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黄淮海地区2003-2014年GRACE水储量时空变化
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  • 英文篇名:Temporal and spatial variation of water storage in Huang-Huai-Hai area during 2003-2014 based on GRACE satellite data
  • 作者:束美珍 ; 杨传国 ; 李玉龙 ; 程雨春 ; 司巧灵
  • 英文作者:SHU Meizhen;YANG Chuanguo;LI Yulong;CHENG Yuchun;SI Qiaoling;College of Hydrology and Water Resources,Hohai University;State Key Laboratory of Hydro-Water Resources and Hydraulic Engineering,Hohai University;Hebei Institute of Environmental Geology Exploration;
  • 关键词:GRACE ; 黄淮海地区 ; 水储量 ; 时空变化 ; 降雨量
  • 英文关键词:GRACE;;Huang-Huai-Hai area;;water storage;;temporal and spatial variation;;precipitation
  • 中文刊名:NSBD
  • 英文刊名:South-to-North Water Transfers and Water Science & Technology
  • 机构:河海大学水文与水资源学院;河海大学水文水资源与水利工程科学国家重点实验室;河北省环境地质勘察院;
  • 出版日期:2018-01-22 17:00
  • 出版单位:南水北调与水利科技
  • 年:2018
  • 期:v.16;No.94
  • 基金:国家重点研发计划“水资源高效开发利用”专项(2016YFC0402706);; 国家自然科学基金项目(41471016);; 公益性行业(气象)科研专项项目(GYHY201406021)~~
  • 语种:中文;
  • 页:NSBD201801015
  • 页数:6
  • CN:01
  • ISSN:13-1334/TV
  • 分类号:99-104
摘要
利用2003-2014年GRACE时变重力场数据反演黄淮海地区水储量变化,并与同期降水数据比较,分析其年际与年内变化特征,结果表明:时间上,2003-2014年黄淮海地区水储量呈现下降趋势,下降速率约0.42mm/月,其子流域海河和淮河流域下降速率分别为0.52mm/月和0.28mm/月;年内仅2月、9月和12月水储量盈余,9月水储量最大,为9.86mm,6月水储量达到最大盈亏量,约56.65mm;空间上,水储量变化整体上由南往北递减,海河流域水储量较淮河流域亏损严重,但随季节变化水储量亏损状态由南向北得到缓解,到冬季水储量呈现盈余;水储量空间变化主要受降雨影响,同时还受区域农业布局和作物灌溉影响。GRACE数据可为黄淮海地区水储量变化研究带来便利,为区域水资源的科学管理和规划提供依据。
        We obtained the variation of water storage in Huang-Huai-Hai area from 2003 to 2014 by using the monthly gravity field data from GRACE satellite data.Then we compared it with the precipitation data in the same period to analyze its interannual and annual temporal and spatial variation characteristics.The results indicated that:temporally,the water storage in the Huang-Huai-Hai area decreased by 0.42 mm/month in 2003-2014,and that in Haihe and Huaihe river sub-basins decreased by0.52 mm/month and 0.28 mm/month respectively.Within a year,the water storage was in surplus only in February,September and December,reaching the maximum in September to 9.86 mm;the maximum water deficit occurred in June at 56.65 mm.Spatially,the water storage decreased from south to north.The water deficit in Haihe river basin was more serious than that in Huaihe river basin.But as the season changes,the water deficit was relieved from south to north,and switched to surplus in winter.The spatial variation of water storage was mainly affected by precipitation,and also affected by regional agricultural layout and crop irrigation.GRACE data can facilitate the study of water storage variation in the Huang-Huai-Hai area and can provide basis for the scientific management and planning of regional water resources.
引文
[1]CHEN J L,WILSON C R,TAPLEY B D,et al.2005drought event in the Amazon River basin as measured by GRACE and estimated by climate models[J].Journal of Geophysical Research(Solid Earth),2009,114(B5).DOI:10.1029/2008JB006056.
    [2]许民,叶柏生,赵求东.2002-2010年长江流域GRACE水储量时空变化特征[J].地理科学进展,2013,32(1):68-77.(XU M,YE B S,ZHAO Q D.Temporal and spatial pattern of water storage changes over the Yangtz river basin during 2002-2010based on GRACE satellite data[J].Progress in Geography,2013,32(1):68-77.(in Chinese))DOI:10.3724/SP.J.1033.2013.00068.
