Liu Q, Yang Z, Cui B. Spatial and temporal variability of annual precipitation during 1961-2006 in Yellow River Basin, China[J]. J Hydrol, 2008, 361: 330-338, doi:10.1016/j.jhydrol.2008.08.002.
Yang J, Tan C, Zhang T. Spatial and temporal variations in air temperature and precipitation in the Chinese Himalayas during the 1971-2007[J]. Int J Climatol, 2013, 33: 2622-2632, doi: 10.1002/joc.3609.
Yang B, Qin C, Wang J, et al. A 3, 500-year tree-ring record of annual precipitation on the northeastern Tibetan Plateau[J]. Proceedings of the National Academy of Sciences, 2014, 111: 2903-2908, doi: 10.1073/pnas.131923811.
[7]
Maussion F, Scherer D, Mlg T, et al. Precipitation seasonality and variability over the Tibetan Plateau as resolved by the High Asia Reanalysis[J]. J Climate, 2014, 27: 1910-1927, doi: 10.1175/JCLI-D-13-00282.1.
[8]
Tong K, Su F, Yang D, et al. Tibetan Plateau precipitation as depicted by gauge observations, reanalyses and satellite retrievals[J]. Int J Climatol, 2014, 34: 265-285, doi: 10.1002/joc.3682.
[9]
Simmonds I, Bi D, Hope P. Atmospheric water vapor flux and its association with rainfall in China in summer[J]. J Climate, 1999, 12: 1353-1367. 2.0.CO;2 target="_blank">
[10]
Liu X, Yin Z Y. Spatial and temporal variation of summer precipitation over the eastern Tibetan plateau and the North Atlantic Oscillation[J]. J Climate, 2001, 14: 2896-2909. 2.0.CO;2 target="_blank">
Webster P J, Yang S. Monsoon and ENSO: Selectively interactive systems[J]. Quart J Roy Meteor Soc, 1992, 118: 877-926, doi: 10.1002/qj.49711850705.
[13]
Saji N H, Goswami B N, Vinayachandran P N, et al. A dipole mode in the tropical Indian Ocean[J]. Nature, 1999, 401: 361-363.
[14]
Chang C P, Zhang Y, Li T. Interannual and interdecadal variations of the East Asian summer monsoon and tropical Pacific SSTs. Part I: roles of the subtropical ridge[J]. J Climate, 2000, 13: 4310-4325. 2.0.CO;2 target="_blank">
[15]
Chang C P, Zhang Y, Li T. Interannual and interdecadal variations of the East Asian summer monsoon and tropical Pacific SSTs. Part II: Meridional structure of the monsoon[J]. J Climate, 2000, 13: 4326-4340. 2.0.CO;2 target="_blank">
[16]
Hong C C, Lu M M, Kanamitsu M. Temporal and spatial characteristics of positive and negative Indian ocean dipole with and without ENSO[J]. J Geophys Res: Atmospheres, 2008, 113, D08107, doi: 10.1029/2007JD009151.
[17]
Yun K S, Seo K H, Ha K J. Relationship between ENSO and northward propagating intraseasonal oscillation in the east Asian summer monsoon system[J]. J Geophys Res: Atmospheres, 2008, 113, D14120, doi: 10.1029/2008JD009901.
[18]
Ju J, Slingo J. The Asian summer monsoon and ENSO[J]. Quart J Roy Meteor Soc, 1995, 121: 1133-1168, doi: 10.1002/qj.49712152509.
[19]
Webster P J, Palmer T N. The past and the future of El Nio[J]. Nature, 1997, 390: 562-564.
[20]
Goswami B N. Interannual variations of Indian summer monsoon in a GCM: external conditions versus internal feedbacks[J]. J Climate, 1998, 11: 501-522. 2.0.CO;2 target="_blank">
[21]
Lau N C, Wang B. Interactions between the Asian monsoon and the El Ni?o Southern Oscillation[M]// Wang B. The Asian monsoon. Chichester: Springer-Praxis, 2006: 479-511.
