用户名: 密码: 验证码:
基于树轮宽度的澜沧江源区干旱重建
详细信息    查看全文 | 推荐本文 |
  • 英文篇名:Drought Reconstruction Based on Tree-Ring Width in Headwaters of the Lancang River
  • 作者:黄小梅 ; 肖丁木 ; 秦宁生
  • 英文作者:HUANG Xiao-mei;XIAO Ding-mu;QIN Ning-sheng;Chengdu Institute of Plateau Meteorology,CMA/Sichuan Provincial Key Laboratory for Heavy Rain and Drought-Flood Disasters in Plateau and Basin;Sichuan Provincial Meteorological Observatory;Sichuan Provincial Climate Center;
  • 关键词:澜沧江源区 ; 树轮宽度 ; SPEI重建
  • 英文关键词:Lancang River;;tree-ring width;;SPEI reconstruction
  • 中文刊名:GHQJ
  • 英文刊名:Arid Zone Research
  • 机构:中国气象局成都高原气象研究所/高原与盆地暴雨旱涝灾害四川省重点实验室;四川省气象台;四川省气候中心;
  • 出版日期:2019-01-15 18:59
  • 出版单位:干旱区研究
  • 年:2019
  • 期:v.36
  • 基金:国家自然科学基金(41772173);; 中国沙漠气象科学研究基金(Sqj2016002)
  • 语种:中文;
  • 页:GHQJ201902002
  • 页数:10
  • CN:02
  • ISSN:65-1095/X
  • 分类号:15-24
摘要
依据采自青海省杂多县昂赛乡的树轮样本,建立树轮宽度差值年表(RES)。相关普查表明,澜沧江源区6—7月平均的12个月时间尺度标准化降水蒸散指数(SPEI)与RES年表具有显著的正相关。利用RES年表重建了澜沧江源区1639—2013年6—7月平均的SPEI变化序列,重建方程方差解释量达到37. 4%,且经过交叉检验证明了方程的稳定性。重建序列展示了澜沧江源区干旱的长期变化情况,发现1694—1710、1753—1778、1830—1847、1862—1872、1892—1908、1919—1929、1978—1989年共7个偏湿阶段和1646—1673、1682—1693、1711—1731、1735—1752、1796—1809、1817—1829、1848—1861、1873—1886、1949—1959、1990—2000年10个偏干阶段。重建的SPEI序列存在30~64、19~21、4. 2~4. 3、2. 6~3. 2、2. 5 a和2. 2 a左右的显著变化周期。相关分析表明,赤道中东太平洋海温对澜沧江源区干湿变化具有显著影响。此外,澜沧江源区干湿变化可能与厄尔尼诺-南方涛动(EN-SO)、太平洋年代际振荡(PDO)、太阳活动等大尺度的气候驱动因子存在一定的联系。此次SPEI重建为澜沧江源区提供了长期干旱变化历史,可为该区水资源管理提供科学依据。
        Tree-ring width residual chronology( RES) was developed from the tree-ring samples collected in Angsai Township,Zaduo County,Qinghai Province. The results of general survey showed that there was a high correlation between the tree-ring width chronology and the SPEI( June-July) at 12-month time scale. The June-July SPEI in the headwaters of the Lancang River was reconstructed from AD 1639 to 2013,and it was used to explain the 37. 4% of the total SPEI variance during their common period. The cross-validation revealed that the reconstructed equation was stable. The results showed that the relatively wet periods occurred during 1694-1710,1753-1778,1830-1847,1862-1872,1892-1908,1919-1929 and 1978-1989,and the relatively dry periods occurred during 1646-1673,1682-1693,1711-1731,1735-1752,1796-1809,1817-1829,1848-1861,1873-1886,1949-1959 and 1990-2000,respectively. The reconstructed SPEI series revealed that there were the significant variation periods of 30-64,19-21,4. 2-4. 3,2. 6-3. 2,2. 5 and 2. 2 years. Correlation analysis showed that the sea surface temperature in the middle-east equator Pacific Ocean affected significantly the dry-wet changes in the headwaters of the Lancang River. Our reconstruction was associated with the large-scale atmospheric-oceanic variability,such as the ElNio-Southern Oscillation( ENSO),Pacific Decadal Oscillation( PDO) and solar activity. This SPEI reconstruction could provide a long-term drought history in the headwaters of the Lancang River and serve as the scientific basis for water resources management in this semiarid region.
引文
[1]吕爱锋,贾绍凤,燕华云,等.三江源地区融雪径流时间变化特征与趋势分析[J].资源科学,2009,31(10):1 704-1 709.[LüAifeng,Jia Shaofeng,Yan Huayun,et al.Temporal variations and trend analysis of the snowmelt runoff timing across the source regions of the Yangtze River,Yellow River and Lancang River[J].Resources Science,2009,31(10):1 704-1 709.]
