Abstract
The impacts of four teleconnection patterns on atmospheric circulation components over Eurasia and the Pacific region, from low to high latitudes in the Northern Hemisphere (NH), were investigated comprehensively in this study. The patterns, as identified by the Climate Prediction Center (USA), were the East Atlantic (EA), East Atlantic/Western Russia (EAWR), Polar/Eurasia (POLEUR), and Scandinavian (SCAND) teleconnections. Results indicate that the EA pattern is closely related to the intensity of the subtropical high over different sectors of the NH in all seasons, especially boreal winter. The wave train associated with this pattern serves as an atmospheric bridge that transfers Atlantic influence into the low-latitude region of the Pacific. In addition, the amplitudes of the EAWR, SCAND, and POLEUR patterns were found to have considerable control on the “Vangengeim–Girs” circulation that forms over the Atlantic–Eurasian region in winter or spring. The EA and EAWR mainly affect the westerlies in winter and spring and the POLEUR and SCAND, respectively, in summer and winter. Strong westerlies confine the extension of the North Polar vortex, which generally results in a small weak vortex and a shallow East Asian trough located in a position further east than normal. Furthermore, the North Polar vortex presents significant connections with the patterns during winter and summer. Analyses in this work suggest that the teleconnection patterns in summer could be driven, at least partly, by the Atlantic Multidecadal Oscillation, which to some degree might transmit the influence of the Atlantic Ocean to Eurasia and the Pacific region.
Similar content being viewed by others
References
Barnston AG, Livezey RE (1987) Classification, seasonal and persistence of low-frequency atmospheric circulation patterns. Mon Wea Rev 115:1083–1126
Bolotinskaja MS, Ryzhakov LJ (1964) Katalog makrosinoptiĉeskih protsessov po klassifikacij G.J. Vangengeima 1891–1962 [catalogue of macro-synoptic processes according to the G.J. Vangengeim’s classification 1891–1962; in Russian]. AANII Leningrad, p. 158
Coy L, Eckermann S, Hopple K (2009) A planetary wave breaking and tropospheric forcing as seen in the stratospheric sudden warming in 2006. J Atmos Sci 66:495–507
Cozannet GL, Lecacheux S, Delvallee E, Desramaut N, Oliveros C, Pedreros R (2011) Teleconnection pattern influence on sea-wave climate in the Bay of Biscay. J Clim 24:641–652
Duan LY, Huang YS, Liang PD (2008) Effect of West Pacific subtropical high on summer precipitation in North China. Meteorol Sci Technol 36(3):273–276
Enfield DB, Mestas-Nunez AM, Trimble PJ (2001) The Atlantic multidecadal oscillation and its relationship to rainfall and river flows in the continental U.S. Geophys Res Let 28:2077–2080
Esbensen SK (1984) A comparison of intermonthly and interannual teleconnections in the 700 mb geopotential height field during the northern hemisphere winter. Mon Wea Rev 112:2016–2032
Gao T, Han JW (2010) Evolutionary characteristics of the atmospheric circulations for frequent and infrequent dust storm springs in Northern China and the detection of potential future seasonal forecast signals. Meteorol Appl 17:76–86
Gao T, Han JW, Gao L, Yan W (2014) Impacts of North India Ocean SST on the extremely cold winters of 2011 and 2012 in the region of Da Hinggan Mountains and its western areas in China. Theor Appl Climatol 117:693–705
Garcia-Herrera R, Paredes D, Trigo RM, Trigo IF, Hernandez E, Barriopedro D, Mendes MA (2007) The outstanding 2004/05 drought in the Iberian Peninsula: Associated atmospheric circulation. J Hydrometorol 8:483–498. doi:10.1175/JHM578.1
Girs AA (1971) Mnogoletnije kolebanija atmosfernoj cirkuljacii idolgosročnyje gidrometeorologičeskije prognozy. [Many-year fluctuations of atmospheric circulation and long-term hydrometeorological forecasts; in Russian]. Gidrometeotzdat, Leningrad, p. 280 pp
Girs AA (1974) Makrocirkuljacionnyj metod dolgosročnyh meteorologičeskih prognozov [macro-circulation method of long-term meteorological forecasts; in Russian]. Gidrometeotzdat, Leningrad, 488 pp
Girs AA, Kondratovich LI (1978) Metody dolgosrocnyh prognozov pogody [methods of long-term weather forecast; in Russian]. Gidrometeotzdat, Leningrad, p. 343 pp
Hoy A, Sepp M, Matschullat J (2013) Large-scale atmospheric circulation forms and their impact on air temperature in Europe and Northern Asia. Theor Appl Climatol 113:643–658. doi:10.1007/s00704-012-0770-3
