| 339 | 1 | 180 |
| 下载次数 | 被引频次 | 阅读次数 |
【目的】为探究青岛市平原区地下水干旱时空特征及对气象干旱的动态响应，【方法】利用2000—2020年20眼监测井逐月地下水位数据及平度站逐月降水数据分别计算标准化地下水指数(SGI)和多尺度的标准化降水指数(SPI),对地下水干旱和气象干旱演变及趋势特征进行分析，并利用Kendall’s秩相关系数定量识别地下水干旱对气象干旱的动态响应关系。【结果】结果显示：研究区地下水与降水都呈现先变湿后变干的趋势，地下水干旱出现时间滞后于气象干旱；地下水干旱对气象干旱的响应时间为30～56个月，整体响应程度较强；春季、夏季、秋季和冬季SGI与SPI-n(n=1,2,…,48)的最大相关系数分别为0.42、0.84、0.65和0.57,地下水干旱对气象干旱在夏、秋的响应程度明显强于春、冬；西南部SGI与SPI-n的相关系数明显小于其他区域。【结论】结果表明：受降水、包气带岩性及地下水开采等因素的影响，研究区地下水干旱及对气象干旱的响应存在时空异质性；从气象干旱到地下水干旱的传播是一个缓慢演化的隐性过程，掌握地下水干旱对气象干旱的时空响应关系，能为地下水干旱的预警和防控提供参考。
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.
[1] SCHWALM C,ANDEREGG W,Michalak A,et al.Global patterns of drought recovery[J].Nature,2017,548:202-205.
[2] 崔素芳，张保祥，荣燕妮，等.基于云模型的山东省干旱时空分布特征[J].南水北调与水利科技(中英文),2023,21(4):679-688.CUI S F,ZHANG B X,RONG Y N,et al.Characteristics of temporal-spatial drought distribution in Shandong Province based on cloud model[J].South-to-North Water Transfers and Water Science & Technology,2023,21(4):679-688.
[3] MISHRA A K,SINGH V P.A review of drought concepts[J].Journal of Hydrology,2010,391(1):202-216.
[4] 汤秋鸿，徐锡蒙，周羽暄，等.全球变化背景下黄河流域水旱灾害演变及应对策略[J].水利发展研究，2025,25(2):13-20.TANG Qiuhong,XU Ximeng,ZHOU Yuxuan,et al.Evolution of floods and droughts in the Yellow River Basin under global change and relevant coping strategies[J].Water Resources Development Research,2025,25(2):13-20.
[5] 智协飞，田云涛，陈昌春，等.干旱传播研究进展与展望Ⅰ:干旱传播含义、特征、类型与研究方法[J].南水北调与水利科技(中英文),2023,21(4):625-653.ZHI X F,TIAN Y T,CHEN C C,et al.Drought propagation:Progress and prospect Ⅰ:The meaning,characteristics,types,and research methods of drought propagation[J].South-to-North Water Transfers and Water Science & Technology,2023,21(4):625-653.
[6] KARTAL V,NONES M.Assessment of meteorological,hydrological and groundwater drought in the Konya closed basin,Türkiye[J].Environmental Earth Sciences,2024,83(9):285.
[7] WOSSENYELEH B K,KASA A,VERBEIREN B,et al.Drought propagation in the hydrological cycle in a semiarid region:a case study in the Bilate catchment,Ethiopia[J].Journal of Hydrology,2022,30:751-766.
[8] 郭伟，李莹，杜莉丽.基于SPI的山西省1972—2012年春夏干旱特征及对玉米产量的影响分析[J].干旱地区农业研究，2018,36(1):230-236.GUO Wei,LI Ying,DU Lili.Characteristic of spring and summer drought variations and its relation with maize yield in Shanxi Province in 1972—2012 based on SPI[J].Agricultural Research in the Arid Areas,2018,36(1):230-236.
[9] BLOOMFIELD J P,MARCHANT B P.Analysis of groundwater drought building on the standardized precipitation index approach[J].Hydrology and Earth System Sciences,2013,17(12):4769-4787.
