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Updated: Jul 18, 2025

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排水过程对气象干旱的反应:基本流量指数作为一个重要的指标
Ruichen Mao1, Aying Shi1, Jinxi Song2
1Shaanxi Key Laboratory of Earth Surface System and Environmental Carrying Capacity, College of Urban and Environmental Sciences, Northwest University, Xi'an, 710127, China.
Journal of environmental management
|August 20, 2023
概括
了解气象干旱 (MD) 如何影响河流流和底流是水资源管理的关键. 这项研究表明,干旱影响因季节性和盆地而异,受基础流量指数 (BFI) 的影响,有助于干旱缓解工作.
科学领域:
- 水文学的水文学
- 水资源管理 水资源管理
- 环境科学 环境科学
背景情况:
- 流水和基流是水资源管理的关键组成部分.
- 了解气象干旱对这些水文元素的影响,对于制定有效的抗干旱战略至关重要.
研究的目的:
- 定义流水和基流对威河流域气象干旱 (MD) 的反应.
- 分析干旱应对特征的空间和季节差异.
- 调查基流指数 (BFI) 在干旱传播中的作用.
主要方法:
- 估计每周的皮尔森相关系数和流出/基流和MD之间的相互信息分数.
- 确定流出/基流到MD的最佳响应时间.
- 讨论响应特征的空间和季节性变化.
- 介绍基本流量指数 (BFI) 以解释干旱传播.
主要成果:
- 由于独特的盆地属性,MD向流水和基流的过渡序列因子盆地而异.
- 流水对MD的反应显示出显著的季节性和水文周期性,在夏季/秋季 (潮季) 较快,较强,在冬季/春季 (干季) 较弱.
- 基本流量指数 (BFI) 有效地解释了盆地和季节间反应时间的变化,表明其在确定干旱传播速度方面的实用性.
结论:
- 该研究阐明了下水过程对气象干旱的反应特征.
- 它增强了对干旱传播机制的理解,这对于减轻与干旱有关的危险至关重要.
- 基础流量指数 (BFI) 作为评估干旱传播速度和对水文系统影响的有价值指标.
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