ROS对流水的贡献将减少50%以上.
- 气温的升温将减少ROS的影响,例如美国西部地区由于降低了积雪.
结论:
- 未来的气候变化将在特定地区加剧ROS事件.
- 随着ROS动态的变化,会改变流水的可用性.
- 适应策略是必要的,以管理ROS对水资源的影响的变化.
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