[10] 艾启阳，粟晓玲，张更喜，等.标准化地下水指数法分析黑河中游地下水时空演变规律[J].农业工程学报，2019,35(10):69-74.AI Qiyang,SU Xiaoling,ZHANG Gengxi,et al.Constructing standardized groundwater index to analyze temporal-spatial evolution of groundwater in middle reaches of Heihe river[J].Transactions of the Chinese Society of Agricultural Engineering,2019,35(10):69-74.
[11] DI N F,GRANATA F.Analysis of trends and abrupt changes in groundwater and meteorological droughts in the United Kingdom.[J].Journal of Hydrology,2024,637(3/4):131430.
[12] THOMAS B F,FAMIGLIETTI J S,LANDERER F W,et al.GRACE groundwater drought index:Evaluation of California Central Valley groundwater drought[J].Remote Sensing of Environment,2017,198:384-392.
[13] WANG F,LAI Hexin,LI Yanbin,et al.Identifying the status of groundwater drought from a GRACE mascon model perspective across China during 2003—2018[J].Agricultural Water Management,2022,260:107251.
[14] ZHAO Y.Quantifying water storage changes and groundwater drought in the Huaihe river basin of chinabased on GRACE data[J].Sustainability,2024,16(19):8437.
[15] KUMAR R,MUSUUZA J L,VAN LOON A F,et al.Multiscale evaluation of the Standardized Precipitation Index as a groundwater drought indicator[J].Hydrology and Earth System Sciences,2016,20(3):1117-1131.
[16] 龚栋栋，高凡，吴彬，等.基于GRACE的新疆平原区地下水干旱时空变化及其对气象干旱的响应[J].干旱区地理，2024,47(9):1496-1507.GONG Dongdong,GAO Fan,WU Bin,et al.Spatial and temporal change of groundwater drought in the Xinjiang plain based on GRACE and its response to meteorological drought[J].Arid Land Geography,2024,47(9):1496-1507.
[17] 粟晓玲，褚江东，张特，等.西北地区地下水干旱时空演变趋势及对气象干旱的动态响应[J].水资源保护，2022,38(1):34-42.SU Xiaoling,CHU Jiangdong,ZHANG Te,et al.Spatio-temporal evolution trend of groundwater drought and its dynamic response to meteorological drought in Northwest China[J].Water Resources Protection,2022,38(1):34-42.
[18] KUBIZ J,BAK B.The reaction of groundwater to several months’ meteorological drought in Poland[J].Polish Journal of Environmental Studies,2019,28(1):187-195.
[19] 崔英杰，魏永富，徐晓民，等.基于标准地下水指数的地下水位动态及其对降水变化的响应[J].科学技术与工程，2020,20(16):6336-6342.CUI Yingjie,WEI Yongfu,XU Xiaomin,et al.Groundwater level dynamics and its response to variations of precipitation based on standardized groundwater index[J].Science Technology and Engineering,2020,20(16):6336-6342.
[20] ZHAO A,XIANG K,ZHANG A,et al.Spatial-temporal evolution of meteorological and groundwater droughts and their relationship in the North China Plain[J].Journal of Hydrology,2022,610:127903.
[21] 杨艺，周恒，王松禄.平度市水资源利用存在问题及对策[J].山东水利，2020,(1):23-24.YANG Yi,ZHOU Heng,WANG Songlu.Problems and countermeasures of water resources utilization in Pingdu City[J].Shandong water Conservancy,2020,(1):23-24.
[22] MCKEE T,DOESKEN N,KLEIST J.Drought monitoring with multipletime scales[C]//American Meteorological Society.Proceedings of the 9th Conference on Applied Climatology.Dallas:American Meteorological Society,1995:233-236.
