| [1]李吉均,方小敏,潘保田,等.新生代晚期青藏高原强烈隆起及其对周边环境的影响[J].第四纪研究,2001,21(5):381-391.[2]郑度,姚檀栋.青藏高原隆升及其环境效应[J].地球科学进展,2006,21(5):451-458.[3]郑度.青藏高原对中国西部自然环境地域分异的效应[J].第四纪研究,2001,21(6):484-489.[4]刘晓东.青藏高原隆升对亚洲季风形成和全球气候与环境变化的影响[J].高原气象,1999,18(3):321-332.[5]刘晓东,李立,安芷生.青藏高原隆升与欧亚内陆及北非的干旱化[J].第四纪研究,2001,21(2):114-122.[6]范广洲,程国栋.青藏高原隆升对西北干旱气候形成影响的模拟(Ⅰ):对大气环流影响[J].高原气象,2003,22:45-57.[7]Liu X D,Chen B D.Climatic warming in the Tibetan Plateau during recent decades[J].International Journal of Climatology,2000,20:1729-1742.[8]Rangwala I,Miller J R,Xu M.Warming in the Tibetan Plateau:possible influences of the changes in surface water vapor[J].Geophysical Research Letters,2009,36:L06703.[9]Webster P J,Magana V O,Palmer T N,et al.Monsoon:processes,predictability,and the prospects for prediction[J].Journal of Geophysical Research,1998,103(C7):14451-14510.[10]Liang E Y,Shao X M,Xu Y.Tree-ring evidence of recent abnormal warming on the southeast Tibetan Plateau[J].Theoretical and Applied Climatology,2009,98:9-18.[11]Qin C,Yang B,Bruning A,et al.Regional extreme climate events on the northeastern Tibetan Plateau since AD 1450 inferred from tree rings[J].Global and Planetary Change,2011,75:143-154.[12]Yang B,Kang X C,Bruning A,et al.A 622-year regional temperature history of southeast Tibet derived from tree rings[J].The Holocene,2010,20(2):181-190.[13]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].The Holocene,2010,20(8):1235-1245.[14]贾文雄,何元庆,李宗省,等.祁连山及河西走廊气候变化的时空分布特征[J].中国沙漠,2008,28(6):1151-1156.[15]Liu X D,Yin Z Y.Spatial and Temporal Variation of Summer Precipitation over the Eastern Tibetan Plateau and the North Atlantic Oscillation[J].Journal of Climate,2001,14:2896-2909.[16]Chen T R,Yu K F,Li S,et al.Anomalous Ba/Ca signals associated with low temperature stresses in Porites corals from the northern South China Sea[J].Journal of Environmental Sciences,2011,23(9):1452-1459.[17]Tan L,Cai Y,An Z,et al.Climate patterns in north central China during the last 1 800 yr and their possible driving force[J].Climate of the Past,2011,7:685-692.[18]葛全胜,丁玲玲,郑景云,等.利用雨雪分寸重建福州前汛期雨季起始日期研究 [J].地球科学进展,2011,26(11):1200-1207.[19]伍国凤,郝志新,郑景云.南昌1736年以来的降雪与冬季气温变化[J].第四纪研究,2011,31(6):1022-1028.[20]李明启,靳鹤龄,张洪.小冰期气候的研究进展[J].中国沙漠,2005,25(5):731-737.[21]杨保,史峰,Sonechkin D M,等.过去千年气候变化重建研究新进展[J].中国沙漠,2011,31(2):485-491.[22]Fritts H C.Tree Rings and Climate[M].London:Academic Press,1976.[23]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.[24]刘晶晶,杨保.青藏高原南部南木林地区树木径向生长对气候因子的响应[J].中国沙漠,2011,31(6):1527-1534.[25]鲁瑞洁,夏虹.腾格里沙漠南缘油松树轮宽度变化及其对气候因子的响应[J].中国沙漠,2006,26(3):399-402.[26]秦莉,袁玉江,史玉光,等.样条函数步长变化对树轮宽度年表与气候相关性的影响初探[J].中国沙漠,2012,32(1):175-180.[27]申红艳,李林,董安详,等.树轮指示的柴达木盆地近539 a旱涝变化特征[J].中国沙漠,2011,31(4):1059-1064.[28]Devi N,Hagedorn F,Moiseev P,et al.Expanding forests and changing growth forms of Siberian larch at the Polar Urals treeline during the 20th century[J].Global Change Biology,2008,14:1581-1591.[29]Thuiller W,Lavorel S,Arujo M B,et al.Climate change threats to plant diversity in Europe[J].Proceedings of the National Academy of Sciences,2005,102(23):8245-8250.[30]Thomas C D,Cameron A,Green R E,et al.Extinction risk from climate change[J].Nature,2004,427:145-148.[31]Pederson N,Cook E R,Jacoby G C,et al.The influence of winter temperatures on the annual radial growth of six northern range margin species[J].Dendrochronologia,2004,22:7-29.[32]Peng J F,Gou X H,Chen F H,et al.Altitudinal variability of climate-tree growth relationships along a consistent slope of Anyemaqen Mountains,northeastern Tibetan Plateau[J].Dendrochronologia,2008,26(2):87-96.[33]Liang E Y,Shao X M,Eckstein D,et al.Topography- and species-dependent growth responses of Sabina przewalskii and Picea crassifolia to climate on the northeast Tibetan Plateau[J].Forest Ecology and Management,2006,236:268-277.[34]Liang E Y,Wang Y F,Xu Y,et al.Growth variation in Abies georgei var.smithii along altitudinal gradients in the Sygera Mountains,southeastern Tibetan Plateau[J].Trees,2010,24:363-373.