[1] 《气候变化国家评估报告》编写委员会. 气候变化国家评估报告[M]. 北京: 科学出版社, 2007: 10-11.[The Committee of China’s National Assessment Report on Climate Change. China’s National Assessment Report on Climate Change. Beijing: Science Press, 2007: 10-11.][2] 赵宗慈, 王邵武, 罗勇, 等. 近百年气候变暖的不确定性分析[J]. 科技导报, 2009, 27(23): 41-48.[ZHAO Zong-ci, WANG Shao-wu, LUO Yong, et al. Uncertainty analysis of climate warming during the last 100 years. Science & Technology Review, 2009, 27(23): 41-48.][3] 胡汝骥, 马虹, 樊自立, 等. 新疆水资源对气候变化的响应[J]. 自然资源学报, 2002, 17(1): 22-27.[HU Ru-ji, MA Hong, FAN Zi-li, et al. Response of water resources to climate change in Xinjiang. Journal of Nature Resource, 2002, 17(1): 22-27.][4] 邵雪梅. 树轮年代学的若干进展[J]. 第四纪研究, 1997, 17(3): 265-271.[SHAO Xue-mei. Advancement in Dendrochronology. Quaternary Sciences, 1997, 17(3): 265-271.][5] 邵雪梅, 王树芝, 徐岩, 等. 柴达木盆地东北部3500年树轮定年年表的初步建立[J]. 第四纪研究, 2007, 27(4): 477-485.[SHAO Xue-mei, WANG Shu-zhi, XU Yan, et al. A 3500-year master tree-ring dating chronology from the northeastern part of the Qaidam Basin. Quaternary Sciences, 2007, 27(4): 477-485.][6] 刘禹, 王雷, 史江峰, 等. 利用贺兰山北部树轮资料重建过去270年以来6-8月平均干燥指数[J]. 第四纪研究, 2005, 25(5): 540-544.[LIU Yu, WANG Lei, SHI Jiang-feng, et al. Reconstruction of mean drought index from June to August for the last 270 years using tree-ring data in the northern Helan Mountain. Quaternary Sciences, 2005, 25(5): 540-544.][7] 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.[GOU Xiao-hua, YANG Mei-xue, PENG Jian-feng, et al. Maximum Temperature Reconstruction for Anmaqing Mountains over the past 830 years on tree-ring records. Quaternary Sciences, 2006, 26(6): 991-998.][8] 宋慧明, 刘禹, 倪万眉, 等. 以树轮宽度重建九寨沟公元1750年以来冬半年平均最低温度[J]. 第四纪研究, 2007, 27(4): 486-491.[SONG Hui-ming, LIU Yu, NI Wan-mei, et al. Winter mean minimum temperature derived from tree-ring width in Qiuzhaigou Region, China since 1750 A.D. Quaternary Sciences, 2007, 27(4): 486-491.][9] Wilson R, Cook E, D’CArrigo R, et al. Reconstructing ENSO: The influence of method, proxy data, climate forcing and teleconnections [J]. Journal of Quaternary Science, 2009, 25(1): 62-78.[10] Xiao S B, Liu W G, Li A C, et al. Pervasive autocorrelation of the chemical index of alteration in sedimentary profiles and its palaeoenvironmental implications [J]. Sedimentology, 2009, 57(2): 670-676.[11] Sundqvist H S, Holmgren K, Moberg A, et al. Stable isotopes in a stalagmite from NW Sweden document environmental changes over the past 4000 years [J]. Boreas, 2009, 39(1): 77-86.[12] 张利平, 陈小凤, 赵志鹏, 等. 气候变化对水文水资源影响的研究进展[J]. 地理科学进展, 2008, 27(3): 60-67.[ZHANG Li-ping, CHEN Xiao-feng, ZHAO Zhi-peng, et al. Progress in study of climate change impacts on hydrology and water resources. Process in Geography, 2008, 27(3): 60-67.][13] 黄粤, 陈曦, 包安明, 等. 开都河流域山区径流模拟及降雨输入的不确定性分析[J]. 冰川冻土, 2010, 32(3): 567-572.