[22]
Ashok K, Guan Z, Yamagata T. Impact of the Indian Ocean dipole on the relationship between the Indian monsoon rainfall and ENSO[J]. Geophys Res Lett, 2001, 28(23): 4499-4502, doi: 10.1029/2001GLO13294.
[23]
Cherchi A, Navarra A. Influence of ENSO and of the Indian Ocean Dipole on the Indian summer monsoon variability[J]. Climate Dyn, 2013, 41(1): 81-103, doi: 10.1007/s00382-012-1602-y.
[24]
Liebmann B, Hartmann D L. An observational study of tropical midlatitude interaction on intraseasonal time scales during winter[J]. J Atmos Sci, 1984, 41: 3333-3350. 2.0.CO;2 target="_blank">
[25]
Yang S, Lau K M, Yoo S H, et al. Upstream subtropical signals preceding the asian summer monsoon circulation[J]. J Climate, 2004, 17: 4213-4229.
[26]
Zhu X, Bothe O, Fraedrich K. Summer atmospheric bridging between Europe and East Asia: Influences on drought and wetness on the Tibetan Plateau[J]. Quaternary International, 2011, 236: 151-157, doi: 10.1016/j.quaint.2010.06.015.
[27]
Gao Y, Wang H J, Li S. Influences of the Atlantic Ocean on the summer precipitation of the southeastern Tibetan Plateau[J]. J Geophys Res: Atmospheres, 2013, 118: 3534-3544, doi: 10.1002/jgrd.50290.
[28]
Mlg T, Maussion F, Scherer D. Mid-latitude westerlies as a driver of glacier variability in monsoonal high Asia[J]. Nature Climate Change, 2014, 4: 68-73.
[29]
Barnston A G, He Y. Impacts of the NAO on U.S. and Canadian surface climate, implications for seasonal prediction[C]. Proceedings of the 21st Annual Climate Diagnostics and Prediction Workshop, Alabama, USA, 1996: 34-37.
[30]
Jones P D, Conway D. Precipitation in the British Isles: an analysis of area-average data updated to 1995[J]. Int J Climatol, 1997, 17: 427-438. 3.0.CO;2-Q target="_blank">
[31]
Thompson D W J, Wallace J M. The Arctic Oscillation signature in the wintertime geopotential height and temperature fields[J]. Geophys Res Lett, 1998, 25: 1297-1300, doi: 10.1029/98GL00950.
[32]
Brandimarte L, Di Baldassarre G, Bruni G, et al. Relation between the North-Atlantic Oscillation and hydroclimatic conditions in Mediterranean areas[J]. Water Resource Management, 2011, 25: 1269-1279, doi: 10.1007/s11269-010-9742-5.
[33]
Hurrell J W, Van Loon H. Decadal changes in the circulation of the Northern Hemisphere: Relation to surface temperature[C]. Proceedings of the 20th Annual Climate Diagnostics Workshop, Seattle, Washington USA, 1995: 292-295.
[34]
Hurrell J W. Influence of variations in extratropical wintertime teleconnections on Northern Hemisphere[J]. Geophys Res Lett, 1996, 23: 665-668, doi: 10.1029/96GL00459.
[35]
Huang N E, Shen Z, Long S R, et al. The empirical mode decomposition and Hilbert spectrum for nonlinear and nonstationary time series analysis[J]. Proceedings of the Royal Society of London Series A, 1998, 454: 903-995.
[36]
王婷. EMD算法研究及其在信号去噪中的应用[D]. 哈尔滨: 哈尔滨工程大学, 2010.
[37]
Wu Z, Huang N E. Ensemble empirical mode decomposition: a noise-assisted data analysis method[J]. Advances in Adaptive Data Analysis, 2009, 1: 1-41, doi: 10.1142/S1793536909000047.
[38]
Wu Z, Schneider E K, Kirtman B P, et al. The modulated annual cycle: an alternative reference frame for climate anomalies[J]. Climate Dyn, 2008, 31: 823-841, doi: 10.1007/s00382-008-0437-z.
