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气候动态对水文干旱动态的签名:定性分析
Louis Kongoda Lisika1, Jacques Celestin Moliba Bankanza2,3, Louis Efoto Eale1
1Mention Physique et Technologie, Faculté des Sciences et Technologies, Université de Kinshasa, B.P. 127, KinshasaXI, Kinshasa, Congo.
Heliyon
|November 11, 2024
概括
刚果河流域经常出现的10年水文干旱与10年,8个月的气候干扰信号周期有关. 这个循环循环循环.
科学领域:
- 气候动力学 气候动力学
- 水文学的水文学
- 生态生态学 生态生态学
背景情况:
- 气候变化对水循环和生态系统产生重大影响.
- 自1969年以来,乌班圭河和卡萨伊河 (刚果河的支流) 经常发生的水文干旱缺乏明确的解释.
- 人类活动和植被变化在刚果流域是最小的,这表明气候动态是主要的驱动因素.
研究的目的:
- 为刚果河流域反复出现的水文干旱提出一个合理的解释.
- 研究气候动态在水文干旱模式中的作用.
- 分析气候干扰的时空动态.
主要方法:
- 贝叶斯式方法应用于网格式降水数据库 (1940-2020).
- 每年生成后期概率地图以可视化气候干扰.
- 对气候干扰信号 (CPS) 的定性分析,最大强度和迁移模式.
主要成果:
- 确定了受气候干扰影响的地区的时空表现.
- 揭示了CPS迁移的平均10年8个月周期.
- 观察到水文干旱事件 (自1969年以来) 和CPS迁移日期之间存在一致的巧合,这表明有很大的影响.
结论:
- 气候动态,特别是周期性干扰信号,在反复发生的水文干旱中起着至关重要的作用.
- 确定的10年8个月周期强烈影响水文干旱动态.
- 未来的研究应该专注于估计从气象干旱到水文干旱的传播时间,以完善对这一循环的理解.
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