Climate Dynamics

, Volume 50, Issue 9–10, pp 3485–3503 | Cite as

Enhancement of the relationship between the winter Arctic oscillation and the following summer circulation anomalies over central East Asia since the early 1990s

  • Shaobo Qiao
  • Po Hu
  • Taichen Feng
  • Jianbo Cheng
  • Zixuan Han
  • Zhiqiang Gong
  • Rong Zhi
  • Guolin Feng


Considering the possible lag of the impact of the winter Arctic oscillation (AO) on the subsequent summer climate anomalies over East Asia and that the relationship between them may differ during different periods, the non-stationary relationship between these systems and the corresponding mechanism of connection are investigated in this study. A regime shift of the winter AO index was detected around 1988, with mean AO indices of −0.69 and 0.10 for 1958–1987 and 1988–2014, respectively, and their differences passed the 99% confidence level. After the regime shift and especially since the early 1990s, negative (positive) winter AO indices corresponds with positive (negative) height anomalies over central East Asia (CEA) during the following summer. Meanwhile, the westerly jet stream tends to be northward (southward) and the East Asian summer monsoon (EASM) is strong (weak), which contributes to the warm (cold) anomalies over central China and the significantly enhanced (reduced) rainfall over northeast China. After the early 1990s, the enhanced connection of the winter AO and the following summer height anomalies over CEA is largely due to the enhanced connection of the winter AO and the following Indian summer monsoon (ISM) rainfall during the same period. The negative (positive) winter AO favors increasing (decreasing) rainfall over the ISM region, which triggers a positive (negative) circumglobal teleconnection (CGT), and results in significantly positive (negative) height anomalies over CEA. One way the winter AO could influence the following ISM rainfall is that the negative (positive) winter AO memories will be maintained by the positive (negative) sea surface temperature (SST) anomalies over the tropical Atlantic of the following summer, which are responsible for the La Niña (El Niño) developing phase and increases (decreases) the ISM rainfall.


Arctic oscillation Regime shift Central East Asia Indian summer monsoon Tropical Atlantic Circumglobal teleconnection 



This study acknowledges the support of the National Basic Research Program of China (973 Program) (2013CB430204), National Natural Science Foundation of China (41530531, 41575082, 41575074, 41475064, 41675107).


