[1]Bao X H, Zhang F Q.2013.Evaluation of NCEP-CFSR, NCEP-NCAR, ERA-Interim and ERA-40 reanalysis datasets against independent sounding observations over the Tibetan Plateau[J].J Climate, 26(1): 206-214.
[2]Bradley R S, Keimig F T, Diaz H F, et al.2009.Recent changes in freezing level heights in the tropics with implications for the deglacierization of high mountain regions[J].Geophys Res Lett, 36(17): L17701.DOI: 10.1029/2009GL037712.
[3]Dee D P, Uppala S M, Simmons A J, et al.2011.The ERA-Interim reanalysis: Configuration and performance of the data assimilation system[J].Quart J Roy Meteor Soc, 137(656): 553-597.
[4]Diaz H F, Eischeid J K, Duncan C, et al.2003.Variability of freezing levels, melting season indicators and snow coverfor selected high-elevation and continental regions in the last 50 years[J].Climatic Change, 59(1-2): 33-52.
[5]Diaz H F, Graham N E.1996.Recent changes in tropical freezing heights and the role of sea surface temperature[J].Nature, 383(6596): 152-155.
[6]Dong L, Zhang M, Wang S, et al.2015.The freezing level height in the Qilian Mountains, northeast Tibetan Plateau based on reanalysis data and observations, 1979-2012[J].Quaternary International, 380-381: 60-67.DOI: 10.1016/j.quaint.2014.08.049.
[7]Folkins I.2013.The melting level stability anomaly in thetropics[J].Atmos Chem Phys, 13(3): 1167-1176.
[8]Kang S C, Xu Y W, You Q L, et al.2010.Review of climate and cryospheric change in the Tibetan Plateau[J].Environ Res Lett, 5(1): 015101.DOI: 10.1088/1748-9326/5/1/015101.
[9]Kendall M R.1955.Rank Correlation Methods[M].London: Charles Griffin.
[10]Liu Z F, Xu Z X, Yao Z J, et al.2012.Comparison of surface variables from ERA and NCEP reanalysis with station data over eastern China[J].Theor Appl Climatol, 107(3-4): 611-621.
[11]Mann H B.1945.Nonparametric tests against trend[J].Econometrica: Journal of the Econometric Society, 13(3): 245-259.
[12]Ohmura A, Kasser P, Funk M.1992.Climate at the equilibrium line of glaciers[J].Journal of Glaciology, 38(130): 397-411.
[13]Pepin N C, Seidel D J.2005.A global comparison of surface and free-air temperatures at high elevations[J].J Geophys Res, 110(D3): D03104.DOI: 10.1029/2004JD005047.
[14]Sen P K.1968.Estimates of the regression coefficient based on Kendall's tau[J].Journal of the American Statistical Association, 63(324): 1379-1389.
[15]Simmons A J, Jones P D, Da Costa Bechtold V, et al.2004.Comparison of trends and low-frequency variability in CRU, ERA-40, and NCEP/NCAR analyses of surface air temperature[J].J Geophys Res, 109(D24): D24115.DOI: 10.1029/2004JD 005306.
[16]Wang S, Zhang M, Pepin N C, et al.2014.Recent changes in freezing level heights in High Asia and their impact on glacier changes[J].J Geophys Res, 119(4): 1753-1765.
[17]Wang X L.2008a.Accounting for autocorrelation in detecting mean shifts in climate data series using the penalized maximal t or F test[J].J Appl Meteor Climatol, 47(9): 2423-2444.
[18]Wang X L.2008b.Penalized maximal F test for detecting undocumented mean shift without trend change[J].J Atmos Ocean Technol, 25(3): 368-384.
[19]Yao T, Thompson L, Yang W, et al.2012.Different glacier status with atmospheric circulations in Tibetan Plateau and surroundings[J].Nature Climate Change, 2(9): 663-667.
[20]You Q L, Fraedrich K, Ren G, et al.2013.Variability of temperature in the Tibetan Plateau based on homogenized surface stations and reanalysis data[J].Int J Climatol, 33(6): 1337-1347.
[21]Zhang G X, Sun S F, Ma Y F, et al.2010.The response of annual runoff to the height change of the summertime 0 ℃ level over Xinjiang[J].Journal of Geographical Sciences, 20(6): 833-847.
[22]Zhang M J, Wang S J, Li Z Q, et al.2012.Glacier area shrinkage in China and its climatic background during the past half century[J].Journal of Geographical Sciences, 22(1): 15-28.
[23]Zhang Y S, Guo Y.2011.Variability of atmospheric freezing-level height and its impact on the cryosphere in China[J].Annals of Glaciology, 52(58): 81-88.
[24]白磊, 王维霞, 姚亚楠, 等.2013.ERA-Interim和NCEP/NCAR再分析数据气温和气压值在天山山区适用性分析[J].沙漠与绿洲气象, 7(3): 51-56.
[25]Bai Lei, Wang Weixia, Yao Yanan, et al.2013.Reliability of NCEP/NCAR and ERA-Interim reanalysis date on Tianshan Mountainous Area[J].Desert Oasis Meteor, 7(3): 51-56.
[26]曹丽娟, 鞠晓慧, 刘小宁.2010.PMFT方法对我国年平均风速的均一性检验[J].气象, 36(10): 52-56.
[27]Cao Lijuan, Ju Xiaohui, Liu Xiaoning.2010.Penalized maximal F test for the homogeneity study of the annual mean wind speed over China[J].Meteor Mon, 36(10): 52-56.
[28]高路, 陈兴伟, 林广发.2014.基于ERA-Interim再分析资料的中国极端气温分析[J].南水北调与水利科技, 12(2): 75-78.
