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Updated: Jul 16, 2025

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A Protocol for Conducting Rainfall Simulation to Study Soil Runoff
Published on: April 3, 2014
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[排水模拟及其对长江流域极端降雨的反应]
Shuang Gao1,2, Chao-Pu Ti2,3, Shui-Rong Tang1
1College of Tropical Crops, Hainan University, Haikou 570228, China.
Huan jing ke xue= Huanjing kexue
|September 12, 2023
概括
极端降水显著增加长江的下水量,特别是在上游. 本研究分析了排水变化,并为气候变化中的水资源管理提供了见解.
科学领域:
- 水文和气候科学 水文和气候科学
- 水资源管理 水资源管理
- 环境建模环境建模
背景情况:
- 排水研究对于水资源分配,洪水/干旱控制和污染管理至关重要.
- 全球变暖改变了极端气候事件,影响了排水模式.
- 了解这些变化对于有效的水资源战略至关重要.
研究的目的:
- 模拟长江流域 (1965-2019) 的时空流量变化.
- 在极端条件下分析流水对降水的反应.
- 为水资源管理决策提供信息.
主要方法:
- 使用了土壤和水资源评估工具 (SWAT) 模型.
- 从1965年到2019年的模拟流水变化.
- 分析了极端降水事件对每日,每月和每年的下水的影响.
主要成果:
- 盆地的总流量从1965年到2019年没有显著变化.
- 流水经历了四个干湿阶段:干湿干湿湿.
- 极端降水事件导致了大量的下水量增加,特别是在长江上游.
- 一个50年的极端降水事件增加了6200% (上游),21% (中游) 和15% (下游) 的每日平均下水量.
- 一个100年极端降水事件每日平均下水量增加了8000% (上游),25% (中游) 和17% (下游).
结论:
- 对极端降水的水文反应在长江流域各不相同.
- 这些发现有助于更好地了解气候变化对水资源的影响.
- 为水资源管理者和决策者提供有价值的数据.
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