[1] BERGGREN R, GIBBS W J, NEWTON C W. Observational Characteristics of the Jet Stream [Z]. WMO Technical Note, 1958.
[2] ENDLICH R M, MCLEAN G S. The structure of the jet stream core [J]. J Atmos Sci, 1957, 14(6): 543-552, https://doi.org/10.1175/1520-0469(1957)0142.0.CO;2. http://d.old.wanfangdata.com.cn/OAPaper/oai_arXiv.org_astro-ph%2f9411106
[3] HUANG S S, YU Z H. On the structure of the sub-tropical highs and some associated aspects of the general circulation of atmosphere [J]. Acta Meteor Sinica, 1962, 31(4): 67-87 (in Chinese). http://en.cnki.com.cn/Article_en/CJFDTOTAL-QXXB1962S1005.htm
[4] GAO S T, TAO S Y, DING Y H. Generalized E-P flux characterizing wave-flow interaction [J]. Sci China (Series B), 1989, 19(7): 774-784 (in Chinese). https://www.researchgate.net/publication/296551690_The_generalized_E-P_flux_of_wave-meanflow_interactions
[5] GAO S T, TAO S Y, DING Y H. Upper wave-East Asian jet interaction during the period of cold wave outbreak [J]. Chin J Atmos Sci, 1992, 16(6): 718-724 (in Chinese), https://doi.org/10.3878/j.issn.1006-9895.1992.06.09.
[6] PATRICK K. Novel Perspectives of Jet-Stream Climatologic and Events of Heavy Precipitation on the Alpine Southside [D]. Zurich: Swiss Federal Institute of Technology (ETH), 2004.
[7] DING Y H, ZHAO S M, HE S X. Study on the multi-year average circulation of global tropical and subtropical 200 hPa from May to October (Ⅰ) - Planet-scale circulation system [J]. Chin J Atmos Sci, 1988, 12(2): 174-181 (in Chinese), https://doi.org/10.3878/j.issn.1006-9895.1988.02.09.
[8] TAN J L, JIANG J, YUAN J P. The seasonal, interannual and interdecadal variations of the intensity of different subtropical upper jet-stream centers [J]. Scientia Meteor Sinica, 2009, 29(4): 482-489 (in Chinese), https://doi.org/10.1016/S1003-6326(09)60084-4. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=qxkx200904008
[9] LAU K M, BOYLE J S. Tropical and extratropical forcing of the large-scale circulation: A diagnostic study [J]. Mon Wea Rev, 1987, 115(2): 400-428, https://doi.org/10.1175/1520-0493(1987)115<0400:taefot>2.0.co;2. doi: 10.1175/1520-0493(1987)115<0400:TAEFOT>2.0.CO;2
[10] TAO S Y, WEI J. The westward northward advance of the subtropical high over the West Pacific in summer [J]. J Appl Meteor Sci, 2006, 17(5): 513-525 (in Chinese), https://doi.org/10.3969/j.issn.1001-7313.2006.05.001. http://en.cnki.com.cn/Article_en/CJFDTotal-YYQX200605000.htm
[11] YE D Z, TAO S Y, LI M C. The abrupt change of circulation over northern hemisphere during June and October [J]. Acta Meteor Sinica, 1958, 29(4): 27-41 (in Chinese).
[12] SHENG C Y. General Climate in China [M]. Beijing: Science Press, 1986 (in Chinese).
[13] CHEN L X. The structure of the East Asian monsoon circulation system and its medium-term changes [J]. Acta Oceanologica Sinica, 1984, 6(6): 744-758 (inChinese).
[14] CHEN L X, ZHU Q G, LUO H B. East Asian Monsoon[M].Beijing: China Meteorological Press, 1991: 362 (in Chinese).
