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陕甘宁地区降水稳定同位素特征及水汽来源
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  • 英文篇名:Stable isotopes characteristics of precipitation over Shaanxi-Gansu-Ningxia and its water vapor sources
  • 作者:刘洁遥 ; 张福平 ; 冯起 ; 魏永芬 ; 黄良红 ; 李宗省 ; 聂硕 ; 李玲
  • 英文作者:LIU Jie-yao;ZHANG Fu-ping;FENG Qi;WEI Yong-fen;HUANG Liang-hong;LI Zong-xing;NIE Shuo;LI Ling;School of Geography and Tourism, Shaanxi Normal University;National Demonstration Center for Experimental Geography Education, Shaanxi Normal University;Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences;River Basin Research Center, Gifu University;Taiyuan Air Traffic Management Center,Civil Aviation Administration of China;
  • 关键词:降水 ; 稳定同位素 ; 同位素效应 ; 气团轨迹 ; 陕甘宁地区
  • 英文关键词:precipitation;;stable isotope;;isotope effect;;water vapor trajectory;;Shaanxi-Gansu-Ningxia region
  • 中文刊名:应用生态学报
  • 英文刊名:Chinese Journal of Applied Ecology
  • 机构:陕西师范大学地理科学与旅游学院;陕西师范大学地理学国家级实验教学示范中心;中国科学院寒区旱区环境与工程研究所;日本国立岐阜大学流域圈科学研究中心;中国民用航空太原空中交通管理中心;
  • 出版日期:2019-05-27 17:06
  • 出版单位:应用生态学报
  • 年:2019
  • 期:07
  • 基金:陕西省自然科学基金面上项目(2018JM4020);; 国家重点研发计划项目(2017YFC0404300);; 中国科学院前沿科学重点研究项目(QYZDJSSW-DQC031)资助~~
  • 语种:中文;
  • 页:57-66
  • 页数:10
  • CN:21-1253/Q
  • ISSN:1001-9332
  • 分类号:P426
摘要
依据全球大气降水稳定同位素观测网络(GNIP)和已有研究中陕甘宁地区的大气降水氢氧稳定同位素资料,并结合相关气象数据,分析了陕甘宁地区大气降水氧稳定同位素的时空分布特征及其影响因子,并建立了大气降水线方程.结果表明:3省大气降水线的斜率、截距由小到大依次为:甘肃、陕西、宁夏,且均小于全球大气降水线方程的斜率、截距,表明3省的降水过程受蒸发作用影响程度沿宁夏、陕西、甘肃增强;陕甘宁地区大气降水中δ~(18)O值在时间变化上,表现为夏秋季节富集、冬春季节贫化,从空间分布来看,由西北至东南,加权平均δ~(18)O值呈减小趋势;3省降水中δ~(18)O温度效应显著,但不存在降水量效应,这体现了中高纬度大陆性气候的特征;高程效应的定量关系为-0.12‰·(100 m)~(-1),纬度效应更显著(纬度每增加1°,降水中δ~(18)O相应贫化0.27‰);采用HYSPLIT模型对各站点的水汽来源进行追踪,气团聚类轨迹表明,夏半年主要有来自孟加拉湾的水汽、东南季风水汽和西风带水汽,冬半年以西风带水汽为主.
