不透水面扩张对郑州主城区降水特征的影响
作者:
作者单位:

(1.华北水利水电大学水资源学院,河南 郑州 450046;2.华北水利水电大学校长办公室, 河南 郑州 450046;3.河南省黄河流域水资源节约集约利用重点实验室,河南 郑州 450046)

作者简介:

黄晓东(1987—),男,讲师,博士,主要从事遥感水文研究。E-mail:huangxiaodong@ncwu.edu.cn 通信作者:韩宇平(1975—),男,教授,博士,主要从事水资源管理研究。E-mail:hanyp@ncwu.edu.cn

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中图分类号:

TV125

基金项目:

国家自然科学基金(51679089)


Effects of impervious surface expansion on precipitation characteristics in main urban area of Zhengzhou City
Author:
Affiliation:

(1.College of Water Resources, North China University of Water Resources and Electric Power, Zhengzhou 450046, China;2.President's Office, North China University of Water Resources and Electric Power, Zhengzhou 450046, China;3.Henan Key Laboratory of Water Resources Conservation and Intensive Utilization in the Yellow River Basin, Zhengzhou 450046, China)

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    摘要:

    为探究下垫面变化对高密度城市地区降水的影响,基于遥感技术反演郑州主城区1990—2019年的不透水面分布信息,并分析了其扩张特征;采用回归模型探讨不透水面比例与降水特征变化的相关性,识别了显著影响主城区降水的不透水面比例阈值,并采用城郊对比法多角度揭示了不透水面扩张对主城区降水的影响程度。结果表明:郑州主城区不透水面扩张趋势显著,扩张形态呈单一核心的“摊大饼”式扩张;不透水面比例与城郊降水强度比呈二次多项式函数关系,对主城区降水产生显著影响的阈值是30%;不透水面扩张导致主城区雨岛效应显著,增雨系数最高达1.39,主城区暴雨发生概率高于郊区53%,降水集中期晚于郊区约8d,对主城区主汛期降水量变化的贡献率达44.39%;不透水面因具有高蓄热、低渗透的固有特征,对地表热力、动力条件具有显著影响,已成为城市化影响降水的主要影响因素之一。

    Abstract:

    In order to explore the impact of underlying surface changes on precipitation in high-density urban areas, the distribution information of impervious surface in the main urban area of Zhengzhou City from 1990 to 2019 was estimated based on the remote sensing technology, and the expansion characteristics were analyzed. A regression model was used to explore the correlation between the proportion of impervious surface and the change of precipitation characteristics, and the threshold value of impervious surface proportion significantly affecting precipitation in the main urban area was identified. The effects of impervious surface expansion on precipitation in the main urban area were revealed from multiple angles with the method of comparison between urban and suburban areas. The results show that the impervious surface exhibited a significant expansion trend, like spreading a pie with a single core, in the main urban area of Zhengzhou City. The proportion of impervious surface had a quadratic polynomial function relationship with the ratio of precipitation intensity, and its threshold significantly affecting precipitation in the main urban area was 30%. The impervious surface expansion resulted in a significant rain island effect in the main urban area, and the maximum precipitation enhancement coefficient was 1.39. The probability of rainstorm in the main urban area was 53% higher than that in the suburbs, and the precipitation concentration period was about 8d later than that in the suburbs. The contribution rate of impervious surface expansion to precipitation change in the main flood season was 44.39%. Impervious water surface, with characteristics of high heat storage capacity and low permeability, has a significant impact on surface thermal and dynamic conditions, and has become one of the main factors of urbanization affecting precipitation.

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黄晓东,刘文锴,曹润祥,等.不透水面扩张对郑州主城区降水特征的影响[J].水资源保护,2022,38(6):22-30.(HUANG Xiaodong, LIU Wenkai, CAO Runxiang, et al. Effects of impervious surface expansion on precipitation characteristics in main urban area of Zhengzhou City[J]. Water Resources Protection,2022,38(6):22-30.(in Chinese))

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  • 收稿日期:2021-09-27
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  • 在线发布日期: 2022-11-19
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