[23] 甘贝贝，刘梅冰.1962—2021 年闽江流域干湿演变特征及其对 ENSO 事件的响应[J].南水北调与水利科技(中英文),2024,22(3):545-556.GAN B B,LIU M B.Dry-wet evolution characteristics and response to ENSO events in the Minjiang River basin from 1962 to 2021[J].South-to-North Water Transfers and Water Science & Technology,2024,22(3):545-556.
[24] 王洁，李王成，李晨，等.基于SPI指数的宁夏干旱特征[J].南水北调与水利科技(中英文),2021,19(3):528-538.Wang Jie,LI Wangchen,LI Chen,et al.Drought characteristics in Ningxia based on standardized precipitation index[J].South-to-North Water Transfers and Water Science & Technology,2021,19(3):528-538.
[25] MXOLISI B,MUKHAWANA D K,THOKOZANI K,et al.Hydrological drought assessment using the standardized groundwater index and the standardized precipitation index in the Berg River Catchment,South Africa[J].Journal of Hydrology:Regional Studies,2024,53,101779.
[26] 虞畅，金君良，王国庆，等.黄河源区典型流域水文要素演变及其对气候变化的响应[J].南水北调与水利科技(中英文),2024,22(5):845-855.YU C,JIN J L,WANG G Q,et al.Evolution of hydrological elements in typical watersheds of the Yellow River source area and their response to climate change[J].South-to-North Water Transfers and Water Science & Technology,2024,22(5):845-855.
[27] KENDALL M G.Rankcorrelation measures [M].London:Charles Griffin,1975,23(1):254-271.
[28] 张海荣，周建中，曾小凡，等.金沙江流域降水和径流时空演变的非一致性分析[J].水文，2015,35(6):90-96.ZHANG Hairong,ZHOU Jianzhong,ZENG,Xxiaofan,et al.Inconsistency analysis of spatial and temporal evolution of precipitation and runoff in Jinshajiang River Basin[J].Journal of China Hydrology,2015,35(6):90-96.
[29] YUE S,PILON P,PHINNEY B,et al.The influence of autocorrelation on the ability to detect trend in hydrological series[J].Hydrological Processes,2010,16(9):1807-1829.
[30] ROHINI K,MUSUUZA J L,VAN L A F,et al.Multiscale evaluation of the Standardized Precipitation Index as a groundwater drought indicator[J].Hydrology and Earth System Sciences,2016,20(8):1117-1131.
[31] LORENZO-LACR J,GARCIA C,MORAN-TEJEDA E.Groundwater level responses to precipitation variability in mediterranean insular aquifers[J].Journal of Hydrology,2017,552:516-531.
[32] 沈业杰，高磊，彭新华.基于氘盈余分析季节性降水对浅层地下水的补给：以鹰潭孙家农田小流域为例[J].土壤，2015,47(2):394-399.SHEN Yejie,GAO Lei,PENG Xinhua.Evaluation of Shallow Groundwater recharge from seasonal precipitation using deuterium excess method:A case of Sunjia agricultural watershed,Yingtan[J].Soils,2015,47(2):394-399.
[33] 赵振华，罗振江，黄林显，等.基于小波分析的济南西郊地下水位对降雨响应机制研究[J].中国岩溶，2023,42(5):1-9.ZHAO Zhenhua,LUO Zhenjiang,HUANG Linxian,et al.Research on the Response Mechanism of Groundwater Level to Rainfall in Xijiao Region of Jinan Based on Wavelet Analysis [J].Carsologica Sinica,2023,42(5):1-9.
[34] LIU Bo,ZHOU Xiangqian,LI Wei,et al.Spatiotemporal characteristics of groundwater drought and its response to meteorological drought in Jiangsu Province,China[J].Water,2016,8(11):480.
基本信息:
DOI：10.13928/j.cnki.wrahe.2025.10.008
中图分类号:P426.616;P641
引用信息:
[1]肖平,马真臻,张西浩,等.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.DOI:10.13928/j.cnki.wrahe.2025.10.008.
基金信息:
国家重点研发计划(2022YFC3204601); 国家自然科学基金项目(52079143,51609261)
2025-01-21
2025-01-21
2025-01-21