河南省栾川县近50a降水特征及其对氧同位素的影响Characteristics of Precipitation and Their Influence on Oxygen Isotope for the Past 50 Years in Luanchuan County,Henan Province,China
贾亦真;
摘要(Abstract):
通过对近631个大气降水量和平均气温数据的分析发现,河南省栾川县近50 a来年降水量呈下降趋势,20世纪60年代降水量偏高,90年代降水量偏低,而年平均气温整体呈现上升趋势,与近20 a全球变暖的规律一致。另外,研究区大气降水氧同位素值和日降水量及日平均气温呈现负相关的关系,结合栾川县近50 a器测资料与相邻地区洞穴石笋δ(18O)记录的对比分析表明,亚洲季风系统在20世纪60年代中期和70年代中期发生的两次减弱事件在栾川县降水量和石笋δ(18O)记录中都有响应,由此说明该地区大气降水的氧同位素组成固然有降水量效应,但大气环流效应更为显著。
关键词(KeyWords): 降水;全球变化;氧同位素;河南栾川
基金项目(Foundation): 国家自然科学基金项目(40902053);; 教育部博士点科学基金项目(20090182120005)
作者(Author): 贾亦真;
Email:
DOI:
参考文献(References):
- [1]Wang H J.The weakening of the Asian Monsoon circulation afterthe end of 1970s[J].Advances in Atmospheric Sciences,2001,18(3):376-386.
- [2]Jiang D B,Wang H J.Natural interdecadal weakening of East A-sian summer monsoon in the late 20th century[J].Chinese Sci-ence Bulletin,2005,50(17):1923-1929.
- [3]任国玉,郭军,徐铭志,等.近50年中国地面气候变化基本特征[J].气象学报,2005,63(6):942-956.
- [4]宋献方,柳鉴容,孙晓敏,等.基于CERN的中国大气降水同位素观测网络[J].地球科学进展,2007,22(7):738-747.
- [5]宋燕,季劲钧,孙丹.20世纪60年代中期亚非夏季风减弱的全球气候背景异常分析[J].大气科学,2009,33(2):313-324.
- [6]Zhang D E,Li H C,Ku T L,et al.On linking climate to Chinesedynastic change:Spatial and temporal variations of monsoonal rain[J].Chinese Science Bulletin,2010,55(01):77-83.
- [7]李彬,袁道先,林玉石,等.桂林地区降水、洞穴滴水及现代洞穴碳酸盐氧碳同位素研究及其环境意义[J].中国科学:D辑,2000,30(1):81-87.
- [8]Zhang P Z,Johnson K R,Chen Y M,et al.Modern systematicsand environmental significance of stable isotopic variations inWanxiang Cave,Wudu,Gansu,China[J].Chinese Science Bul-letin,2004,49(15):1649―1652.
- [9]Wang Y J,Cheng H,Edwards R L,et al.The Holocene Asianmonsoon:Links to solar changes and north Atlantic climate[J].Science,2005,308:854-857.
- [10]Zhang P Z,Cheng H,Edwards R L,et al.A test of climate,sun,and culture relationships from an 1810-year Chinese cave re-cord[J].Science,2008,322:940-942.
- [11]Hu C Y,Henderson G M,Huang J H,et al.Quantification of Hol-ocene Asian monsoon rainfall from spatially separated cave record[J].Earth Planet Science Letters,2008,266:221-232.
- [12]Tan L C,Cai Y J,Cheng H,et al.Summer monsoon precipitationvariations in central China over the past 750 years derived from ahigh-resolution absolute-dated stalagmite[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2009,280:432-439.
- [13]Cai B G,Edwards R L,Cheng H,et al.A dry episode during theYounger Dryas and centennial-scale weak monsoon events duringthe early Holocene:A high-resolution stalagmite record from south-east of the Loess Plateau,China[J].Geophys Research Letters,2008,35:L02705,1-6.
- [14]Yang X L,Zhang P Z,Chen F H,et al.Modern stalagmite oxy-gen isotopic composition and its implications of climatic changefrom a high-elevation cave in the eastern Qinghai-Tibet Plateau overthe past 50 years[J].Chinese Science Bulletin,2007,52(9):1238-1247.
- [15]谭明.环流效应:中国季风区石笋氧同位素短尺度变化的气候意义:古气候记录与现代气候研究的一次对话[J].第四纪研究,2009,29(5):851-862.
- [16]何璐瑶,胡超涌,黄俊华,等.石笋氧同位素指示东亚季风大尺度环流特征[J].第四纪研究,2009,29(5):950-956.
- [17]贾锡强,王文奇.用序列特征值周期迭加法制作栾川长期天气预报[J].河南气象,1994(1):16-17.
- [18]吴海涛.栾川县近40年气候变化分析[J].河南气象,2005(2):19.
- [19]吴海涛.气候变化对栾川工农业生产的影响[J].河南气象,2006(1):58-59.
- [20]Zhang ML,Cheng H,Yuan DX,et al.High resolution climate re-cords from two stalagmites in Qixin cave,South Guizhou,andHeinrich events during the last glacial period[J].Episodes,2004,27(2):1-7.
- [21]Zhang M L,Cheng H,Yuan D X,et al.Carbon and oxygen iso-tope records and paleoclimate reconstruction(140-250 ka B.P.)from a stalagmite of Shuinan Cave,Guilin,China[J].Environ-mental Geology,2006,49:752-764.
- [22]郑淑蕙,侯发高,倪葆龄.我国大气降水的氢氧同位素研究[J].科学通报,1983,28(3):801-806.
- [23]李茂松,李森,李育慧.中国近50年洪涝灾害灾情分析[J].中国农业气象,2004,25(1):38-41.