    [3]尼胜楠,陈剑利,李进,等.利用GRACE卫星时变重力场监测长江、黄河流域水储量变化[J].大地测量与地球动力学,2014,34(4):49-55.(NI S N,CHEN J L,LI J,et al.Terrestrial water storage change in the Yangtze and Yellow river basins from GRACE time-variable gravity measurements[J].Journal of Geodesy and Geodynamics,2014,34(4):49-55.(in Chinese))
    [4]冯伟,Lemoine J M,钟敏,等.利用重力卫星GRACE监测亚马逊流域2002-2010年的陆地水变化[J].地球物理学报,2012,55(3):814-821.(FENG W,LEMOINE J M,ZHONG M,et al.Terrestrial water storage changes in the Amazon basin measured by GRACE during 2002-2010[J].Chinese Journal of Geophysics,2012,55(3):814-821.(in Chinese))DOI:10.6038/j.issn.0001-5733.2012.03.011.
    [5]王文,王鹏,崔巍.长江流域陆地水储量与多源水文数据对比分析[J].水科学进展,2015,26(6):759-768.(WANG W,WANG P,CUI W.A comparison of terrestrial water storage data and multiple hydrological data in the Yangtze river basin[J].Advances in Water Science,2015,26(6):759-768.(in Chinese))DOI:10.14042/j.cnki.32.1309.2015.06.001.
    [6]胡小工,陈剑利,周永宏,等.利用GRACE空间重力测量监测长江流域水储量的季节性变化[J].中国科学(D辑),2006,36(3):225-232.(HU X G,CHEN J L,ZHOU Y H,et al.Monitoring the seasonal water storage changes in Yangtze River basin with GRACE spatial gravimetric measurements[J].Science in China(Series D),2006,36(3):225-232.(in Chinese))DOI:10.3321/j.issn:1006-9267.2006.03.003.
    [7]许朋琨,张万昌.GRACE反演近年青藏高原及雅鲁藏布江流域陆地水储量变化[J].水资源与水工程学报,2013(1):23-29.(XU P K,ZHANG W C.Inversion of terrestrial water storage changes in recent years for Qinghai-Tibetan plateau and Yarlung Zangbo River basin by GRACE[J].Journal of Water Resources and Water Engineering,2013(1):23-29.(in Chinese))
    [8]SCHMIDT R,SCHWINTZE R P,FLECHTNE R F,et al.GRACE observations of changes in continental water storage[J].Global and Planetary Change,2006,50(1):112-126.DOI:10.1016/j.gloplacha.2004.11.018.
    [9]CHEN J L,WILSON C R,FAMIGLIETTI J S,et al.Attenuation effect on seasonal basin-scale water storage changes from GRACE time-variable gravity[J].Journal of Geodesy,2007,81:237-245.DOI:10.1007/s00190-006-0104-2.
    [10]杨元德,鄂栋臣,晁定波,等.GRACE估算陆地水储量季节和年际变化[J].地球物理学报,2009(12):2987-2992.(YANG Y D,E D C,CHAO D B,et al.Seasonal and inter-annual change in land water storage from GRACE[J].Chinese Journal of Geophysics,2009(12):2987-2992.(in Chinese))DOI:10.3969/j.issn.0001-5733.2009.12.007.
    [11]范云峰.GRACE重力卫星在陆地水储量变化监测中的应用[J].全球定位系统,2013,38(5):83-86.(FAN Y F.Application of GRACE satellite gravity changes in land water storage monitoring[J].GNSS World of China,2013,38(5):83-86.(in Chinese))DOI:10.3969/j.issn.1008-9268.2013.05.018.
    [12]曹艳萍,南卓铜,胡兴林.利用GRACE重力卫星数据反演黑河流域地下水变化[J].冰川冻土,2012,34(3):680-689.(CAO Y P,NAN Z T,HU X L.Changes of groundwater storage in the Heihe River basin derived from GRACE gravity satellite data[J].Journal of Glaciology and Geocryology,2012,34(3):680-689.(in Chinese))
    [13]王杰,黄英,曹艳萍,等.利用GRACE重力卫星观测研究近7年云南省水储量变化[J].节水灌溉,2012(5):1-5.(WANG J,HUANG Y,CAO Y P,et al.Spatial and temporal variation of water storage in recent seven years from GRACE in Yunnan Province[J].Water Saving Irrigation,2012(5):1-5.(in Chinese))
    [14]胡春胜,张喜英,程一松,等.太行山前平原地下水动态及超采原因分析[J].农业系统科学与综合研究,2002,18(2):89-91.(HU C S,ZHANG X Y,CHENG Y S,et al.An analysis on dynamics of water table and overdraft of groundwater in the piedmont of Mt.Taihang[J].System Sciences and Comprehensive Studies in Agriculture,2002,18(2):89-91.(in Chinese))DOI:10.3969/j.issn.1001-0068.2002.02.003.