[35]Liang E Y,Liu X H,Yuan Y J,et al.The 1920s drought recorded by tree rings and historical documents in the semi-arid and arid areas of northern China[J].Climatic Change,2006,79:403-432.[36]Tian Q H,Gou X H,Zhang Y,et al.Tree-based drought reconstruction (A.D.1855-2001) for the Qilian Mountains,northwestern China[J].Tree Ring Research,2007,63:27-36.[37]Liu J J,Yang B,Qin C.Tree-ring based annual precipitation reconstruction since AD 1480 in south central Tibet[J].Quaternary International,2010,236:75-81.[38]Wang X C,Zhang Q B,Ma K P,et al.A tree-ring record of 500-year dry-wet changes in northern Tibet,China[J].The Holocene,2008,18(4):579-588.[39]Yang B,Qin C,Bruning A,et al.Rainfall history for the Hexi Corridor in the arid northwest China during the past 620 years derived from tree rings[J].International Journal of Climatology,2011,31:1166-1176.[40]Chen F H,Yu Z C,Yang M L,et al.Holocene moisture evolution in arid central Asia and its out-of-phase relationship with Asian monsoon history[J].Quaternary Science Reviews,2008,27(3/4):351-364.[41]杨保.树轮记录的小冰期以来青藏高原气候变化的时空特征[J].第四纪研究,2012,32(1):81-94.[42]Yang B,Kang X C,Liu J J,et al.Annual temperature history in Southwest Tibet during the last 400 years recorded by tree rings[J].International Journal of Climatology,2009,30:962-971.[43]Bruning A,Grieβinger J.Late Holocene variations in monsoon intensity in the Tibetan-Himalayan region-evidence from tree rings[J].Journal of the Geological Society of India,2006,68(3):485-494.[44]Cook E R,Kairiukstis L A.Methods of Dendrochronology[M].Netherlands:Kluwer Academic Press,1990.[45]Rinn F.TSAP-Win:Time Series Analysis and Presentation for Dendrochronology and Related Applications.Version 0.55 User Reference[Z].Heidelberg,Germany,2003.http://www.rimatech.com.[46]Holmes R L.Computer-assisted quality control in tree-ring dating and measurement[J].Tree-Ring Bulletin,1983,43:69-95.[47]Cook E R,Briffa K R,Jones P D.Spatial Regression Methods in Dendroclimatology:applications in the Environmental Science[M].Dordrecht:Kluwer Academic Press,1994.[48]Cook E R,Peters K.Calculating unbiased tree-ring indices for the study of climatic and environmental change[J].The Holocene,1997,7:361-370.[49]Osborn T J,Briffa K R,Jones P D.Adjusting variance for sample-size in tree ring chronologies and other regional-mean time-series[J].Dendrochronologia,1997,15:89-99.[50]Wigley T,Briffa K R,Jones P D.On the average value of correlated time series,with applications in dendroclimatology and hydrometeorology[J].Journal of Applied Meteorology and Climatology,1984,23:201-213.[51]Biondi F,Waikul K.DENDROCLIM2002:a C++ program for statistical calibration of climate signals in tree-ring chronologies[J].Computers and Geosciences,2004,30(3):303-311.[52]Palmer W C.Meteorological drought[R].Washington,D.C:U.S.Department of Commerce,1965.[53]Dai A G,Trenberth K E,Qian T T.A global data set of Palmer Drought Severity Index for 1870-2002:relationship with soil moisture and effects of surface warming[J].Journal of Hydrometeorology,2004,5:1117-1130.[54]Cook E R,Briffa K R,Meko D M,et al.The segment length curse in long tree-ring chronology development for palaeoclimatic studies[J].The Holocene,1995,5:229-237.[55]Liang E Y,Shao X M,Liu X H.Annual precipitation variation inferred from tree rings since AD 1770 for the western Qilian Mts.,northern Tibetan Plateau[J].Tree Ring Research,2009,65(2):95-103.[56]郑淑霞,上官周平.树木年轮与气候变化关系研究[J].林业科学,2006,42(6):100-107.[57]李江风,袁玉江,由希尧,等.树木年轮水文学研究与应用[M].北京:科学出版社,2000.[58]王亚军,陈发虎,勾晓华,等.祁连山中部树木年轮宽度与气候因子的响应关系及气候重建[J].中国沙漠,2001,21(2):136-140.[59]勾晓华,杨梅学,彭剑峰,等.树轮记录的阿尼玛卿山区过去830年夏半年最高温变化[J].第四纪研究,2006,26(6):991-998.[60]王婷,于丹,李江风,等.树木年轮宽度与气候变化关系研究进展[J].植物生态学报,2003,27(1):23-33.[61]Vaganov E A,Hughes M K,Shashkin A V.Growth dynamics of conifer tree rings,imagines of past and future environments[J].Ecological Studies,2005,183:21-104. |
2013, Vol. 33 