Hoy A, Schucknecht A, Sepp M, Matschullat J (2014) Large-scale synoptic types and their impact on European precipitation. Theor Appl Climatol 116:19–35. doi:10.1007/s00704-013-0897-x
Hu Q, Feng S (2012) AMO- and ENSO-driven summertime circulation and precipitation variations in North America. J Clim 25:6477–6495
Huang L, He JH,, Lu CY (2012) Review and outlook of researches about Western Pacific subtropical high (in Chinese with an English abstract). J Arid Meteorol 30(2):225–260
Huang XM, Guan ZY, Dai ZJ, Mei HX (2013) A further look at the interannual variations of east Asian trough intensity and their impacts on winter climate of China (in Chinese with an English abstract). Acta Meteorological Sinica 71(3):416–428
Kalnay E et al. (1996) The NCEP/NCAR 40-year reanalysis project. Bull Amer Meteor Soc 77:437–471
Kumar A, Hoerling MP (2003) The nature and causes for the delayed atmospheric response to el Niño. J Clim 16:1391–1403
Lau NC, Leetmaa A, Nath MJ, Wang HL (2005) Influences of ENSO-induced indo–Western Pacific SST anomalies on extratropical atmospheric variability during the boreal summer. J Clim 18:2922–2942
Lee MY, Hsu HH (2013) Identification of the Eurasian-North Pacific multidecadal oscillation and its relationship to the AMO. J Clim 26:8139–8153
Li J, Yu RC, Zhou TJ (2008) Teleconnection between NAO and climate downstream of the Tibetan plateau. J Clim 21:4680–4690
LinHo LH, Huang XL, Lau NC (2008) Winter-to-spring transition in East Asia: a planetary-scale perspective of the South China spring rain onset. J Clim 21:3081–3096
Liu YY, Chen W (2012) Variability of the Eurasian teleconnection pattern in the northern hemisphere winter and its influences on the climate in China (in Chinese with an English abstract). Chin J of Atmospheric Science 36(2):423–432
Liu YY, Wang L, Zhou W (2014) Three Eurasian teleconnection patterns: spatial structures, temporal variability, and associated winter climate anomalies. Clim Dyn 42:2817–2839
Luo L, He JH, Tan YK (2005) The composite features and possible mechanisms during the westward extension of subtropical high in the Western Pacific (in Chinese with an English abstract). Sci Meteorol Sinica 25(5):465–473
Oort AH, Yienger JJ (1996) Observed interannual variability in the Hadley circulation and its connections to ENSO. J Clim 9:2751–2767
Panagiotopoulos F, Shahgedanova M, Stephenson DB (2002) A review of northern hemisphere winter-time teleconnection patterns. J de Physique 12(10):27–47. doi:10.1051/jp4:20020450
Qian WH, Liang HY (2012) Atmospheric teleconnections and regional-scale atmospheric anomalies over the northern hemisphere (in Chinese with an English abstract). Chinese J Geophys 55(5):1449–1461
Ren XJ, Yang XQ, Sun XG (2013) Zonal oscillation of Western Pacific subtropical high and subseasonal SST variations during Yangtze persistent heavy rainfall events. J Clim 26:8929–8946
Rogers JC (1981) The North Pacific oscillation. Int J Climatol 1(1):39–57
Sidorenkov NS, Orlov IA (2008) Atmospheric circulation epochs and climate changes. Russ Meteorol Hydrol 33(9):553–559
Smoliak BV (2009) A Eurasian pattern of northern hemisphere wintertime sea level pressure variability. University of Washington Graduate School, Degree of Master of Science
Sung MK, Lim GH, Kwon WT, Boo KO, Kug JS (2009) Short-term variation of Eurasian pattern and its relation to winter weather over East Asia. Int J Climatol 29:771–775
Takaya K, Nakamura H (2013) Interannual variability of east Asian winter monsoon and related modulations of the planetary waves. J Clim 26:9445–9461
Thompson DWJ, Wallace JM (1998) The Arctic oscillation signature in the winter geopotential height and temperature fields. Geophys Res Lett 25(9):1297–1300
Van Loon H, Rogers JC (1978) The seesaw in winter temperature s between Greenland and Northern Europe. Part I: general description. Mon Wea Rev 106:296–310
Vangengeim GJ (1935) Opyt primenenija sinopticeskih metodov kizuceniju i harakteristike klimata [experimental usage of synoptical methods for studying and characterizing of climate; in Russian]. Gidrometeotzdat, Moskva, p. 109 pp
Vangengeim GJ (1940) Dolgostocnyi prognoz temperatury vozduha Ivskrytija rek [long term forecast of air temperature and river openings; in Russian]. Trudy GGI 10
von Storch H, Zwiers FW (1999) Statistical analysis in climate research. Cambridge University Press, Cambridge, pp. pp 93–pp 44
Walker GT, Bliss EW (1932) World weather V. Mem. Roy Meteor Soc 4:53–84
Wallace JM, Gutzler DS (1981) Teleconnections in the geopotential height field during the northern hemisphere winter. Mon Wea Rev 109:784–812
