由于极端风暴聚集,密西西比河下部洪水危险增加
Yuan Liu1, Daniel B Wright1, Felipe Quintero2
1Department of Civil and Environmental Engineering, University of Wisconsin-Madison, Madison, WI, USA.
Science advances
|October 1, 2025
概括
复合风暴集群显著增加了密西西比河下流盆地 (LMRB) 的洪水严重性. 未来的气候变化将加剧这种情况,将洪水类型转向更具灾难性的事件,需要更新的管理策略.
科学领域:
- 水文学 水文学
- 气候科学 气候科学
- 环境工程 环境工程
背景情况:
- 下密西西比河流域 (LMRB) 的重大洪水通常与极端风暴事件有关.
- 风暴集群在LMRB洪水危险中的特定作用在历史上未被充分探索.
研究的目的:
- 调查复合时空风暴聚类对LMRB洪水特征的影响.
- 在气候变化场景下预测未来洪水类型的变化.
主要方法:
- 在LMRB中分析历史洪水数据和风暴模式.
- 在SSP3-7.0情景下的气候建模,用于2070-2100年期间.
- 来自不同风暴集群类型的洪水峰值,水量和持续时间的比较.
主要成果:
- 来自复合风暴集群的洪水比单个风暴的洪水具有更高的峰值,体积和持续时间.
- 未来的气候预测显示,极端风暴和降水量增加,干旱间隔减少.
- 预计到2070-2100年,主导洪水类型将从孤立风暴 (38%) 转变为复合风暴集群 (49%).
结论:
- 风暴集群是LMRB洪水危险的一个关键因素,往往导致更严重的事件.
- 预计气候变化将通过增加风暴集群加剧洪水风险.
- 目前对LMRB的洪水分析和管理策略必须纳入风暴集群的影响及其未来变化.
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