Eichler A, Olivier S,Henderson K et al.Temperature response in the Altai region lags solar forcing.Geophysical Research Letters,2009, 36 (L01808),doi: 10.1029/2008GL035930
[2]
Moore G W K, Holdsworth G,Alverson K.Extratropical response to ENSO as expressed in an ice core from the Saint Elias mountain range. Geophysical Research Letters,2001, 28 (18):3457～3460
[3]
Bradley R S, Vuille M,Hardy D et al.Low latitude ice cores record Pacific sea surface temperatures.Geophysical Research Letters,2003, 30 (4),1174,doi: 10.1029/2002GL016546
[4]
Knüsel S, Brütsch S,Henderson K A et al.ENSO signals of the twentieth century in an ice core from Nevado Illimani,Bolivia.Journal of Geophysical Research,2005, 110 (D01102),doi: 10.1029/2004JD005420
[5]
Seimon A. Improving climatic signal representation in tropical ice cores: A case study from the Quelccaya Ice Cap,Peru.Geophysical Research Letters,2003, 30 (14),1772,doi: 10.1029/2003GL017191
Vuille M. Atmospheric circulation over the Bolivian Altiplano during dry and wet periods and extreme phases of the southern Oscillation. International Journal of Climatology,1999, 19 (14):1579～1600 3.0.CO;2-N target="_blank">
Wang Ninglian.Variations in net accumulation rate of the Malan ice core from the northern Tibetan Plateau over the period of 1887 though 1998 and their relationship to solar activity. Quaternary Sciences, 2009, 29 (5):913～919
[10]
Duan Keqin, Wang Ninglian,Li Yuefang et al.Accumulation in Dasuopu ice core in Qinghai Tibet Plateau and solar activity.Chinese Science Bulletin,2000, 45 (11):1038～1042
[11]
Wang Ninglian, Jiang Xi,Thompson L G et al.Accumulation rates over the past 500 years recorded in ice cores from the northern and southern Tibetan Plateau,China.Arctic,Antarctic,and Alpine Research,2007, 39 (4):671～677
Zhang Dongqi,Qin Dahe,Hou Shugui et al.Net accumulation rate of the East Rongbuk glacier and Indian summer monsoon rainfall.Journal of Glaciology and Geocryology,2004, 26 (2):129～134
[14]
Zhang Xinping,Yao Tandong,Jin Huijun.The influence of ENSO event on the modern δ18O on the Guliya Ice Core.Journal of Glaciology and Geocryology,2000, 22 (1):23～28
[15]
Wang N L, Thompson L G,Davis M E et al.Influence of variations in NAO and SO on air temperature over the northern Tibetan Plateau as recorded by δ18O in the Malan ice core.Geophysical Research Letters,2003, 30 (22),2167,doi: 10.1029/2003GL018188
[16]
Yang M X, Yao T D,He Y Q et al.ENSO events recorded in the Guliya ice core.Climatic Change,2000, 47 (4):401～409
Liu Yaping,Hou Shugui,Ren Jiawen et al.Distribution features of borehole temperatures in the Miaoergou flat-topped glacier,east Tianshan Mountains.Journal of Glaciology and Geocryology,2006, 28 (5):668～671
[19]
Liu Y, Hou S,Hong S et al.High-resolution trace element records of an ice core from the eastern Tien Shan,Central Asia,since 1953 AD. Journal of Geophysical Research,2011, 116 (D12307),doi: 10.1029/2010JD015191
Tian Lide,Yao Tandong,Yu Wusheng et al.Stable isotopes of precipitation and ice core on the Tibetan Plateau and moisture transports.Quaternary Sciences,2006, 26 (2):145～152
[22]
Wang Yetang, Hou Shugui,Liu Yaping.Glacier change in the Karlik Shan,eastern Tien Shan during 1971/72～2001/02.Annals of Glaciology,2009, 50 (53):1～7
Song Linlin,Hou Shugui,Liu Yaping.δ18O record of the Miaoergou ice core from the Karlik Mountains,East Tien Shan,since 1953A.D.Journal of Lanzhou University(Natural Sciences),2011, 47 (5):36～41
[25]
Vachon R W, Welker J M,White J W C et al.Moisture source temperatures and precipitation δ18O-temperature relationships across the United States.Water Resources Research,2010, 46 (W07523),doi: 10.1029/2009WR008558
[26]
Thompson D W J, Wallace J M.Regional climate impacts of the northern Hemisphere annular mode.Science,2001, 293 :85～89
Wang Ninglian.The boundary between the northern and southern Tibetan Plateau with different variations in the warm season air temperatures on the decadal time scale.Quaternary Sciences,2006, 26 (2):165～172
Kang Shichang,Qin Dahe,Ren Jiawen et al.Relationships between an ice core records from southern Tibetan Plateau and atmospheric circulation over Asia.Quaternary Sciences,2006, 26 (2):153～164
[31]
Grigholm B, Mayewski P A,Kang S et al.Atmospheric soluble dust records from a Tibetan ice core: Possible climate proxies and teleconnection with the Pacific Decadal Oscillation.Journal of Geophysical Research,2009, 114 (D20118),doi: 10.1029/2008JD011242
[32]
Anouk de Brauwere, Fjo De Ridde,Rik Pintelon et al.A comparative study of methods to reconstruct a periodic time series from an environmental proxy record.Earth-Science Reviews,2009, 95 (3～4):97～118
[33]
Ashok K, Guan Z,Saji N H et al.Individual and combined influences of the ENSO and Indian Ocean Dipole on the Indian summer monsoon.Journal of Climate,2004, 17 (16):3141～3155 2.0.CO;2 target="_blank">
[34]
Kumar K K, Rajagopalan B,Hoerling M et al.Unraveling the mystery of Indian monsoon failure during El Ni？o. Science,2006, 314 :115～119
[35]
Vuille M, Werner M,Bradley R S et al.Stable isotopes in precipitation in the Asian monsoon region.Journal of Geophysical Research,2005, 110 (D23108),doi: 10.1029/2005JD006022
[36]
Brown J, Simmonds I,Noone D.Modeling δ18O in tropical precipitation and the surface ocean for present-day climate. Journal of Geophysical Research,2006, 111 (D05105),doi: 10.1029/2004JD005611
[37]
Lenters J D, Cook K H.On the origin of the Bolivian high and related circulation features of the South American climate. Journal of the Atmospheric Sciences,1997, 54 (5):656～677 2.0.CO;2 target="_blank">
[38]
Garreaud R D, Aceituno P.Interannual rainfall variability over the South American Altiplano.Journal of Climate,2001, 14 (12):2779～2789 2.0.CO;2 target="_blank">
