全部 标题 作者
关键词 摘要

OALib Journal期刊
ISSN: 2333-9721
费用:99美元

查看量下载量

相关文章

更多...
科学通报  2012 

利用兴安落叶松树轮最大晚材密度重建大兴安岭北部5~8月气温变化

, PP. 1785-1793

Keywords: 兴安落叶松,树木年轮,最大晚材密度,夏季气温重建

Full-Text   Cite this paper   Add to My Lib

Abstract:

对大兴安岭北部3个样点的兴安落叶松(Larixgmelinii)树轮样本进行树轮密度的分析,相关分析结果显示,树轮最大晚材密度年表与夏季气温变化有显著正相关关系,利用其中两个样点的树轮最大晚材密度对研究区1855年以来5~8月的平均最高气温变化进行了重建,重建值的解释方差量为39.5%.在大兴安岭北部过去的154年里,存在4个冷期1874~1893,1927~1948,1951~1960和1992~2002年;以及4个暖期1855~1873,1894~1916,1961~1991和2003~2008年.该地区20世纪末冬季气温的变暖现象比夏季更为明显.重建结果与研究区周边的气温序列均有较好的一致性,可以指示较大区域的气候特征.

References

[1]  2 Esper J, Cook E R, Schweingruber F H. Low-frequency signals in long tree-ring chronologies for reconstructing past temperature variability. Science, 2002, 295: 2250-2253??
[2]  3 丁一汇, 戴晓苏. 中国近百年来的温度变化. 气象, 1994, 12: 19-26
[3]  4 王绍武, 叶瑾琳, 龚道溢, 等. 近百年中国年气温序列的建立. 应用气象学报, 1998, 9: 392-401
[4]  5 勾晓华, 杨梅学, 彭剑峰. 树轮记录的阿尼玛卿山区过去830 年夏半年最高温变化. 第四纪研究, 2006, 26: 991-998
[5]  6 朱海峰, 郑永宏, 邵雪梅, 等. 树木年轮记录的青海乌兰地区近千年温度变化. 科学通报, 2008, 53: 1835-1841
[6]  8 Aucour A M, Tao F X, Sheppard S M F, et al. Climatic and monsoon isotopic signals (δD, δ13C) of northeastern China tree rings. J Geophys Res, 2002, 107: 4074, doi: 10.1029/2001JD000464
[7]  10 徐海, 洪业汤, 朱咏煊, 等. 安图红松树轮稳定δ13C, δ18O 序列记录的气候变化信息. 地质地球化学, 2002, 30: 59-65
[8]  11 于大炮, 王顺忠, 唐立娜, 等. 长白山北坡落叶松年轮年表及其与气候变化的关系. 应用生态学报, 2005, 16: 14-20
[9]  13 邵雪梅, 吴祥定. 利用树轮资料重建长白山区过去气候变化. 第四纪研究, 1997, 1: 76-85
[10]  14 Liu Y, Bao G, Song H M, et al. Precipitation reconstruction from Hailar pine (Pinus sylvestris var. mongolica) tree rings in the Hailar region, Inner Mongolia, China back to 1865 AD. Palaeogeogr Paleoclimatol Paleoecol, 2009, 282: 81-87
[11]  16 尹红, 郭品文, 刘洪滨, 等. 利用树轮重建小兴安岭五营1796 年以来的温度变化. 气候变化研究进展, 2009, 5: 18-23
[12]  18 沙万英, 邵雪梅, 黄玫. 20 世纪80 年代以来中国的气候变暖及其对自然区域界线的影响. 中国科学D 辑: 地球科学, 2002, 32:317-326
[13]  19 Wang L, Payette S, Begin Y. 1300-year tree-ring width and density series based on living, dead and subfossil black spruce at tree-line in Subarctic Quebec, Canada. Holocene, 2001, 11: 333-341??
[14]  20 陈津, 王丽丽, 朱海峰, 等. 用天山雪岭云杉年轮最大密度重建新疆伊犁地区春夏季平均最高温度变化. 科学通报, 2009, 54:1295-1302
[15]  21 段建平, 王丽丽, 李论, 等. 树轮最大密度记录的贡嘎山区公元1837 年以来的温度变化. 科学通报, 2010, 55: 1036-1042
[16]  24 王丽丽, 邵雪梅, 黄磊, 等. 黑龙江漠河兴安落叶松与樟子松树轮生长特性及其对气候的响应. 植物生态学报, 2005, 29: 380-385
[17]  25 Lenz O, Schaer E, Schweingruber F H. Methodische Probleme bei der radiographisch-densitometrischen Bestimmung der Dichte und der Jahrringbreiten von Holz. Holzforschung, 1976, 30: 114-123??
[18]  26 Schweingruber F H, Bartholin T, Schar E, et al. Radiodensitometric-dendroclimatological conifer chronologies from Lapland (Scandinavie) and the Alps (Switzerland). Boreas, 1988, 17: 559-566
[19]  27 Holmes R L. Computer-assisted quality control in tree-ring dating and measurement. Tree-Ring Bull, 1983, 43: 69-78
[20]  28 Cook E R. A time series analysis approach to tree ring standardization. Dissertation for the Doctoral Degree. Tuscon: University of Arizona,1985
[21]  29 黄嘉佑. 气象统计分析与预报方法. 北京: 气象出版社, 2000
[22]  30 Oh H S, Ammann C M, Naveau P, et al. Multi-resolution time series analysis applied to solar irradiance and climate reconstruction. J Atmos Sol-Terr Phys, 2003, 65: 191-201??
[23]  32 Aydin N, Markus H S. Directional wavelet transform in the context of complex Quadrature Doppler signals. IEEE Signal Proc Lett, 2000,7: 278-280??
[24]  33 Zhang Q, Cheng G, Yao T, et al. A 2326-year treering record of climate variability on the northeastern Qinghai-Tibetan Plateau. Geophys Res Lett, 2003, 30: 1-4
[25]  39 Schweingruber F H, Briffa K R, Jones P D. Yearly maps of summer temperatures in western Europe from AD 1750 to 1975 and western North America from 1600 to 1982: Results of a radiodensitometrical study on tree rings. Vegetatio, 1991, 92: 5-71
