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黄土高原不同水平年旱涝时空分布特征

吴歌 符素华 殷兵

吴歌,符素华,殷兵.黄土高原不同水平年旱涝时空分布特征[J].农业工程,2022,12(7):65-71. doi: 10.19998/j.cnki.2095-1795.2022.07.013
引用本文: 吴歌,符素华,殷兵.黄土高原不同水平年旱涝时空分布特征[J].农业工程,2022,12(7):65-71. doi: 10.19998/j.cnki.2095-1795.2022.07.013
WU Ge,FU Suhua,YIN Bing.Spatial and temporal distribution of drought and flood in Loess Plateau in different hydrological years[J].Agricultural Engineering,2022,12(7):65-71. doi: 10.19998/j.cnki.2095-1795.2022.07.013
Citation: WU Ge,FU Suhua,YIN Bing.Spatial and temporal distribution of drought and flood in Loess Plateau in different hydrological years[J].Agricultural Engineering,2022,12(7):65-71. doi: 10.19998/j.cnki.2095-1795.2022.07.013

黄土高原不同水平年旱涝时空分布特征

doi: 10.19998/j.cnki.2095-1795.2022.07.013
基金项目: 国家自然科学基金重点项目(42130701);国家重点研发计划项目(2017YFD0800502)
详细信息
    作者简介:

    吴歌,博士生,主要从事土壤侵蚀与水土保持研究 E-mail:812537224@qq.com

    符素华,通信作者,博士,教授,博士生导师,主要从事土壤侵蚀机理研究 E-mail:suhua@bnu.edu.cn

  • 中图分类号: S27

Spatial and Temporal Distribution of Drought and Flood in Loess Plateau in Different Hydrological Years

  • 摘要:

    全球气候变暖大背景下,黄土高原总体呈现暖干化趋势,未来干旱还可能会加剧。为了全面了解黄土高原旱涝时空变化特征,为黄土高原应对旱涝灾害提供决策依据,根据黄土高原及周边263个气象站的降水数据划分降水水平年,以标准化降水指数(SPI)为指标,分析了黄土高原地区不同水平年年际及年内旱涝特征。结果显示,黄土高原在丰、平、枯水年均有不同程度的干旱发生。丰水年黄土高原干旱面积占5.7%,雨涝面积占40.9%;平水年干旱面积占12.7%,雨涝面积占19.3%;枯水年干旱面积占44.4%,雨涝面积占17.9%。不同水平年的干旱区域存在差异。不同水平年内春旱较重,丰水年和平水年雨季开始后干旱逐渐缓解,枯水年雨季不能有效缓解春季以来的干旱,且秋涝明显,各水平年年内干旱的时空分布存在显著差异。不同水平年年际和年内旱涝差异大且变化频繁,为了确保黄土高原农业生产旱涝保收,应合理布设小型水利工程与田间灌溉设施。

     

  • 图 1  不同水平年干旱面积比例和持续时间

    Figure 1.  Drought area and duration in different hydrological years

    图 2  不同资料序列确定的典型水平年年降水量

    Figure 2.  Annual rainfall determined by different data source

    表  1  SPI等级划分

    Table  1.   SPI classification

    旱/涝等级特旱重旱中旱轻旱正常轻涝中涝重涝特涝
    SPI≤−2.0(−2.0, −1.5](−1.5, −1.0](−1.0, −0.5](−0.5, 0.5)[0.5, 1.0)[1.0, 1.5)[1.5, 2.0)≥2.0
    下载: 导出CSV
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  • 收稿日期:  2021-10-27
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