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一种概率方法来加强阿尔卑斯山地区的干旱建模:从气象干旱过渡到水文干旱
Linshan Yang1, Wanghan He2, Xingyi Zou2
1State Key Laboratory of Ecological Safety and Sustainable Development in Arid Lands, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, 730000, China; Qilian Mountains Eco-Environment Research Centre in Gansu Province, Lanzhou, 730000, China.
Journal of environmental management
|June 24, 2025
概括
阿尔卑斯山地区的水文干旱比气象干旱更严重和更长时间. 了解这种转变对于更好的水资源管理和早期干旱预警至关重要.
科学领域:
- 水文学 水文学
- 气候学 气候学 气候学
- 环境科学 环境科学
背景情况:
- 阿尔卑斯山地区因干旱而面临重大水资源管理挑战.
- 了解从气象干旱到水文干旱的过渡对于缓解战略至关重要.
研究的目的:
- 调查山 (QLM) 的气象干旱到水文干旱的过渡动态.
- 确定影响干旱过渡的关键因素,并评估水调节能力的弹性.
主要方法:
- 从19个阿尔卑斯山盆地 (1982-2015) 分析了每月的流量和气象数据.
- 应用Gumbel copula函数和贝叶斯方法来建模干旱过渡.
- 相关性分析用于评估干旱持续时间,严重程度和影响因素之间的关系.
主要成果:
- 在QLM,水文干旱不那么频繁,但比气象干旱更严重和更长时间.
- 干旱过渡反应时间随着干旱持续时间的增加而减少.
- 冰川覆盖面和土壤水的变化是影响干旱过渡的重要因素,解释了超过20%的变化.
结论:
- 干旱加剧在QLM的气象,水文和复合干旱中显示出一致的模式.
- 随着干旱严重程度的增加,QLM的水调节能力的弹性可能正在下降.
- 调查结果强调需要改进干旱早期预警系统和高山环境中的水资源管理.
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