[29]Gao Lu, Chen Xingwei, Lin Guangfa.2014.Analysis of extreme temperatures in China based on ERA-Interim reanalysis Date[J].South-to-North Water Transfers and Water Science & Technology, 12(2): 75-78.
[30]高路, 郝璐.2014.ERA-Interim气温数据在中国区域的适用性评估[J].亚热带资源与环境学报, 9(2): 75-81.
[31]Gao Lu, Hao Lu.2014.Verification of ERA-Interim Reanalysis Date over China[J].Journal of Subtropical Resources and Environment, 9(2): 75-81.
[32]宫恒瑞, 石玉, 冯志敏.2010.春季融雪期0 ℃层高度与乌鲁木齐河径流量的关系[J].干旱区研究, 27(1): 69-74.
[33]Gong Hengrui, Shi Yu, Feng Zhimin.2010.Relationship between the 0 ℃ layer height and the streamflow of the Urumqi River in the period of spring snowmelt[J].Arid Zone Research, 27(1): 69-74.
[34]胡增运, 倪勇勇, 邵华, 等.2013.CFSR, ERA-Interim和MERRA降水资料在中亚地区的适用性[J].干旱区地理, 36(4): 700-708.
[35]Hu Zengyun, Ni Yongyong, Shao Hua, et al.2013.Applicability study of CFSR, ERA-Interim and MERRA precipitation estimates in Central Asia[J].Arid Land Geography, 36(4): 700-708.
[36]黄小燕, 张明军, 王圣杰, 等.2011.中国西北地区近50年夏季0 ℃层高度及气温时空变化特征[J].地理学报, 66(9): 1191-1199.
[37]Huang Xiaoyan, Zhang Mingjun, Wang Shengjie, et al.2011.Variation of 0 ℃ isotherm height and ground temperature in Summer in Northwest China during the past 50 years[J].Journal of Geographical Sciences, 66(9): 1191-1199.
[38]江吉喜, 范梅珠.2002.夏季青藏高原上的对流云和中尺度对流系统[J].大气科学, 26(2): 263-270.
[39]Jiang Jixi, Fan Meizhu.2002.Convective clouds and mesoscale convective systems over the Tibetan Plateau in summer[J].Chinese J Atmos Sci, 26(2): 263-270.
[40]康兴成.1996.小冰期以来高亚洲地区的气候变化[J].冰川冻土, 18(增刊): 289-295.
[41]Kang Xingcheng.1996.Climate changes in the Qing-Zang Plateau Area since the little ice age[J].Journal of Glaciology and Geocryology, 18(Suppl): 289-295.
[42]刘时银, 丁永建, 叶佰生, 等.2000.高亚洲地区冰川物质平衡变化特征研究[J].冰川冻土, 22(2): 98-105.
[43]Liu Shiyin, Ding Yongjian, Ye Baisheng, et al.2000.Regional characteristics of glacier mass balance variations in High Asia[J].Journal of Glaciology and Geocryology, 22(2): 98-105.
[44]毛炜峄, 吴钧, 陈春艳.2004.0 ℃层高度与夏季阿克苏河洪水的关系[J].冰川冻土, 26(6): 697-704.
[45]Mao Weiyi, Wu Jun, Chen Chunyan.2004.Relationship of 0 ℃ level height and summer flood of AKsu River, Xinjiang[J].Journal of Glaciology and Geocryology, 26(6): 697-704.
[46]王立伟, 张明军, 高峰.2014.1977-2010年长江源区夏季大气0 ℃层高度变化[J].高原气象, 33(3): 769-774.
[47]Wang Liwei, Zhang Mingjun, Gao Feng.2014.Variation of 0 ℃ atmospheric height in the headwaters of Changjiang River in summer during 1977-2010[J].Plateau Meteor, 33(3): 769-774.DOI: 10.7522/j.issn.1000-0534.2014.00048.
[48]王圣杰, 张明军, 李忠勤, 等.2011.近50年来中国天山冰川面积变化对气候的相应[J].地理学报, 66(1): 38-46.
[49]Wang Shengjie, Zhang Mingjun, Li Zhongqin, et al.2011.Response of Glacier Area variation to climate change in Chinese Tianshan Mountains in the past 50 years[J].Journal of Geographical Sciences, 66(1): 38-46.
[50]谢自楚, 刘潮海.2010.冰川学导论[M].上海:上海科学普及出版社,
[51]Xie Zichu, Liu Chaohai.2010.Introduction to glaciology[M].Shanghai: Shanghai popular science press.
[52]谢自楚, 周宰根, 李巧媛, 等.2009.高亚洲冰川系统物质平衡特征及其对全球变化响应研究进展与展望[J].地球科学进展, 24(10): 1065-1072.
[53]Xie Zichu, Zhou Zaigen, Li Qiaoyuan, et al.2009.Progress and prospects of mass balance characteristic and responding to global change of glacier system in High Asia[J].Adv Earth Sci, 24(10): 1065-1072.
[54]姚檀栋, 刘时银, 蒲健辰, 等.2004.高亚洲冰川的近期退缩及其对西北水资源的影响[J].中国科学: D辑, 34(6): 535-543.
[55]Yao Tandong, Liu Shiyin, Pu Jianchen, et al.2004.Recent glacial retreat in High-Asia in China and its impact on water resources in Northwest China[J].Science in China: Series D, 2004, 34(6): 535-543.
[56]赵玉春, 王叶红.2010.高原涡诱生西南涡特大暴雨成因的个例研究[J].高原气象, 29(4): 819-831.
[57]Zhao Yuchun, Wang Yehong.2010.A case study on Plateau Vortex inducing Southwest Vortex and producing extremely heavy rain[J].Plateau Meteor, 29(4): 819-831.