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  • ISSN 1000-694X
  • 双月刊 创刊于1981年
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中国地理学会沙漠分会2014年学术研讨会论文选

基于树轮δ13C的阿尔泰山南坡夏季降水变化分析

  • 张瑞波 ,
  • 尚华明 ,
  • 袁玉江 ,
  • 魏文寿 ,
  • 张同文 ,
  • 陈峰 ,
  • 喻树龙 ,
  • 范子昂 ,
  • 秦莉
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  • 中国气象局乌鲁木齐沙漠气象研究所 中国气象局树轮年轮理化研究重点开放实验室/新疆树木年轮生态实验室, 新疆 乌鲁木齐 830002
张瑞波(1983-),男,陕西武功人,副研究员,主要从事气候变化与环境、树木年轮气候学研究.Email: river0511@163.com

收稿日期: 2014-10-13

  修回日期: 2014-11-28

  网络出版日期: 2015-01-20

基金资助

国家自然科学基金项目(41275120, 41405139);国家公益性行业(气象)科研专项(GYHY 201206026);中国沙漠气象科学研究基金项目(Sqj2014014)

Summer Precipitation Variation in the Southern Slope of the Altay Mountains Recorded by Tree-ring δ13C

  • Zhang Ruibo ,
  • Shang Huaming ,
  • Yuan Yujiang ,
  • Wei Wenshou ,
  • Zhang Tongwen ,
  • Chen Feng ,
  • Yu Shulong ,
  • Fan Ziang ,
  • Qin Li
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  • Key Laboratory of Tree-ring Physical and Chemical Research of China Meteorological Administration/Key Laboratory of Tree Ring Ecology of Xinjiang Uigur Autonomous Region, Institute of Desert Meteorology, China Meteorological Administration, Urumqi 830002, China

Received date: 2014-10-13

  Revised date: 2014-11-28

  Online published: 2015-01-20

摘要

利用阿尔泰山南坡东、中、西部3个样点的西伯利亚落叶松树轮δ13C序列,结合阿勒泰地区7个气象站降水资料分析表明,树轮δ13C序列对阿尔泰山南坡夏季降水有较好的响应,最高相关系数可达到-0.682(p<0.0001).利用回归方法重建了过去160年来阿尔泰山南坡夏季降水量.阿尔泰山南坡夏季降水在1850-1871年偏多,1872-1956年经历了长期的干旱,20世纪60年代至今,随着新疆整体气候的暖湿化,阿尔泰山南坡经历了较长的湿润期.重建的夏季降水与上年冬季北极涛动(AO)有较好的相关性,北极涛动可能对阿尔泰山南坡过去160年降水有较大影响.阿尔泰山南坡过去160年夏季降水变化存在11 a(95% )、2.7 a (95%)、2.4 a(95%)、2.1 a(99%)和2.0 a(99%)的准周期变化.

本文引用格式

张瑞波 , 尚华明 , 袁玉江 , 魏文寿 , 张同文 , 陈峰 , 喻树龙 , 范子昂 , 秦莉 . 基于树轮δ13C的阿尔泰山南坡夏季降水变化分析[J]. 中国沙漠, 2015 , 35(1) : 106 -112 . DOI: 10.7522/j.issn.1000-694X.2014.00198

Abstract

In this paper, we developed 3 tree-ring δ13C chronologies from eastern, central and western on south slope of the Altay Mountains based on standard dendrochronology methods and stable carbon isotope research process. Correlation analysis combined with precipitation data from 7 meteorological stations in the Altay Mountains showed that, the tree-ring δ13C series response to summer precipitation on south slope of the Altay Mountains, the highest single correlation index can reach to -0.682 (p<0.0001). The summer precipitation was constructed with regression method. The reconstruction could go back to 1850 and has an adjusted r2 of 0.453 (1962-2008). The precipitation variability in the past 160 years was analyzed, it shown that the summer precipitation is above normal in the 1850-1871, then the climate have a long dryer period in 1872-1956, and after 1960s until today, it experienced a long wetter period with the climate warming and wetting in Xinjiang. There have a good correlation between summer precipitation and Arctic Oscillation (AO), and Arctic Oscillation may have a greater impact on precipitation variability on south slope of the Altay Mountains. The summer precipitation have the quasi-periodic variations of 11 a (95%), 2.7 a (95%), 2.4 a (95%), 2.1 a (99%) and 2.0 a (99%) .