    [2]马艳,靳立亚,段炼,等.三江源湿地的退化对区域气候的影响[J].高原山地气象研究,2011,31(1):42-45.[Ma Yan,Jin Liya,Duan Lian,et al.Impact of the wetland degeneracy in threeriver source on regional climate model[J].Plateau and Mountain Meteorology Research,2011,31(1):42-45.]
    [3]赵洪宇,张雪芹,解承莹.多源水汽再分析资料在青藏高原的适用性评估[J].干旱区研究,2017,34(2):300-308.[Zhao Hongyu,Zhang Xueqin,Xie Chengying.Applicability of reanalysis data of multi-source water vapor over the Tibetan Plateau[J].Arid Zone Research,2017,34(2):300-308.]
    [4]王欢,李栋梁.黄河源区径流量变化特征及其影响因子研究进展[J].高原山地气象研究,2013,33(2):93-99.[Wang Huan,Li Dongliang.Research progress on variations and effectors of the runoff in the source region of Yellow River[J].Plateau and Mountain Meteorology Research,2013,33(2):93-99.]
    [5]周长进,关志华.澜沧江(湄公河)正源及其源头的再确定[J].地理研究,2001,20(2):184-190.[Zhou Changjin,Guan Zhihua.The source of Lancangjiang(Mekong)River[J].Geographical Research,2001,20(2):184-190.]
    [6]吴迪,赵勇,裴源生,等.澜沧江-湄公河流域温度和降水变化趋势分析[J].中国水利科学研究院学报,2011,9(4):304-312.[Wu Di,Zhao Yong,Pei Yuansheng,et al.Variation trends of temperature and precipitation in Lancang-Mekong River Basin during 1980-2009[J].Journal of China Institute of Water Resources and Hydropower Research,2011,9(4):304-312.]
    [7]Cook E R,Anchukaitis K J,Buckley B M,et al.Asian monsoon failure and megadrought during the last millennium[J].Science,2010,328(5 977):486-489.
    [8]Yang B,Qin C,Huang K,et al.Spatial and temporal patterns of variations in tree growth over the northeastern Tibetan Plateau during the period AD 1450-2001[J].Holocene,2010,20:1 235-1 245.
    [9]秦宁生,时兴合,邵雪梅,等.川西高原树木年轮所指示的平均最高气温变化[J].高原山地气象研究,2008,28(4):18-24.[Qin Ningsheng,Shi Xinghe,Shao Xuemei,et al.Average maximum temperature change recorded by tree rings in West Sichuan Plateau[J].Plateau and Mountain Meteorology Research,2008,28(4):18-24.]
    [10]程雪寒,吕利新.藏东南树木年轮记载的公元1560年以来的极端干旱事件[J].第四纪研究,2015,35(5):1 093-1 101.[Cheng Xuehan,LüLixin.Extreme drought events since 1560 A.D.recorded by tree rings on the southeast Qinghai-Tibetan Plateau[J].Quaternary Sciences,2015,35(5):1 093-1 101.]
    [11]秦宁生,邵雪梅,靳立亚,等.青海南部高原圆柏年轮指示的近500年来气候变化[J].科学通报,2003,48(19):2 068-2 072.[Qin Ningsheng,Shao Xuemei,Jin Liya,et al.Climate change over southern Qinghai Plateau in the past 500 years recorded in Sabina tibetica tree rings[J].Chinese Science Bulletin,2003,48(19):2 068-2 072.]
    [12]Gou X,Chen F,Cook E,et al.Streamflow variations of the Yellow River over the past 593 years in western China reconstructed from tree-rings[J].Water Resource Research,2007,43:W6 434.
    [13]秦宁生,靳立亚,时兴合,等.利用树轮资料重建通天河流域518年径流量[J].地理学报,2004,59(4):550-556.[Qin Ningsheng,Jin Liya,Shi Xinghe,et al.A 518-year runoff reconstruction of Tongtian River basin using tree-ring width chronologies[J].Acta Geographica Sinica,2004,59(4):550-556.]
    [14]时兴合,秦宁生,邵雪梅,等.青海杂多圆柏年轮指示的近700年旱涝变化[J].高原气象,2009,28(4):769-776.[Shi Xinghe,Qin Ningsheng,Shao Xuemei,et al.The drought and flood signals in recent 700 years indicated by long tree-rings of Sabina Tibetica in Zaduo of Qinghai Province[J].Plateau Meteorology,2009,28(4):769-776.]
