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青岛市平原区地下水干旱特征及对气象干旱的动态响应

肖平 马真臻 张西浩 肖璇 苟淇书 郭梦瑶 林鹏飞

水利水电技术(中英文)2025,Vol.56Issue(10):97-110,14.
水利水电技术(中英文)2025,Vol.56Issue(10):97-110,14.DOI:10.13928/j.cnki.wrahe.2025.10.008

青岛市平原区地下水干旱特征及对气象干旱的动态响应

Groundwater drought characteristics and its dynamic response to meteorological drought in Qingdao plain area

肖平 1马真臻 1张西浩 2肖璇 3苟淇书 4郭梦瑶 5林鹏飞1

作者信息

  • 1. 中国水利水电科学研究院流域水循环模拟与调控国家重点实验室,北京 100038
  • 2. 青岛市水务管理局,山东青岛 266071
  • 3. 青岛市水利勘测设计研究院有限公司,山东青岛 266100
  • 4. 青岛市水文中心,山东青岛 266001
  • 5. 河海大学水利水电学院,江苏南京 210098
  • 折叠

摘要

Abstract

[Objective]To explore the spatiotemporal characteristics of groundwater drought and its dynamic response to meteorological drought in Qingdao plain areas,[Methods]the standardized groundwater index(SGI)and standardized precipitation index(SPI)at the multi-scale were calculated using monthly groundwater level data from 20 monitoring wells and monthly precipitation data from Pingdu Station from 2000 to 2020.The evolution and trend characteristics of groundwater drought and meteorological drought were analyzed,and Kendall's rank correlation coefficient was used to quantitatively identify the dynamic response relationship between groundwater drought and meteorological drought.[Results]The result indicate that both groundwater and precipitation in the study area tend to become wet first and then dry,and the occurrence time of groundwater drought is later than that of meteorological drought.The response time of groundwater drought to meteorological drought is 30~56 months,and the overall response degree is strong.The maximum correlation coefficients between SGI and SPI-n(n=1,2,…48)in spring,summer,autumn,and winter were 0.42,0.84,0.65,and 0.57,respectively.The response degree of groundwater drought to meteorological drought was significantly stronger in summer and autumn than in spring and winter.The correlation coefficient between SGI and SPI-n in the southwest is significantly lower than in other regions.[Conclusion]The result reveal that there is spatiotemporal heterogeneity in groundwater drought and its response to meteorological drought in the study area,influenced by factors such as precipitation,lithology of the aquifer,and groundwater exploitation.The propagation from meteorological drought to groundwater drought is a slowly evolving implicit process.Understanding the spatiotemporal response relationship between groundwater drought and meteorological drought can provide reference for the early warning and prevention of groundwater drought.

关键词

地下水干旱/气象干旱/标准化地下水指数/标准化降水指数/动态响应/水资源/时空变化

Key words

groundwater drought/meteorological drought/standardized groundwater index/standardized precipitation index/dynamic response/water resources/spatiotemporal changes

分类

地质学

引用本文复制引用

肖平,马真臻,张西浩,肖璇,苟淇书,郭梦瑶,林鹏飞..青岛市平原区地下水干旱特征及对气象干旱的动态响应[J].水利水电技术(中英文),2025,56(10):97-110,14.

基金项目

国家重点研发计划(2022YFC3204601) (2022YFC3204601)

国家自然科学基金项目(52079143,51609261) (52079143,51609261)

水利水电技术(中英文)

OA北大核心

1000-0860

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