[天气,土壤和水文干旱传播在内蒙古不同水平之间的关系,中国]
Meng-Meng Zhang1,2, En-Liang Guo1,2, Yong-Fang Wang1,2,3
11 College of Geographical Science, Inner Mongolia Normal University, Hohhot 010022, China.
概括
干旱在内蒙古各地正在加剧,土壤水分不足主要引发水文干旱. 了解这些传播模式是有效干旱减缓战略的关键.
科学领域:
- 环境科学 环境科学
- 水文学的水文学
- 气候学 气候学 气候学
背景情况:
- 干旱传播机制对于制定有效的减缓战略至关重要.
- 内蒙古面临着重大的气象,土壤和水文干旱挑战.
研究的目的:
- 研究内蒙古气象,土壤和水文干旱传播的时空特征.
- 分析不同干旱类型之间的滞后效应和过渡时间.
主要方法:
- 利用了ERA5-Land土壤湿度和地表排水数据 (1980-2022) 和气象站观测.
- 计算了标准化指数:SPEI,SSI和SRI在各种时间尺度上.
- 应用运行理论,Theil-Sen趋势分析,曼-肯德尔测试和皮尔森相关性分析.
主要成果:
- 超过85%的内蒙古地区显示干旱趋势加剧;湿趋势可以忽略不计.
- 气象干旱频繁但短暂;土壤干旱不频繁但严重且持久.
- 土壤水分不足是水文干旱的主要驱动因素,与气象干旱相比,合力更强.
- 干旱传播通常发生在2-6个月内,更高级干旱传播更有效.
结论:
- 土壤水分不足是水文干旱开始的关键因素.
- 干旱传播动态在内蒙古的区域不同.
- 调查结果为区域干旱形成机制和模型开发提供了重要的见解.
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