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降雨强度的增加会在一个大河流盆地内引发空间上不同的水文变化
Yiping Wu1,2, Xiaowei Yin1, Guoyi Zhou3
1Institute of Global Environmental Change, Department of Earth & Environmental Science, Xi'an Jiaotong University, Xi'an, Shaanxi, 710049, PR China.
Nature communications
|January 27, 2024
概括
全球变暖加剧了降雨量,导致中国南部上游干旱和下游洪水. 这种对比的模式威胁到水和粮食安全.
科学领域:
- 气候科学 气候科学
- 水文学的水文学
- 环境科学 环境科学
背景情况:
- 干旱和洪水与极端降雨有关,随着全球变暖而加剧.
- 中国西南地区同时发生的干旱和中国东南地区的洪水凸显了人们对相互关系的不充分理解.
研究的目的:
- 在54年的时间里 (1965-2018) 调查水文气象变量的时空变化.
- 了解中国南部西河流域土壤湿度和干燥度模式对比背后的机制.
主要方法:
- 分析水气变量的时空变化.
- 研究导致土壤干燥/湿模式的机制.
- 在西河流域对54年 (1965-2018) 的研究.
主要成果:
- 降雨强度的增加导致了严重的上游干燥,减少了土壤的储水量,水产和基流量.
- 下游地区的土壤水储量,水产和基础流量增加.
- 形成了对比的土壤干燥 (上游) 和湿度 (下游) 模式.
结论:
- 降雨强度和地形相互作用,同时产生干旱和洪水风险.
- 这些对比的模式在气候变化下增加了水和粮食安全的脆弱性.
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