[15] TAO S Y, CHEN L X. The structure of general circulation over continent of Asia in summer [J]. Acta Meteor Sinica, 1957, 28: 233-247 (in Chinese), https://doi.org/10.11676/qxxb1957.019. http://en.cnki.com.cn/Article_en/CJFDTOTAL-QXXB195703005.htm
[16] TAO S Y, ZHAO S X, ZHOU X P, et al. The research progress of the synoptic meteorology and synoptic forecast [J]. Chin J Atmos Sci, 2003, 27(4): 451-467 (in Chinese), https://doi.org/10.3878/j.issn.1006-9895.2003.04.03. http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQXK200304002.htm
[17] LI C Y, WANG Z T, LIN S Z, et al. The relationship between East Asian summer monsoon activity and northward jump of the upper westerly jet location [J]. Chin J Atmos Sci, 2004, 28(5): 641-658 (in Chinese), https://doi.org/10.3878/j.issn.1006-9895.2004.05.01. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=daqikx200405001
[18] KUANG X Y, ZHANG Y C. Impact of the position abnormalities of East Asian subtropical westerly jet on summer precipitation in middle-lower reaches of Yangtze River [J]. Plateau Meteor, 2006, 25(3): 382-389 (in Chinese), https://doi.org/10.3321/j.issn:1000-0534.2006.03.004. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gyqx200603004
[19] JIN R H, LI W J, ZHANG B, et al. A study of the relationship between East Asia subtropical westerly jet and abnormal Meiyu in the middle-lower reaches of the Yangtze River [J]. Chin J Atmos Sci, 2012, 36(4): 722-732 (in Chinese), https://doi.org/10.3878/j.issn.1006-9895.2011.11076. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=daqikx201204006
[20] GUO H, ZHANG Q Y. The dominant modes of precipitation anomalies in Eastern China during the peak of pre-rainy season in South China and possible causes[J]. Climatic Environ Res, 2016, 21(6): 633-652 (in Chinese), https://doi.org/10.3878/j.issn.1006-9585.2016.16032. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=qhyhjyj201606002
[21] ZHANG Q Y, XUAN S L, SUN S Q. Anomalous circulation characteristics of intraseasonal variation of East Asian subtropical westerly jet in summer and precursory signals [J]. Chin J Atmos Sci, 2018, 42(4): 935-950 (in Chinese), https://doi.org/10.3878/j.issn.1006-9895.1803.18107. http://d.old.wanfangdata.com.cn/Periodical/daqikx201804015
[22] HOSKINS B J, KAROLY D J. The steady linear response of a spherical atmosphere to thermal and orographic forcing [J]. J Atmos Sci, 1981, 38(6): 1179-1196, https://doi.org/10.1175/1520-0469(1981)038<1179:TSLROA>2.0.co;2. doi: 10.1175/1520-0469(1981)038<1179:TSLROA>2.0.CO;2
[23] HOSKINS B J, AMBRIZZI T. Rossby wave propagation on a realistic longitudinally varying flow [J]. J Atmos Sci, 1993, 50(12): 1661-1671, https://doi.org/10.1175/1520-0469(1993)050<1661:rwpoar>2.0.co;2. doi: 10.1175/1520-0469(1993)050<1661:RWPOAR>2.0.CO;2
[24] AMBRIZZI T, HOSKINS B J, HSU H H. Rossby wave propagation and teleconnection patterns in the austral winter [J]. J Atmos Sci, 1995, 52(21): 3661-3672, https://doi.org/10.1175/1520-0469(1995)052<3661:RWPATP>2.0.CO;2. doi: 10.1175/1520-0469(1995)052<3661:RWPATP>2.0.CO;2
[25] CHANG E K M. Characteristics of wave packets in the upper troposphere, Part Ⅱ: Seasonal and hemispheric variations [J]. J Atmos Sci, 1999, 56(11): 1729-1747, https://doi.org/10.1175/1520-0469(1999)056<1729:cowpit>2.0.co;2. doi: 10.1175/1520-0469(1999)056<1729:COWPIT>2.0.CO;2
[26] TERAO T. The zonal wavelength of the quasi-stationary Rossby wave trapped in the westerly jet [J]. J Meteor Soc Japan, 1999, 77: 687-699, https://doi.org/10.2151/jmsj1965.77.3_687.
[27] LU R Y, OH J H, KIM B J: A teleconnection pattern in upper-level meridional wind over the North African and Eurasian continent in summer [J]. Tellus, 2002, 54A: 44-55, https://doi.org/10.3402/tellusa.v54i1.12122. https://www.researchgate.net/publication/229672949_A_teleconnection_pattern_in_upper-level_meridional_wind_over_the_North_African_and_Eurasian_continent_in_summer
[28] NITTA T. Convective activities in the tropical western Pacific and their impact on the northern hemisphere summer circulation [J]. J Meteor Soc Japan, 1987, 65(3): 373-390. doi: 10.2151/jmsj1965.65.3_373
[29] HUANG R H, LI W J. Influence of the heat source anomaly over the tropical western Pacific on the subtropical high over East Asia [C]// International Conference on the General Circulation of East Asia. Chengdu: Institute of Atmospheric Physics, Chinese Academy of Sciences, 1987: 40-51. https://www.researchgate.net/publication/313062662_Influence_of_the_heat_source_anomaly_over_the_tropical_western_Pacific_on_the_subtropical_high_over_East_Asia
[30] HUANG R H, SUN F Y. Interannual variation of the summer teleconnection pattern over the Northern Hemisphere and its numerical simulation [J]. Chin J Atmos Sci, 1992, 16(1): 52-61 (in Chinese), https://doi.org/10.3878/j.issn.1006-9895.1992.01.08. http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQXK199201007.htm
[31] HUANG R H, SUN F Y. Impacts of the thermal state and the convective activities in the tropical western warm pool on the summer climate anomalies in East Asia [J]. Chin J Atmos Sci, 1994, 18(2): 141-151 (in Chinese), https://doi.org/10.1007/BF02658170. http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQXK199402001.htm
[32] TAO S Y, WEI J, LIANG F, et al. Analysis of high impact weather induced by the downstream effect of Rossby waves [J]. Meteor Mon, 2010, 36(7): 81-93 (in Chinese), https://doi.org/10.7519/j.issn.1000-0526.2010.7.015. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=qx201007014
[33] MEI S L, GUAN Z Y. Propagation of baroclinic wav packets in upper troposphere during the Meiyu period of 1998 over middle and lower reaches of Yangtze river valley [J]. J Trop Meteor, 2009, 25(3): 300-306(in Chinese), https://doi.org/10.3969/j.issn.1004-4965.2009.03.007.