Wang ZY, Ding YH (2009) Impacts of the long-term change of the summer Asian polar vortex on the circulation system and the water vapor transport in East Asia (in Chinese with an English abstract). Chinese J Geophys 52(1):20–29
Wang HJ, He SP (2015) The North China/Northeastern Asia severe summer drought in 2014. J Clim 28:6667–6681
Wang WL, Wang JY, Xie YQ, Wang WG, Wang ZW, Wang K, Du LM, Deng NS, Cai SM, Li YL (2012) Analysis of decadal variation of East Asia trough and West Pacific subtropical high in summer (in Chinese with an English abstract). Adv Earth Sci 27(3):304–320
Watanabe M, Nitte T (1999) Decadal changes in the atmospheric circulation and associated surface climate variations in the northern hemisphere winter. J Clim 12:494–510
Wen M, Yang S, Kumar A, Zhang PQ (2009) An analysis of the large-scale climate anomalies associated with the snowstorms affecting China in January 2008. Mon Wea Rev 137:1111–1131
Woo SH, Kim BM, Kug JS (2015) Temperature variation over East Asia during the lifecycle of weak stratospheric polar vortex. J Clim 28:5857–5872
Yang GY, Zhang Y (1994) The relationship between anomalous trough over East Asia and el Niño (in Chinese with an English abstract). Q J Applied Meteorol 5(1):114–118
Yang SY, Wu BY, Zhang RH, Zhou SW (2014) Propagation of low-frequency oscillation over Eurasian mid-high latitude in winter and its association with Eurasian teleconnection pattern (in Chinese with an English abstract). Chin J Atmos Sci 38(1):121–132
Yin ZY, Wang HL, Liu XD (2014) A comparative study on precipitation climatology and interannual variability in the lower midlatitude East Asia and Central Asia. J Clim 27:7830–7848
Yu JY, Kao PK, Paek H, Hsu HH, Hung CW, Lu MM, An SI (2015) Linking emergence of the Central-Pacific el Niño to the Atlantic multi-decadal oscillation. J Clim 28:651–662
Zhang R, Delworth TL (2007) Impact of the Atlantic multidecadal oscillation on North Pacific climate variability. Geophys Res Let 34(1–6):L23708. doi:10.1029/2007GL031601
Zhang HD, Lu WS, Gao ST, Zhang YS (2006) Influence of the north polar vortex activity on the contemporaneous and subsequent air temperature in China (in Chinese with an English abstract). J Nanjing Inst Meteorol 29(4):507–526
Zhang HD, Jin RH, Zhang YZ (2008) Relationships between summer northern polar vortex with subtropical high and their influence on precipitation in North China (in Chinese with an English abstract). J Tropical Meteorol 24(4):417–422
Zhang JW, Li DL, Liu YJ (2014) New features of polar vortex and its impacts on winter temperature of China (in Chinese with an English abstract). Plateau Meteorol 33(3):721–732
Zhao ZG (1999) Atmospheric circulation conditions of China flood and drought during summer (in Chinese). China Meteorological Press, Beijing, pp. 79–94
Zhao P, Yang S, Yu RC (2010) Long-term changes in rainfall over Eastern China and large-scale atmospheric circulation associated with recent global warming. J Clim 23:1544–1562
Zhao JH, Feng GL, Yang J, Zhi R, Wang QG (2012) Analysis of the distribution of the large-scale drought/flood of summer in China under different types of the Western Pacific subtropical high (in Chinese with an English abstract). Acta Meteorol Sinica 70(5):1011–1031
Acknowledgments
The first author would like to thank the China Scholarship Council (CSC) and the University of California, Irvine, USA, for the financial support and provision of a pleasant working environment during her period as a senior visiting scholar. Cordial thanks are extended to the anonymous reviewers and editors for their constructive comments and suggestions for the improvement of this paper. Many thanks are offered to Professor Jinyi Yu for his suggestions concerning the presented topic. The authors appreciate the help given by Dr. Fangting Yu regarding the improvement of the written English. This study was supported by the US National Science Foundation (AGS-1233542 and AGS-1505145), National Natural Science Foundation of China (No. 40965007), Natural Science Foundation of Inner Mongolia, China (No. 2013MS0923), and Financial Support for Scientific Research of Inner Mongolia Meteorological Bureau, China Meteorological Administration (No. nmqxkjcx201607).
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Gao, T., Yu, Jy. & Paek, H. Impacts of four northern-hemisphere teleconnection patterns on atmospheric circulations over Eurasia and the Pacific. Theor Appl Climatol 129, 815–831 (2017). https://doi.org/10.1007/s00704-016-1801-2
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s00704-016-1801-2