参考文献

[1] IPCC.Climate change 2013:The Physical Science Basis[M/OL].Cambridge,UK:Cambridge University Press.2013-09-30 [2013-09-30].http://www.ipcc.ch/report/ar5/wg1/#.Uq_tD7KBRR1
[2] Dai A G,Trenberth K E,Karl T R.Global variations in droughts and wet spells:1900-1995[J].Geography Research Letters,1998,25:3367-3370.
[3] Mann M E,Bradley R S,Hughes M K,et al.Global-scale temperature patterns and climate forcing over the past six centuries[J].Nature,1998,392:779-787.
[4] McCarroll D,Loader N J.Stable isotopes in tree rings[J].Quaternary Science Reviews,2004,23:771-801.
[5] Nuerlan H.Hydrological features of rivers in Altai prefeture[J].Hydrology,2001,21(4):53-55.
[6] 胡义成,袁玉江,魏文寿,等.用树木年轮重建阿尔泰东部6-7月平均温度序列[J].中国沙漠,2012,32(4):1003-1009.
[7] 尚华明,魏文寿,袁玉江,等.哈萨克斯坦东北部310年来初夏温度变化的树轮记录[J].山地学报,2011,29(4):402-408.
[8] 陈峰,袁玉江,魏文寿,等.用西伯利亚落叶松年轮最大密度重建和布克赛尔5-8月份平均最高温度[J].生态学报,2010,30(17):4652-4658.
[9] Ovtchinnikov D,Adamenko M,Panushkina I.A 1105-year tree-ring chronology in Altai region and its application for reconstruction of summer temperatures[J].Geolines,2000,11:121-122.
[10] 尚华明,魏文寿,袁玉江,等.树木年轮记录的阿勒泰436a来6月温度变化[J].干旱区资源与环境,2010,24(8):116-121.
[11] 李江风.新疆年轮气候年轮水文研究[M].北京:气象出版社,1989 .
[12] 张同文,袁玉江,喻树龙,等.用树木年轮重建阿勒泰西部5-9月365年来的月平均气温[J].干旱区研究,2008,25(2):288-294
[13] 尚华明,魏文寿,袁玉江,等.阿尔泰山南坡树轮宽度对气候变暖的响应[J].生态学报,2010,9:2246-2253
[14] 张同文,袁玉江,喻树龙,等.树木年轮重建阿勒泰西部1481-2004年6-9月降水量序列[J].冰川冻土,2008,30(4):659-667
[15] Chen F,Yuan Y J,Wei W S,et al.Precipitation reconstruction for the southern Altay Mountains (China) from tree rings of Siberian spruce,reveals recent wetting trend[J].Dendrochronologia,2014,32:266-272.
[16] Xu G B,Liu X H,Qin D H,et al.Relative humidity reconstruction for northwestern China's Altay Mountains using tree-ring δ18O[J].Chines Science Bulletin,2014,59(2):190-200.
[17] Sidorova O V,Siegwolf R T W,Myglan V S,et al.The application of tree-rings and stable isotopes for reconstructions of climate conditions in the Russian Altai[J].Climatic Change 2013,120:153-167.
[18] Mann H B.Non-parametric test against trend[J].Econometrika,1945,13:245-259
[19] Cook E R.A Time Series Analysis Approach to Tree-ring Standardization[D].Tucson,USA:The University of Arizona,1985.
[20] 张瑞波,袁玉江,魏文寿,等.西伯利亚落叶松树轮稳定碳同位素对气候的响应[J].干旱区研究,2012,29(2):328-334.
[21] 张瑞波,尚华明,魏文寿,等.树轮δ13C 记录的阿勒泰地区近160 a夏季气温变化[J].沙漠与绿洲气象,2014,8(2):34-40.
[22] Saurer M,Siegenthaler U,Schweingruber F.The climate-carbon isotope relationship in tree rings and the significance of site conditions[J].Tellus,1995,47B:320-330.
[23] Alexander V K,Kerstin S T,Anatolii N,et al.Climate signals in tree-ring width,density and δ13C from larches in Eastern Siberia(Russia) [J].Chemical Geology,2008,252:31-41.
[24] Shi Y F,Shen Y P,Kang E,et al. Recent and future climate change in northwest China[J].Climate Change,2007,80:379-393.
[25] Sidorova O V,Saurer M,Myglan V S,et al.A multi-proxy approach for revealing recent climatic changes in the Russian Altai[J].Climate Dynamics,2012,38:175-188.