[34] XU J P, WANG W, CAI X J, et al. A Comparison of the Rossby wave activities and circulation features of the drought in winter-spring of 2011 and in summer of 2013 over mid-lower reaches of the Yangtze river basin [J]. J Trop Meteor, 2017, 33(6): 992-999 (in Chinese), https://doi.org/10.16032/j.issn.1004-4965.2017.06.020. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=rdqxxb201706020
[35] KALNAY E, KANAMITSU M, KISTLER R, et al. The NCEP / NCAR 40-year reanalysis project [J]. Bull Amer Meteor Soc, 1996, 77(3): 437-471, https://doi.org/10.1175/1520-0477(1996)077<0437:TNYRP>2.0.CO;2. doi: 10.1175/1520-0477(1996)077<0437:TNYRP>2.0.CO;2
[36] XU Q, YANG Y W, YANG Q M. The Meiyu in middle-lower reaches of Yangtze River during 116 recent years(Ⅰ) [M]// LIU Z C(ed), Torrential Rain · Disaster. Beijing: China Meteorological Press, 2001: 44-53 (in Chinese).
[37] JIN R H. Middle-Range Variation of The East Asian Subtropical Westerly Jet and Its Influence on Abnormal Character of Meiyu [M]. Nanjing: Nanjing University of Information Science and Technology, 2012.
[38] DING Y H, LIU J J, SUN Y, et al. A study of the synoptic-climatology of the Meiyu system in East Asia[J]. Chin J Atmos Sci, 2007, 31(6): 1082-1101(in Chinese), https://doi.org/10.3878/j.issn.1006-9895.2007.06.05. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=daqikx200706006
[39] LI Y, JIN R H, ZHOU N F, et al. An analysis on characteristics of heavy rainfall processes during the Meiyu season in Jianghuai region [J]. Acta Meteor Sinica, 2017, 75(5): 717-728 (in Chinese), https://doi.org/10.11676/qxxb2017.052. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=qxxb201705003
[40] TORRENCE C, COMPO G P. A practical guide to wavelet analysis [J]. Bull Amer Meteor Soc, 1998, 79: 61-78, https://doi.org/10.1175/1520-0477(1998)07960;0061:apgtwa62;2.0.co;2. doi: 10.1175/1520-0477(1998)079<0061:APGTWA>2.0.CO;2
[41] GE F, XIAO T G, JIN R H, et al. Propagation and accumulation of perturbation energy in the severe cold surge, ice snow and frozen disaster in South China during January 2008 [J]. Meteor Mon, 2008, 34(12): 11-20(in Chinese), https://doi.org/10.7519/j.issn.1000-0526.2008.12.002. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=qx200812002
[42] XIAO T G, SUN Z B, GE F. The characteristic of wave packet propagation in 2008 Sichuan"Sep. 22"heavy rainfall process [J]. Scientia Meteor Sinica, 2010, 30(2): 185-192 (in Chinese), https://doi.org/10.3969/j.issn.1009-0827.2010.02.007. http://en.cnki.com.cn/Article_en/CJFDTOTAL-QXKX201002008.htm
[43] MIAO J H, XIAO T G, LIU Z Y. Theoretic foundation and computational method about the wave-packet propagation diagnosis [J]. Acta Meteor Sinica, 2002, 60(4): 461-467 (in Chinese), https://doi.org/10.11676/qxxb2002.054. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=qxxb200204009
[44] PLUMB R A. On the three-dimensional propagation of stationary waves [J]. J Atmos Sci, 1985, 42(3): 217-229, https://doi.org/10.1175/1520-0469(1985)042<0217:OTTDPO>2.0.CO;2. doi: 10.1175/1520-0469(1985)042<0217:OTTDPO>2.0.CO;2
[45] TAKAYA K, NAKAMURA H. A formulation of a wave-activity flux for stationary Rossby waves on a zonally varying basic flow [J]. Geophys Res Lett, 1997, 24(23): 2985-2988, https://doi.org/10.1029/97gl03094. doi: 10.1029/97GL03094
[46] ELIASSEN A, PALM E. On the transfer of energy in stationary mountain waves [J]. Geofys Publ, 1961, 22(1): 1-23. https://www.researchgate.net/publication/234038625_On_the_tranfer_of_energy_in_stationary_mountain_waves
[47] HUANG R H. The conservation equation of wave action of planetary waves in spherical atmosphere and the stationary planetary wave propagation waveguide characterized by wave action flux [J].Sci China (B), 1984, 14(8): 766-775 (in Chinese), https://doi.org/10.1360/zb1984-14-8-766.