[26]  41 孙毓, 王丽丽, 陈津, 等. 中国落叶松属树木年轮生长特性及其对气候变化的响应. 中国科学: 地球科学, 2010, 40: 645-653
[27]  43 Ding Y H. Seasonal march of the East-Asian summer monsoon. In: Zhang C P, ed. East Asian Monsoon. Singapore: World Scientific,2004. 3-53
[28]  1 Moberg A, Sonechkin D M, Holmgren K, et al. Highly variable Northern Hemisphere temperatures reconstructed from low- and highresolution proxy data. Nature, 2005, 433: 613-617??
[29]  7 刘禹, 安芷生, Linderholm H W, 等. 青藏高原中东部过去2485 年以来温度变化的树轮记录. 中国科学D 辑: 地球科学, 2009, 39:166-176
[30]  9 徐海, 洪业汤, 朱咏煊, 等. 安图红松树轮稳定碳同位素记录的低云量信息. 地球化学, 2002, 31: 309-314
[31]  12 Chen Z J, He X Y, Chen W, et al. Solar activity, global surface air temperature anomaly and Pacific Decadal Oscillation signals observed in urban outskirts tree ring records from Shenyang, China. Adv Space Res, 2006, 38: 2272-2284??
[32]  15 Zhu H F, Fang X Q, Shao X M, et al. Tree ring-based February-April temperature reconstruction for Changbai Mountain in Northeast China and its implication for East Asian winter monsoon. Clim Past, 2009, 5: 661-666??
[33]  17 任国玉, 周薇. 辽东半岛本世纪气温变化的初步研究. 气象学报, 1994, 52: 493-498
[34]  22 Schweingruber F H. Measurement of densitometric properties of wood. In: Hughes M K, Kelly P M, Pilcher J R, et al, eds. Climate from Tree Rings. New York: Cambridge University Press, 1982. 8-11
[35]  23 Schweingruber F H, Briffa K R. Tree-ring Density Networks for Climate Reconstruction. In: Jones P D, Bradley R S, Jouzel J, eds. Climatic Variations and Forcing Mechanisms of the Last 2000 Years. NATO ASI Series, Series I: Global Environmental Change. Berlin: Springer, 1996. 43-66
[36]  31 Torrence C, Compo G P. A practical guide to wavelet analysis. Bull Am Meteorol Soc, 1998, 79: 61-78??
[37]  34 Lu H, Zhang F, Liu X, et al. Periodicity of palaeoclimatic variations recorded by loess-paleosol sequences in China. Quat Sci Rev, 2004,23: 1891-1900??
[38]  35 Yu Z, Sun Z. Analysis of multi-scale features of tropical Pacific Ocean sea surface temperature. J Nanjing Inst Meteorol, 2004, 27:193-199
[39]  36 Wang L, Duan J, Chen J, et al. Temperature reconstruction from tree-ring maximum density of Balfour spruce in eastern Tibet, China. Int J Climatol, 2010, 30: 972-979
[40]  37 Michaelsen J. Cross-validation in statistical climate forecast models. J Clim Appl Meteorol, 1987, 26: 1589-1600??
[41]  38 Briffa K R, Jones P D, Schweingruber F H. Summer temperature patterns over Europe: A reconstruction from 1759 AD based on muximum latewood density indices of conifers. Quat Res, 1988, 30: 36-52??
[42]  40 Luckman B H, Briffa K R, Jones P D, et al. Treering based reconstruction of summer temperatures at the Columbia Icefield, Alberta, Canada, AD 1073-1983. Holocene, 1997, 7: 375-389
[43]  42 郑景云, 尹云鹤, 李炳元. 中国气候区划新方案. 地理学报, 2010, 65: 3-12
[44]  44 周秀骥, 赵平, 陈军明, 等. 青藏高原热力作用对北半球气候影响的研究. 中国科学D 辑: 地球科学, 2009, 39: 1473-1486
[45]  45 Davi N, D’Arrigo R, Jacoby G C, et al. Warm-season annual to decadal temperature variability for Hokkaido, Japan, inferred from maximum latewood density (AD 1557-1990) and ring width data (AD 1532-1990). Clim Change, 2001, 52: 201-217
[46]  46 D’Arrigo R, Jacoby G, Pederson N, et al. Mongolian tree-rings, temperature sensitivity and reconstructions of Northern Hemisphere temperature. Holocene, 2000, 10: 669-672??
[47]  47 Mann M, Bradley R, Hughes M. Northern Hemisphere temperatures during the past millennium: Inferences, uncertainties, and limitations. Geophys Res Lett, 1999, 26: 759??
[48]  48 刘实, 王勇, 缪启龙, 等. 近50 年东北地区热量资源变化特征. 应用气象学报, 2010, 21: 266-278

Full-Text

Contact Us

service@oalib.com

QQ:3279437679

WhatsApp +8615387084133