[39]
Qian C, Fu C, Wu Z, et al. On the secular change of spring onset at Stockholm[J]. Geophys Res Lett, 2009, 36, L12706, doi: 10.1029/2009GL038617.
[40]
Franzke C. Long range dependence and climate noise characteristics of Antarctic temperature data[J]. J Climate, 2010, 23: 6074-6081.
[41]
Shi F, Yang B, Gunten L, et al. Ensemble empirical mode decomposition for tree-ring climate reconstructions[J]. Theor Appl Climatol, 2012, 109: 233-243, doi: 10.1007/s00704-011-0576-8.
Hurrell J W, Van Loon H. Decadal variations in climate associated with the North Atlantic Oscillation[J]. Climatic Change, 1997, 36: 301-326, doi: 10.1023/A:1005314315270.
Xu H, Hou Z, Ai L, et al. Precipitation at Lake Qinghai, NE Qinghai-Tibet Plateau, and its relation to Asian summer monsoons on decadal/interdecadal scales during the past 500 years[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2007, 254: 541-549, doi: 10.1016/j.palaeo.2007.07.007.
[51]
Tian L, Ma L, Yu W, et al. Seasonal variations of stable isotope in precipitation and moisture transport at Yushu, eastern Tibetan Plateau[J]. Science in China, 2008, 51: 1121-1128, doi: 10.1007/s11430-008-0089-1.
[52]
Yu W, Ma Y, Sun W, et al. Climatic significance of δ18O records from precipitation on the western Tibetan Plateau[J]. Chinese Science Bulletin, 2009, 54: 2732-2741, doi: 10.1007/s11434-009-0495-6.
[53]
Yao T, Zhou H, Yang X. Indian monsoon influences altitude effect of δ18O in precipitation/river water on the Tibetan Plateau[J]. Chinese Science Bulletin, 2009, 54: 2724-2731, doi: 10.1007/s11434-009-0497-4.
[54]
Wei F Y, Xie Y, Mann M E. Probabilistic trend of anomalous summer rainfall in Beijing: Role of interdecadal variability[J]. J Geophys Res: Atmospheres, 2008, 113, D20106, doi: 10.1029/2008JD010111.
Gu W, Li C Y, Li W J, et al. Interdecadal unstationary relationship between NAO and east China's summer precipitation patterns[J]. Geophys Res Lett, 2009, 36, L13702, doi: 10.1029/2009GL038843.
Bothe O, Fraedrich K, Zhu X. The large-scale circulations and summer drought and wetness on the Tibetan Plateau[J]. Int J Climatol, 2010, 30: 844-855, doi: 10.1002/joc.1946.
[59]
Bothe O, Fraedrich K, Zhu X. Large-scale circulations and Tibetan plateau summer drought and wetness in the high-resolution climate model[J]. Int J Climatol, 2011, 31: 832-846, doi: 10.1002/joc.2124.
[60]
Liu Huancai, Duan Keqin, Li Man, et al. Impact of the North Atlantic Oscillation on the Dipole Oscillation of summer precipitation over the central and eastern Tibetan Plateau[J]. Int J Climatol, 2015, doi: 10.1002/joc.4304.
Wu Z W, Wang B, Li J P, et al. An empirical seasonal prediction model of the east Asian summer monsoon using ENSO and NAO[J]. J Geophys Res: Atmospheres, 2009, 114, D18120, doi: 10.1029/2009JD011733.
[64]
Gu W, Li C Y, Wang X, et al. Linkage between Meiyu precipitation and North Atlantic SST on the decadal time scale[J]. Adv Atmos Scis, 2009, 26(1): 101-108, doi: 10.1007/s00376-009-0101-5.
[65]
Zuo J Q, Li W J, Sun C H, et al. Impact of North Atlantic sea surface temperature tripole on the East Asian summer monsoon[J]. Adv Atmos Sci, 2013, 30(4): 1173-1186, doi: 10.1007/s00376-012-2125-5.
[66]
Bjerkness J. Atlantic air-sea interation[J]. Adv Geophys, 1964, 10: 1-82.