[26] Thompson D W,Wallace J M.The arctic oscillation signature in the wintertime geopotential height and temperatuIe fields[J].Geography Research Letter,1998,25,1297-1300.
[27] Li J P,Wang J L.A modified zonal index and its physical sense[J].Geography Research Letters,2003,30(12):16-32.
[28] Higgins R W,Leetmaa A,Xue Y,et a1.Dominant factors influencing the seasonal predictability of U.S.precipitation and surface air temperature[J].Journal of Climate,2000,13:3994-4017.
[29] Trigo R M,Pozo-Vazquez D,Osborn T J,et a1.North Atlantic Oscillation influence on precipitation,river flow and water resources in the Iberian Peninsula[J].International Journal of Climatology,2004,24:925-944.
[30] 郭渠,孙卫国,程炳岩.我国西北地区气候变化与北极涛动的交叉小波分析[J].南京气象学院院报,2008,31(6):811-818
[31] Mann M E,Lee J M.Robust estimate estimation of background noise and signal detection in climatic time series[J].Climatic Change,1996,33(3):409-445.
[32] Thomson D J.Time series analysis of Holocene climate date[J].Philosophical Transactions of the Royal Society A,1990,330:601-616.
[33] Thomson D J.Quadratic inverse spectrum estimates:applications to palaeoclimatology[J].Philosophical Transactions of the Royal Society A,l990,332:593-597.
[34] 罗哲贤.中国西北干旱气候动力学引论[M].北京:气象出版社,2005:130-170.
[35] 张瑞波,魏文寿,袁玉江,等.1396-2005年天山南坡阿克苏河流域降水序列重建与分析[J].冰川冻土,2009,31(1):27-33.
[36] 张瑞波,袁玉江,魏文寿,等树轮记录的吉尔吉斯斯坦东部过去百年干湿变化[J].干旱区地理,2013,36(4):691-699.
[37] 高卫东,袁玉江,张瑞波,等.树木年轮记录的天山北坡中部过去338 a降水变化[J].中国沙漠,2011,31(6):1535-1540.
[38] 魏文寿,袁玉江,喻树龙,等.中国天山山区235 a气候变化及降水趋势预测[J].中国沙漠,2008,28(5):803-808.
[39] Zhang T W,Yuan Y J,Liu Y,et al.A tree ring based precipitation reconstruction for the Baluntai region on the southern slope of the central Tien Shan Mountains,China,since A.D.1464[J].Quaternary International,2013,283,55-62.
[40] 秦莉,袁玉江,喻树龙,等.利用树轮宽度资料重建天山东段近443年相对湿度变化[J].地球环境学报,2012,3(3):908-914.
[41] Chen F,Yuan Y J,Chen F H,et al.A 426-year drought history for Western Tian Shan,Central Asia inferred from tree-rings and its linkages to the North Atlantic and Indo-West Pacific Oceans[J].The Holocene,2013,23(8):1095-1104.
[42] 蔺甲,袁玉江,魏文寿,等.利用树轮年表重建新疆博州中东部1622-2010年降水量[J].中国沙漠,2013,33(5):1527-1535.
[43] 陈峰,袁玉江,魏文寿,等.树轮记录的伊犁地区近354年帕尔默干旱指数变化[J].高原气象2011,30(2):355-362.
[44] Chen F,Yuan Y J,Wei W S,et al.Tree-ring-based annual precipitation reconstruction for the Hexi Corridor,NW China:consequences for climate history on and beyond the mid-latitude Asian continent[J].Boreas,2013,42:1008-1021.
[45] 陈峰,袁玉江,魏文寿,等.腾格里沙漠南缘近315年5-6月PDSI指数变化[J].地理科学,2011,31(4):434-439.
[46] Chen F,Yuan Y J,Wei W S,et al.Tree-ring-based reconstruction of precipitation for the Changling Mountains,China,since A.D.1691[J].International Journal of Biometeorology,2012,56:765-774.
[47] Wilson R C,Hudson H S.Sun luminosity variations in solar cycle 21[J].Nature,l988,332:8l0-812.
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