| [1]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(8):1166-1176.[2]Zhang Y,Tian Q,Gou X,et al.Annual precipitation reconstruction since AD 775 based on tree rings from the Qilian Mountains,northwestern China[J].International Journal of Climatology,2011,31(3):371-381.[3]Kang S Y,Yang B,Qin C.Recent tree-growth reduction in north central China as a combined result of a weakened monsoon and atmospheric oscillations[J].Climatic Change,2012,115:519-536.[4]Fang K Y,Gou X H,Chen F H,et al.Tree-ring based drought reconstruction for Guiqing Mountain (China):linkage to the Indian and Pacific Oceans[J].International Journal of Climatology,2010,30:1137-1145.[5]Chen F,Yuan Y J,Wei W S,et al.Temperature reconstruction from tree-ring maximum latewood density of Qinghai spruce in middle Hexi Corridor,China[J].Theoretical and Applied Climatology,2011,107:633-643.[6]Chen F,Yuan Y J,Wei W S.Climatic response of Picea crassifolia tree-ring parameters and precipitation reconstruction in the western Qilian Mountains,China[J].Journal of Arid Environments,2011,75:1121-1128.[7]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.[8]陈峰,袁玉江,魏文寿,等.树轮记录的甘肃山丹近224年降水变化[J].地理与地理信息科学,2010,26(5):82-86.[9]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.[10]陈峰,袁玉江,魏文寿,等.树轮记录的酒泉近240 a来的6-9月气温变化[J].干旱区研究,2012,29(1):47-54.[11]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 1450-2006[J].Holocene,2010,20(8):1235-1245.[12]马宁,王乃昂,朱金峰,等.巴丹吉林沙漠周边地区近50 a来气候变化特征[J].中国沙漠,2011,31(6):1541-1547.[13]郭小芹,刘明春.河西走廊近40 a气候生产潜力特征研究[J].中国沙漠,2011,31(5):1323-1329.[14]王素萍,张存杰,韩永翔.甘肃省不同气候区蒸发量变化特征及其影响因子研究[J].中国沙漠,2010,30(3):675-680.[15]李鸣骥,石培基.黑河流域张掖市近38a以来气候变化特征分析[J].中国沙漠,2007,27(6):1048-1054.[16]成爱芳,赵景波,冯起.甘肃陇中地区清代干旱灾害与气候变化研究[J].中国沙漠,2011,31(6):1611-1616.[17]Holmes R L.Computer-assisted quality control in tree-ring dating and measurement[J].Tree-Ring Bulletin,1983,43:69-75.[18]Cook E R.A Time Series Analysis Approach to Tree-ring Standardization[D].Tucson:The University of Arizona, 1985.[19]魏凤英.现代气候统计诊断与预测技术[M].北京:气象出版社,2007.[20]Chen F,Yuan Y J,Wei W S,et al.Reconstructed temperature for Yongan,Fujian,Southeast China:Linkages to the Pacific Ocean climate variability[J].Global and Planetary Change,2012,86/87:11-19.[21]陈峰,袁玉江,魏文寿,等.树轮记录的过去384 a乌鲁木齐河源7月温度变化[J].冰川冻土,2011,33(1):55-63.[22]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.[23]陈峰,袁玉江,魏文寿,等.特克斯河流域近236 a降水变化及其趋势分析[J].山地学报,2010,28(5):545-551.[24]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,2000:51-124.[24]刘禹,史江峰,Shishov V,等.以树轮晚材宽度重建公元1726年以来贺兰山北部5~7月降水量[J].科学通报,2004,49(3):256-269.[26]袁林.西北灾荒史[M].兰州:甘肃人民出版社,1994:479-618.[27]Li J,Chen F,Cook E,et al.Drought reconstruction for north central China from tree rings:the value of the Palmer drought severity index[J].International Journal of Climatology,2007,27:903-909.[28]李栋梁,刘德祥.甘肃气候[M].北京:气象出版社,2000.[29]朱炳瑗,李栋梁.ENSO现象与甘肃省夏季降水[J].高原气象,1989,8(1):64-69.[30]Rittenour T M,Brigham-Grette J,Mann M E.El Nio-like climate teleconnections in New England during the late Pleistocene[J].Science,2000,288(12):1039-1042.[31]Huber M,Caballero R.Eocene El Nio:evidence for robust tropical dynamics in the "Hothouse"[J].Science,2003,299(7):877-881.[32]Yi L,Yu H,Xu X,et al.Exploratory precipitation in North-Central China during the past four centuries[J].Acta Geologica Sinica-English Edition,2010,84(1):223-229.[33]Wang HJ.The weakening of the Asian monsoon circulation after the end of 1970s[J].Advances in Atmospheric Sciences,2001,18:376-386.[34]刘海文,周天军,朱玉祥,等.东亚夏季风自20世纪90年代初开始恢复增强[J].科学通报,2012,57(9):765-769. |
2013, Vol. 33 