        Based on hydrogen and oxygen stable isotopes in precipitation and meteorological data over Shaanxi-Gansu-Ningxia provided by the Global Network of Isotopes in Precipitation(GNIP) and in previous literature, the spatial and temporal variations of oxygen stable isotopes in precipitation and their driving factors were analyzed, the local meteoric water line(LMWL) functions were established. The results showed that the slope and intercept of the LMWL changed in the order of Gansu
引文
[1] Li X-F (李小飞),Zhang M-J (张明军),Li Y-J (李亚举),et al.Characteristics of δ18O in precipitation and moisture transports over the arid region in Northwest China.Environmental Science (环境科学),2012,33(3):711-719 (in Chinese)
    [2] Liu J-R (柳鉴容),Song X-F (宋献方),Yuan G-F (袁国富),et al.Characteristics of δ18O in precipitation over Northwest China and its water vapor sources.Acta Geogrephica Sinica (地理学报),2008,63(1):12-22 (in Chinese)
    [3] Dansgaard W.Stable isotopes in precipitation.Tellus,1964,6:436-468
    [4] Araguás-Araguás L,Froehlich K,Rozanski K.Stable isotope composition of precipitation over Southeast Asia.Journal of Geophysical Research,1998,103:28721-28742
    [5] Dansgaard W.The abundance of δ18O in atmospheric water and water vapour.Tellus,1953,5:461-469
    [6] Zhang X-P (章新平),Yao T-D (姚檀栋).World spatial characteristics of oxygen isotope ratio in precipita-tion.Journal of Glaciology and Geocryology (冰川冻土),1994,16(3):202-210 (in Chinese)
    [7] Song X-F (宋献方),Liu J-R (柳鉴容),Sun X-M (孙晓敏),et al.Establishment of Chinese network of isotopes in precipitation (CHNIP) based on CERN.Advances in Earth Science (地球科学进展),2007,22(7):738-747 (in Chinese)
    [8] Zhu J-J (朱建佳),Chen H (陈辉),Gong G-L (巩国丽),et al.Hydrogen and oxygen isotopic compositions of precipitation and its water vapor sources in Eas-tern Qaidam basin.Environmental Science (环境科学),2015,36(8):2784-2790 (in Chinese)
    [9] Zhao S-K (赵诗坤),Pang S-G (庞朔光),Wen R (文蓉),et al.Influence of below-cloud secondary evaporation on stable isotope compositionin precipitation in the Haihe River Basin,China.Progress in Geography (地理科学进展),2015,34(8):1031-1038 (in Chinese)
    [10] Wu J-K (吴锦奎),Yang Q-Y (杨淇越),Ding Y-J (丁永健),et al.Variations and simulation of stable isotopes in precipitation in the Heihe River basin.Environmental Science (环境科学),2011,32(7):1857-1866 (in Chinese)
    [11] Chen Y-T (陈衍婷),Du W-J (杜文娇),Chen J-S (陈进生),et al.Composition of hydrogen and oxygen isotopic of precipitation and source apportionment of water vapor in Xiamen Area.Acta Scientiae Circumstan-tiae (环境科学),2016,36(2):667-674 (in Chinese)
    [12] He J-Q (贺建桥),Zhang W (张伟),Zhou J (周剑),et al.The impact of mountain range orientation on the lapse rate of precipitation δ18O in the upper reaches of the Heihe River Basin in the Qilian Mountains.Journal of Glaciology and Geocryology (冰川冻土),2016,38(2):359-367 (in Chinese)
    [13] Fan J-Z (范建忠),Li D-K (李登科),Gao M-S (高茂盛).Spatio-temporal variations of evapotranspiration in Shaanxi Province using MOD16 products.Ecology and Environmental Sciences (生态环境学报),2014,23(9):1536-1543 (in Chinese)
    [14] Liu C-Y (刘春雨),Dong X-F (董晓峰),Liu Y-Y (刘英英),et al.Spatial differences of net primary productivity in Gansu Province.China Population,Resources and Environment (中国人口·资源与环境),2014,24(1):163-170 (in Chinese)
    [15] Gao Y (高阳),Jin J-W (金晶炜),Cheng J-M (程积民),et al.Carbon sequestration status of forest ecosystems in Ningxia Hui Autonomous Region.Chinese Journal of Applied Ecology (应用生态学报),2014,25(3):639-646 (in Chinese)
    [16] Yan J-H (闫军辉),Liu D-M (刘冬梅),Yan J-P (延军平).The spatial structure of climate change in Shaanxi-Gansu-Ningxia region.Journal of Arid Land Resources and Environment (干旱区资源与环境),2009,23(9):67-71 (in Chinese)
    [17] Li S-S (李双双),Yan J-P (延军平),Wan J (万佳).The spatial-temporal changes of vegetation restoration on Loess Plateau in Shaanxi-Gansu-Ningxia region.Acta Geogrephica Sinica (地理学报),2012,67(7):960-970 (in Chinese)
    [18] Wang X-D (王晓东).Climate change in Shaanxi-Gan-Ning area and its impacts analysis.Arid Land Geography (干旱区地理),2004,27(1):25-28 (in Chinese)
    [19] Liu J-Y (刘洁遥),Zhang F-P (张福平),Feng Q (冯起),et al.Influence of below-cloud secondary evaporation on stable isotope composition in precipitation in Northwest China.Chinese Journal of Applied Ecology (应用生态学报),2018,29(5):1479-1488 (in Chinese)