[HUANG Yue, CHEN Xi, BAO An-ming, et al. Distributed hydrological modeling in Kaidu Basin: MIKE-SHE Model calibration and uncertainty estimation. Journal of Glaciology and Geocryology, 2010, 32(3): 567-572.][14] 宋连春, 韩永翔, 孙国武. 中亚和中国西北干旱气候变化特征及其对产业结构的影响[J]. 干旱气象, 2003, 21(3): 43-47.[SONG Lian-chun, HAN Yong-xiang, SUN Guo-wu. The arid climate variable characteristics and its influence on production structure in the central Asia and northwest of China. Arid Meteorology, 2003, 21(3): 43-47.][15] 阿不都斯力木·阿不力克木. 中国新疆与中亚国家农业合作潜力及对策分析[J]. 世界农业, 2010(7): 38-42.[Abduslim Ablikem. The potential of agricultural cooperation and countermeasure analysis between Xinjiang and the central Asia. World Agriculture, 2010(7): 38-42.][16] 中国科学院兰州冰川冻土研究所. 中国冰川目录. Ⅲ, 天山山区(东部散流内流区)[M]. 北京: 科学出版社, 1987: 61-84.[Lanzhou Institute of Glaciology and Geoeryology, CAS. China’s Glaciers Directory: Tianshan Mountains. Beijing: Science Press, 1987: 61-84.][17] 王润, 孙占东, 高前兆. 2002年前后博斯腾湖水位变化和中亚气候[J]. 冰川冻土, 2006, 28(3): 324-329.[WANG Run, SUN Zhan-dong, GAO Qian-zhao. Water level change in bostan lake under climatic variation background of central Asia around 2002. Journal of Glaciology and Geocryology, 2006, 28(3): 324-329.][18] 高华中, 朱诚, 李宗尧. 开都河灌区灌溉引水对博斯腾湖面积影响的定量分析[J]. 自然资源学报, 2005, 20(4): 502-507.[GAO Hua-zhong, ZHU Cheng, LI Zong-yao. Quantitative analysis of the impact of irrigation water from Kaidu River on the area change of Bosten Lake. Journal of Natural Resource, 2005, 20(4): 502-507.][19] 黄粤. 干旱区无资料或缺资料流域水文预报研究. 北京: 中国科学院研究生院, 2009.[HUANG Yue. Distributed Hydraulic Modeling in Arid Ungauged Basin. Beijing: Graduate University of Chinese Academy of Sciences, 2009.][20] Hay L E, Wilby R L, Leavesley G H. A comparision of Delta change and downscaled GCM scenarios for three mountainous basins in the United States [J]. Journal of the American Water Resources Association, 2000, 36(2): 387-397.[21] 赵芳芳, 徐宗学. 统计降尺度方法和Delta方法建立黄河源区气候情景的比较分析[J]. 气象学报, 2007, 65(4): 653-664.[ZHAO Fang-fang, XU Zong-xue. Comparative analysis on downscaled climate scenarios for headwater catchment of Yellow River using SDS and Delta methods. Acta Meteorologica Sinica, 2007, 65(4): 653-664.][22] 郝振纯, 李丽, 徐毅, 等. 区域气候情景Delta-DCSI降尺度方法[J]. 四川大学学报: 工程科学版, 2009, 41(5): 1-7.[HAO Zhen-chun, LI Li, XU Yi, et al. Study on Delta-DCSI downscaling method of GCM output. Journal of Sichuan University: Engineering Science Edition, 2009, 41(5): 1-7.][23] Hotelling H. Relation betweentwo sets of variates [J]. Biometrika, 1936, 28: 139-142.[24] Glahn H R. Canonical correlation and its relationship to discriminate analysis and multiple regressions [J]. Journal of the Atmospheric Science, 1968, 25: 23-31.[25] Barnett T P. Interaction of the monsoon and pacific trade wind systems at interannual time scales, Part I: The equatorial zone [J]. Monthly Weather Review, 1983, 111: 756-773.[26] Nicholls N. The use of canonical correlation to study teleconnections [J]. Monthly Weather Review, 1987, 115: 393-399. |