    [15]Ye M L,Qin N S,Bai A J,et al.Tree ring width records of maximum temperature in April-June on source region of Yangtze River from 1470 to 2009[J].Quaternary Sciences,2015,35(5):1 102-1 111.
    [16]Xiao D M,Shao X M,Qin N S,et al.Tree-ring-based reconstruction of streamflow for the Zaqu River in the Lancang River source region,China,over the past 419 years[J].Internatial Journal of Biometeorology,2017,61(7):1 173-1 189.
    [17]肖丁木,秦宁生,黄小梅.树轮记录的长江源区近412年以来3-5月降水量变化[J].冰川冻土,2016,38(6):1 691-1 700.[Xiao Dingmu,Qin Ningsheng,Huang Xiaomei.A 412-year March-May precipitation series reconstructed from tree-ring records in the source regions of Yangtze River[J].Journal of Glaciology and Geocryology,2016,38(6):1 691-1 700.]
    [18]Vicente-Serrano S M,Beguería S,López-Moreno J I.A multiscalar drought index sensitive to global warming:the standardized precipitation evapotranspiration index[J].Journal of Climate,2010,23:1 696-1 718.
    [19]Wang L,Chen W.Applicability analysis of standardized precipitation evapotranspiration index in drought monitoring in China[J].Plateau Meteorology,2014,33(2):423-431.
    [20]Allen K J,Ogden J,Buckley B M,et al.The potential to reconstruct broad scale climate indices associated with Southeast Australian droughts from Athrotaxis species,Tasmania[J].Climate Dynamics,2011,37(9-10):1 799-1 821.
    [21]Vicente-Serrano S M,Lopez-Moreno J I,Lorenzo-Lacruz J,et al.The NAO impact on droughts in the Mediterranean Region[J].Hydrological,Socioeconomic and Ecological Impacts of the North Atlantic Oscillation in the Mediterranean Region,2011,46:23-40.
    [22]Bao G,Liu Y,Liu N,et al.Drought variability in Eastern Mongolian Plateau and its linkages to the large-scale climate forcing[J].Climate Dynamics,2015,44:717-733.
    [23]Chen F,Yuan Y,Yu S,et al.A 225-year long drought reconstruction for east Xinjiang based on Siberia larch(Larix sibirica)treering widths:Reveals the recent dry trend of the eastern end of Tien Shan[J].Quaternary International,2015,358:42-47.
    [24]Gou X,Deng Y,Gao L,et al.Millennium tree-ring reconstruction of drought variability in the eastern Qilian Mountains,Northwest China[J].Climate Dynamics,2014,45(7-8):1 761-1 770.
    [25]The Editing Committee of Forest.Forest in Qinghai[M].Beijing:China Forestry Publishing House,1993:240-245.
    [26]魏凤英.现代气候统计诊断与预测技术[M].北京:气象出版社,1999:1-275.[Wei Fengying.Modern Weather Forecasting Techniques and Statistical Diagnosis[M].Beijing:China Meteorological Press,1999:1-275.]
    [27]Kohler M A.On the use of double-mass analysis for testing the consistency of meteorological record sand for making required adjustment[J].Bulletin of American Meteorological Society,1949,30:188-189.
    [28]Holmes R L.Computer-assisted quality control in tree-ring dating and measurement[J].Tree-Ring Bulletin,1983,43:69-78.
    [29]Cook E R.A Time Series Analysis Approach to Tree-ring Standardization[D].Tucson:University of Arizona,1985.
    [30]Fang K Y,Gou X H,Peters K,et al.Removing biological trends from tree-ring series:Testing modified hungeshoff curves[J].Treering Research,2010,66:51-59.
    [31]VFritts H C.Tree Ring and Climate[M].London:Academic Press,1976:1-567.
    [32]Fan Z X,Brauning A,Cao K F.Tree-ring based drought reconstruction in the Hengduan Mountains Region(China)since A.D.1655[J].International Journal of Climatology,2008,28:1 879-1 887.
    [33]Zhang Q B,Cheng G D,Yao T D,et al.A 2 326-year tree-ring record of climate variability on the northeastern Qinghai-Tibetan Plateau[J].Geophysical Research Letters,2003,30(14):1 739.
    [34]肖丁木,秦宁生,黄小梅.利用树轮资料重建黄河源区曲什安河1505-2010年流量变化[J].中国沙漠,2017,37(2):372-383.[Xiao Dingmu,Qin Ningsheng,Huang Xiaomei.Tree-ring based streamflow reconstruction for the Qushian River of Yellow River source region from 1505 to 2010[J].Journal of Desert Research,2017,37(2):372-383.]