    [15]YANG Y H,TIAN F.Abrupt change of runoff and its major driving factors in Haihe River Catchment,China[J].Journal of Hydrology,2009,3(4):373-383.DOI:10.1016/j.jhydrol.2009.06.040.
    [16]YI S,SUN W,FENG W,et al.Anthropogenic and climatedriven water depletion in Asia[J].Geophysical Research Letters,2016,43(17):9061-9069.DOI:10.1002/2016GL069985.
    [17]任永强,潘云,宫辉力.海河流域地下水储量时变趋势分析[J].首都师范大学学报(自然科学版),2013,(4):88-94.(REN Y Q,PAN Y,GONG H L.Haihe basin groundwater reserves time-varying trends analysis[J].Journal of Capital Normal University(Natural Science Edition),2013,(4):88-94.(in Chinese))DOI:10.3969/j.issn.1004-9398.2013.04.020.
    [18]苏晓莉,平劲松,叶其欣.GRACE卫星重力观测揭示华北地区陆地水量变化[J].中国科学(地球科学),2012,42(6):917-922.(SU X L,PING J S,YE Q X.Terrestrial water variations in the North China Plain revealed by the GRACE mission[J].Scientia Sinica(Terrae),2012,42(6):917-922.(in Chinese))
    [19]王超,杨涛.重力卫星监测的中国陆地水资源储量时空变化特征[J].水电能源科学,2013,31(7):20-23.(WANG C,YANG T.Spatial-temporal characteristics of terrestrial water storage variations in China based on GRACE satellite data[J].Water Resources and Power,2013,7(31):20-23.(in Chinese))
    [20]ZHONG M,DUAN J B,XU H Z,et al.Trend of China land water storage redistribution at medi-and large-spatial scales in recent five years by satellite gravity observations[J].Chinese Science Bulletin,2009,54(5):816-821.DOI:10.1007/s11434-008-0556-2.
    [21]BETTADPUR S.Level-2gravity field product user handbook[M].Austin:Center for Space Research,2007:18-21.
    [22]吴利平,詹军,田军锋.基于GRACE卫星重力测量资料监测中国大陆及邻区陆地水储量变化[J].科技咨询,2009(19):6-8.(WU L P,ZHAN J,TIAN J F.Monitoring the land water storage change in Chinese mainland and its adjacent areas based on GRACE satellite gravity measurement data[J].Science and Technology Information,2009(19):6-8.(in Chinese))DOI:10.3969/j.issn.1672-3791.2009.19.004.
    [23]石建省,李国敏,梁杏,等.华北平原地下水演变机制与调控[J].地球学报,2014,35(5):527-534.(SHI J S,LI G M,LIANG X,et al.Evolution mechanism and control of groundwater in the north China plain[J].Acta Geoscientica Sinica,2014,35(5):527-534.(in Chinese))DOI:10.3975/cagsb.2014.05.01.
    [24]贾绍凤,李媛媛,吕爱锋,等.海河流域平原区浅层地下水超采量估算[J].南水北调与水利科技,2016(4):1-7,71.(JIA S F,LI Y Y,LYU A F,et al.Estimation of excess pumping of shallow groundwater aquifer in Haihe plain[J].South-toNorth Water Transfers and Water Science&Technology,2016(4):1-7,71.(in Chinese))DOI:10.13476/j.cnki.nsbdqk.2016.04.001.
    [25]房全孝,王建林,于舜章.华北平原小麦-玉米两熟制节水潜力与灌溉对策[J].农业工程学报,2011,27(7):37-44.(FANG Q X,WANG J L,YU S Z.Water-saving potential and irrigation strategies for wheat-maize double cropping system in the North China Plain[J].Transactions of the Chinese Society of Agricultural Engineering,2011,27(7):37-44.(in Chinese))DOI:10.3969/j.issn.1002-6819.2011.07.007.
    [26]SYED T H,FAMIGLIETTI J S,RODELL M,et al.Analysis of terrestrial water storage changes from GRACE and GLDAS[J].Water Resources Research,2008,44(W024332).DOI:10.1029/2006WR005779.

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