宋鹏越, 徐宗学, 宋苏林, 李鹏. 城市化进程对汛期降水特征的影响——以济南市为例[J]. 北京师范大学学报(自然科学版). DOI: 10.12202/j.0476-0301.2024056
引用本文: 宋鹏越, 徐宗学, 宋苏林, 李鹏. 城市化进程对汛期降水特征的影响——以济南市为例[J]. 北京师范大学学报(自然科学版). DOI: 10.12202/j.0476-0301.2024056
SONG Pengyue, XU Zongxue, SONG Sulin, LI Peng. Impact of Urbanization on Precipitation Characteristics during Flood Period- A Case Study in Jinan City[J]. Journal of Beijing Normal University(Natural Science). DOI: 10.12202/j.0476-0301.2024056
Citation: SONG Pengyue, XU Zongxue, SONG Sulin, LI Peng. Impact of Urbanization on Precipitation Characteristics during Flood Period- A Case Study in Jinan City[J]. Journal of Beijing Normal University(Natural Science). DOI: 10.12202/j.0476-0301.2024056

城市化进程对汛期降水特征的影响以济南市为例

Impact of Urbanization on Precipitation Characteristics during Flood Period- A Case Study in Jinan City

  • 摘要: 以往多项研究均表明城市化对降水存在影响,但开展不同城市化阶段对研究区降水影响的研究较少.本文以济南市为研究区,结合1985—2022年土地利用变化与降水数据,探讨了城市化过程对汛期降水特征的影响.论文首先分析了研究区历史土地利用变化特征,揭示了增雨系数对不透水率的响应规律;然后定量分析了不透水率对不同等级降水的具体影响对降水的影响程度.结果表明:济南市城市化过程可以分为四个阶段,1995—2000年不透水面积增速最大,平均为114.77 km2·a−1.当不透水率大于26%时,增雨系数将大于1.0;大于43%时将达到1.10;超过60%时将达到1.20.城市化进程随不透水率提高明显促进了小型降雨的发生.

     

    Abstract: Prior multiple studies have shown the impact of urbanization on precipitation, but there is a scarcity of research focusing on the impact of precipitation in the study area at different stages of urbanization.Jinan City was selected as the study area, and the impact of urbanization on precipitation during flood period was investigated by using land use and precipitation data from 1985 to 2022. The characteristics of land use change in the study area was analyzed. Response patterns of rainfall to underlying surface imperviousness was explored. The effects of imperviousness on different precipitation was studied. The findings showed that the urbanization process in Jinan City experienced four stages, with the period from 1995 to 2000 witnessed the most substantial increase in impervious surfaces at an average rate of 114.77 km2/a. When the imperviousness rate exceeded 26%, the rainfall enhancement coefficient was greater than 1.0, and 1.10 when imperiousness exceeded 43%, and potentially 1.20 when imperiousness rate exceeded 60%. The expansion of impervious surfaces notably increased the occurrence of light rainfall.

     

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