    [35]白虎志,董安祥,郑广芬,等.中国西北地区近500年旱涝分布图集[M].北京:气象出版社,2010:211-223.[Bai Huzhi,Dong Anxiang,Zheng Guangfen,et al.Yearly Charts of Dryness/Wetness in Northwest China for the Last 500-year Period[M].Beijing:China Meteorological Press,2010:211-223.]
    [36]Mann M E,Lees J M.Robust estimation of background noise and signal detection in climatic time series[J].Climatic Change,1996,33(3):409-445.
    [37]Tourre Y M,Rajagopalan B,Kushnir Y,et al.Patterns of coherent decadal and interdecadal climate signals in the Pacific Basin during the 20th century[J].Geophysical Research Letters,2001,28(10):2 069-2 072.
    [38]Hale G E.Preliminary results of an attempt to detect the general magnetic field of the sun[J].Astrophysical Journal,1913,38(1):27-98.
    [39]Allan R,Lindesay J,Parker D.El Ni1o Southern Oscillation&Climatic Variability[M].Australia:CSIRO Publishing,1998:405.
    [40]邢佩.青藏高原树轮气候重建与中国东部树种的树轮气候学评价---以青海三江源、西藏昌都和浙江古田山地区为例[D].北京:中国科学院大学,2013.[Xing Pei.Climate Reconstruction on the Qinghai-Tibetan Plateau Based on Tree Ring and Dendroclimatological Evaluation of Tree Species in Eastern China:A Case Study in Sanjiangyuan Region of Qinghai,Changdu Prefecture of Tibet and Gutian Mountain of Zhejiang[D].Beijing:University of Chinese Academy of Sciences,2013.]
    [41]Gou X H,Chen F H,Cook E,et al.Streamflow variations of the Yellow River over the past 593 years in Western China reconstructed from tree rings[J].Water Resources Research,2007,43(6):1 820-1 830.
    [42]黄小梅,肖丁木,秦宁生.大果圆柏树轮记录的公元1606-2012年长江源区4-6月帕尔默干旱指数变化[J].中国沙漠,2017,37(4):784-792.[Huang Xiaomei,Xiao Dingmu,Qin Ningsheng.Palmer Drought Severity Index in April-June reconstruction based on Juniper Tibetica tree-ring during 1606-2012 in the Yangtze River source region[J].Journal of Desert Research,2017,37(4):784-792.]
    [43]吕爱锋,贾绍凤,王素慧,等.PDO和ENSO指数与三江源地区径流变化的相关关系研究[J].南水北调与水利科技,2010,8(2):49-52.[LüAifeng,Jia Shaofeng,Wang Suhui,et al.Relationship between streamflow in Sanjiangyuan and the indices of ENSO and PDO[J].South-to-North Water Transfers and Water Science&Technology,2010,8(2):49-52.]
    [44]刘青春,秦宁生,靳力亚,等.三江源地区春夏季降水与太平洋海温的关系[J].气象科技,2007,35(3):335-339.[Liu Qingchun,Qing Ningsheng,Jin Liya,et al.Relationship between spring and summer rainfall in three-river source region and Pacific SST[J].Meteorological Science and Technology,2007,35(3):335-339.]
    [45]张平,陈碧辉,毛晓亮.青藏高原东侧降水与印度洋海温的遥相关特征[J].高原山地气象研究,2008,28(2):15-21.[Zhang Ping,Chen Bihui,Mao Xiaoliang.The teleconnection characteristics between the precipitation on the east side of Tibetan Plateau and Indian ocean SST[J].Plateau and Mountain Meteorology Research,2008,28(2):15-21.]
    [46]肖贻青,王健,姚静.西安地区近五百年旱涝变化趋势与近百年旱涝成因分析[J].干旱区研究,2017,34(6):1 448-1 456.[Xiao Yiqing,Wang Jian,Yao Jing.Trends of drought and flood in recent 500 years and their causes in recent 100 years in Xi’an[J].Arid Zone Research,2017,34(6):1 448-1 456.]
    [47]Smith T M,Reynolds R W.Improved extended reconstruction of SST(1854-1997)[J].Journal of Climate,2004,17(12):2 466-2 477.
    [48]Wang B,Wu R G,Fu X H.Pacific-East Asian teleconnection:How does ENSO affect East Asian climate[J].Journal of Climate,2000,13(9):1 517-1 536.
    [49]周连童,黄荣辉.关于我国夏季气候年代际变化特征及其可能成因的研究[J].气候与环境研究,2003,8(3):274-290.[Zhou Liantong,Huang Ronghui.Research on the characteristics of interdecadal variability of summer climate in China and its possible cause[J].Climatic and Environmental Research,2003,8(3):274-290.]

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700