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Updated: Sep 15, 2025

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Continuous Hydrologic and Water Quality Monitoring of Vernal Ponds
Published on: November 13, 2017
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在南部帕拉伊巴州河流盆地评估雨量和流量指数
Agueda T DE Carvalho1, Celso B M Ribeiro1, Aline S Procópio1
1Universidade Federal de Juiz de Fora, Departamento de Engenharia Ambiental e Sanitária, Rua José Lourenço Kelmer, s/n, São Pedro, 36036-900 Juiz de Fora, MG, Brazil.
Anais da Academia Brasileira de Ciencias
|July 16, 2025
概括
南帕拉伊巴州流域的极端降雨和河流流动事件没有显著的趋势. 尽管河流流量下降,但降水模式仍然稳定,这表明减少河流流量的非气象原因.
科学领域:
- 水文学的水文学
- 气候科学 气候科学
- 环境科学 环境科学
背景情况:
- 南方帕拉伊巴河流域是一个关键的水资源区域.
- 了解极端降雨和河流流量对于水资源管理和气候变化适应至关重要.
- 需要进行长期数据分析,以确定水文变化的趋势和驱动因素.
研究的目的:
- 分析1962年至2022年在南方帕拉伊巴河流域发生的极端最大降雨和河流流动事件.
- 为了确定极端水文事件的趋势和历史时间序列数据.
- 为了研究降水模式和溪流流动趋势之间的关系.
主要方法:
- 从雨量计和流量计站通过HIDROWEB收集数据.
- 使用99百分位数 (降雨量) 和冈贝尔分布 (流量) 识别极端值.
- 使用曼-肯达尔测试进行趋势分析,使用CHIRPS数据进行空间分析.
主要成果:
- 极端降雨和河流流动事件通常没有统计学意义.
- 历史降水系列显示出混合的正负趋势,而溪流流动趋势始终是负的.
- 空间分析显示,盆地的降雨分布异质.
结论:
- 南帕拉伊巴河流域表现出明显的流量下降趋势.
- 降水趋势与观测到的溪流流量减少没有相关性.
- 河流流量减少可能受到气象变化以外的其他因素的影响,例如土地使用或水抽取.
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