    [20] Tian C (田超),Meng P (孟平),Zhang J-S (张劲松),et al.Seasonal characteristics of δD and δ18 O in precipitation and its water vapor sources in the Xiaolangdi Reservoir area of Yellow River,China.Chinese Journal of Applied Ecology (应用生态学报),2015,26(12):3579-3587 (in Chinese)
    [21] Zhang Y-M (郑琰明),Zhong W (钟巍),Peng X-Y (彭晓莹),et al.Correlation of δ18 O in precipitation and moisture sources at Yunfu,western Guangdong Province,China.Environmental Science (环境科学),2009,30(3):637-643 (in Chinese)
    [22] Zhang Y-H (张应华),Wu Y-Q (仵彦卿),Wen X-H (温小虎),et al.Application of environmental isotopes in water cycle.Advances in Water Science (水科学进展),2006,17(5):738-747 (in Chinese)
    [23] Zhang M-J (张明军),Ma Q (马潜),Li Y-J (李亚举),et al.Research of isotopic characteristic in precipitation and water vapor origin at the edge of monsoon region:A case study of Lanzhou City.Journal of Northwest Normal University (Natural Science) (西北师范大学学报:自然科学版),2011,47(6):80-86 (in Chinese)
    [24] Zheng S-H (郑淑蕙),Hou F-G (侯发高),Ni B-L (倪葆龄).Studies on stable deuterium and oxygen-18 isotope composition of precipitation in China.Chinese Science Bulletin (科学通报),1983,28(13):801-806 (in Chinese)
    [25] Li X-F (李小飞),Zhang M-J (张明军),Wang S-J (王圣杰),et al.Spatial and temporal variations of hydrogen and oxygen isotopes in precipitation in Yellow River Basin and its environmental significance.Acta Geologica Sinica (地质学报),2013,87(2):269-277 (in Chinese)
    [26] Huang J-Z (黄锦忠),Tan H-B (谭红兵),Wang R-A (王若安),et al.Hydrogen and oxygen isotopic analysis of perennial meteoric water in Northwest China.Journal of China Hydrology (水文),2015,35(1):33-50 (in Chinese)
    [27] Wang K-L (王可丽),Jiang H (江灏),Zhao H-Y (赵红岩).Atmospheric water vapor transport from westerly and monsoon over the northwest China.Advances in Water Science (水科学进展),2005,16(3):432-438 (in Chinese)
    [28] Li X-F (李小飞),Zhang M-J (张明军),Ma Q (马潜),et al.Characteristics of stable isotopes in precipitation over Northwest China and its water vapor sources.Environmental Science (环境科学),2012,33(9):2924-2931 (in Chinese)
    [29] Liu JR,Song XF,Yuan GF,et al.Characteristics of δ18O in precipitation over eastern monsoon China and the water vapor sources.Chinese Science Bulletin,2010,55:200-211
    [30] Wei K-Q (卫克勤),Lin R-F (林瑞芬).The influence of the monsoon climate on the isotopic composition of precipitation in China.Geochimica (地球化学学报),1994,23(1):33-41 (in Chinese)
    [31] Li J-F (李佳芳),Shi P-J (石培基),Zhu G-F (朱国锋),et al.Characteristics of δ18O in precipitation and moisture transports in the central Hexi Corridor.Acta Scientiae Circumstantiae (环境科学学报),2015,35(4):947-955 (in Chinese)
    [32] Zhang X-P (章新平),Yao T-D (姚檀栋).Distributional features of δ18O in precipitation in China.Acta Geogrephica Sinica (地理学报),1998,53(4):356-363 (in Chinese)
    [33] Kohn MJ,Welker JM.On the temperature correlation of δ18O in modern precipitation.Earth and Planetary Science Letters,2005,231:87-96
    [34] Yu WS,Yao TD,Tian LD,et al.Relationships between δ18O in precipitation and air temperature and moisture origin on a south-north transect of the Tibetan Plateau.Atmospheric Research,2008,87:158-169
    [35] Liu Z-F (刘忠方),Tian L-D (田立德),Yao T-D (姚檀栋),et al.Spatial distribution of δ18O in precipitation over China.Chinese Science Bulletin (科学通报),2009,54(6):804-811 (in Chinese)
    [36] Hu K (胡可),Chen H-S (陈洪松),Nie Y-P (聂云鹏),et al.Characteristics of seasonal variation of deuterium and oxygen-18 isotope composition of precipitation in karst peak-cluster depression area,northwest Guangxi of China.Transactions of the Chinese Society of Agricultural Engineering (农业工程学报),2013,29(5):53-62 (in Chinese)
    [37] Zhang X-P (章新平),Liu J-M (刘晶淼),Masayoshi Nakawo (中尾正义),et al.Vapor origins revealed by deuterium excess in precipitation in southwest China.Journal of Glaciology and Geocryology (冰川冻土),2009,31(4):613-619 (in Chinese)
    [38] Peng TR,Wang CH,Huang CC,et al.Stable isotopic characteristic of Taiwan’s precipitation:A case study of western Pacific monsoon region.Earth and Planetary Science Letters,2010,289:357-366

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