[48] LI C Y. Intraseasonal oscillations in the atmosphere [J]. Chin J Atmos Sci, 1990, 14(1): 32-45 (in Chinese), https://doi.org/10.3969/j.issn.1006-9585.2000.04.005. doi: 10.1175-1520-0469(1987)044-0950-OOLFOI-2.0.CO%3b2/
[49] LI C Y. Introduction to Climate Dynamics (Second Edition) [M]. Beijing: Science Press, 2000 (in Chinese).
[50] YANG L M, ZHANG Q Y. Relationships between perturbation kinetic energy anomaly along East Asian westerly jet and subtropical high in summer [J]. J Appl Meteor Sci, 2007, 18(4): 452-459 (in Chinese), https://doi.org/10.3969/j.issn.1001-7313.2007.04.005. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=yyqxxb200704005
[51] KRISHNAMURTI T N. Summer monsoon experiment-areview [J]. Mon Wea Rev, 1985, 113(9): 1590-1626. doi: 10.1175/1520-0493(1985)113<1590:SMER>2.0.CO;2
[52] HUANG R H, LI W J. Influence of heat source anomaly over the western tropical Pacific on the subtropical high over East Asia and its physical mechanism [J]. Chin J Atmos Sci, 1988, 12(s1): 107-116(in Chinese), https://doi.org/10.3878/j.issn.1006-9895.1988.t1.08. https://www.researchgate.net/publication/313062662_Influence_of_the_heat_source_anomaly_over_the_tropical_western_Pacific_on_the_subtropical_high_over_East_Asia
[53] ENOMOTO T, HOSKINS B J, MATSUDA Y. The formation mechanism of the Bonin high in August [J]. Quart J Roy Meteor Soc, 2003, 129(587): 157-178, https://doi.org/10.1256/qj.01.211.
[54] SONG Y, MIAO J H, JU J H. Relationships between features of wave packet propagation and movement of western Pacific subtropical high [J]. Acta Meteor Sinica, 2006, 64(5): 576-582 (in Chinese), https://doi.org/10.11676/qxxb2006.056. http://en.cnki.com.cn/article_en/cjfdtotal-qxxb200605003.htm
[55] HE J H, YU J J, SHEN X Y, et al. Research on mechanism and variability of east Asian monsoon [J]. J Trop Meteor, 2004, 20(5): 449-459 (in Chinese), https://doi.org/10.3969/j.issn.1004-4965.2004.05.001. http://en.cnki.com.cn/Article_en/CJFDTOTAL-RDQX200405000.htm
[56] ZHANG Q Y, TAO S Y. Influence of Asian mid-high latitude circulation on East Asian summer rainfall [J]. Acta Meteor Sinica, 1998, 56(2): 199-211 (in Chinese), https://doi.org/10.1007/s00376-999-0032-1. http://en.cnki.com.cn/article_en/cjfdtotal-qxxb802.006.htm
[57] ZHANG Q Y, TAO S Y. The study of the sudden northward jump of the subtropical high over the western Pacific [J]. Acta Meteor Sinica, 1999, 57(5): 539-548 (in Chinese), https://doi.org/10.1007/s00376-999-0032-1. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199900533752
[58] ZHANG Q Y, TAO S Y, ZHANG S L. The persistent heavy rainfall over the Yangtze River valley and its associations with the circulations over East Asian during summer [J]. Chin J Atmos Sci, 2003, 27(6): 1018-1030 (in Chinese), https://doi.org/10.3878/j.issn.1006-9895.2003.06.06. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=daqikx200306006
[59] HUANG R H, HUANGFU J L, LIU Y, et al. Development from the theory of energy dispersion of Rossby waves to studies on the dynamics of quasi-stationary planetary waves [J]. Chin J Atmos Sci, 2016, 40(1): 3-21 (in Chinese), https://doi.org/10.3878/j.issn.1006-9895.1503.14298. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=daqikx201601002
[60] YANG L M, ZHANG Q Y. Climate features of summer Asia subtropical westerly jet stream [J]. Climatic Environ Res, 2008, 13(1): 10-20 (in Chinese), https://doi.org/10.3878/j.issn.1006-9585.2008.01.02. http://en.cnki.com.cn/Article_en/CJFDTotal-QHYH200801001.htm