  1. Adler RF, Huffman GJ, Chang A, Ferraro R, Xie PP, Janowiak J, Rudolf B, Schneider U, Curtis S, Bolvin D, Gruber A, Susskind J, Arkin P, Nelkin E (2003) The version-2 global precipitation climatology project (GPCP) monthly precipitation analysis (1979–present). J Hydrol 4:1147–1167Google Scholar
  2. Ambrizzi T, Hoskins BJ, Hsu HH (1995) Rossby wave propagation and teleconnection patterns in the austral winter. J Atmos Sci 52:3661–3672CrossRefGoogle Scholar
  3. Bretherton CS, Smith C, Wallace JM (1992) An intercomparison of methods for finding coupled patterns in climate data. J Clim 5:541–560CrossRefGoogle Scholar
  4. Cayan DR (1992) Latent and sensible heat flux anomalies over the northern oceans: The connection to monthly atmospheric circulation. J Clim 5:354–369CrossRefGoogle Scholar
  5. Chang TC, Hsu HH, Hong CC (2016) Enhanced Influences of Tropical Atlantic SST on WNP–NIO Atmosphere–Ocean Coupling since the Early 1980s. J Clim 29:6509–6525CrossRefGoogle Scholar
  6. Chen W (2002) Impacts of El Niño and La Niña on the cycle of the East Asian winter and summer monsoon (in Chinese). Chin. J Atmos Sci 26:595–610Google Scholar
  7. Chen W, Li T (2007) Modulation of northern hemisphere wintertime stationary planetary wave activity: East Asian climate relationships by the Quasi-Biennial oscillation. J Geophys Res 112:D20. doi: 10.1029/2007JD008611 Google Scholar
  8. Chen W, Graf HF, Huang RH (2000) The interannual variability of East Asian winter monsoon and its relation to the summer monsoon. Adv Atmos Sci 17:46–60Google Scholar
  9. Chen M, Xie P, Janowiak JE, Arkin PA (2002) Global land precipitation: a 50-yr monthly analysis based on gauge observations. J Hydrol 3:249–266Google Scholar
  10. Chen W, Yang S, Huang R (2005) Relationship between stationary planetary wave activity and the East Asian winter monsoon. J Geophys Res 110:D14. doi: 10.1029/2004JD005669 Google Scholar
  11. Chen W, Feng J, Wu R (2013) Roles of ENSO and PDO in the link of the East Asian winter monsoon to the following summer monsoon. J Clim 26:622–635CrossRefGoogle Scholar
  12. Chen S, Wu R, Chen W (2015a) The changing relationship between interannual variations of the North Atlantic oscillation and Northern Tropical Atlantic SST. J Clim 28:485–504CrossRefGoogle Scholar
  13. Chen W, Lee JY, Lu R, Dong B, Ha KJ (2015b) Intensified impact of tropical Atlantic SST on the western North Pacific summer climate under a weakened Atlantic thermohaline circulation. Clim Dyn 45:2033–2046CrossRefGoogle Scholar
  14. Choi KS, Wu CC, Byun HR (2012) Possible connection between summer tropical cyclone frequency and spring Arctic oscillation over East Asia. Clim Dyn 38:2613–2629CrossRefGoogle Scholar
  15. Cui Y, Duan A, Liu Y, Wu G (2015) Interannual variability of the spring atmospheric heat source over the Tibetan Plateau forced by the North Atlantic SSTA. Clim Dyn 45:1617–1634CrossRefGoogle Scholar
  16. Ding Q, Wang B (2005) Circumglobal teleconnection in the Northern Hemisphere summer. J Clim 18:3483–3505CrossRefGoogle Scholar
  17. Ding Q, Wang B, Wallace JM, Branstator G (2011) Tropical-extratropical teleconnections in boreal summer: Observed interannual variability. J Clim 24:1878–1896CrossRefGoogle Scholar
  18. Frankignoul C (1985) Sea surface temperature anomalies, planetary waves, and air–sea feedback in the middle latitudes. Rev Geophys 23:357–390CrossRefGoogle Scholar
  19. Frankignoul C, Czaja A, Heveder BL (1998) Air–sea feedback in the North Atlantic and surface boundary conditions for ocean models. J Clim 11:2310–2324CrossRefGoogle Scholar
  20. Gong D, Ho C (2003) Arctic oscillation signals in the East Asian summer monsoon. J Geophys Res 108:D2. doi: 10.1029/2002JD002193 Google Scholar
  21. Gong D, Wang S, Zhu J (2001) East Asian winter monsoon and Arctic oscillation. Geophys Res Lett 28:2073–2076. doi: 10.1029/2000GL012311 CrossRefGoogle Scholar
  22. Gong D, Yang J, Kim SJ (2011) Spring Arctic oscillation-East Asian summer monsoon connection through circulation changes over the western North Pacific. Clim Dyn 37:2199–2216CrossRefGoogle Scholar
  23. Gong Z, Feng G, Ren F, Li J (2014) A regional extreme low temperature event and its main atmospheric contributing factors. Theor Appl Climatol 117:195–206CrossRefGoogle Scholar
  24. Gong D, Guo D, Gao Y, Yang J, Mao R, Qu J, Gao M, Li S, Kim SJ (2016) Boreal winter Arctic oscillation as an indicator of summer SST anomalies over the western tropical Indian Ocean. Clim Dyn. doi: 10.1007/s00382-016-3216-2 Google Scholar
  25. Gu W, Li C, Li W, Zhou W, Chan JCL (2009) Interdecadal unstationary relationship between NAO and east China’s summer precipitation patterns. Geophys Res Lett 36:L13702. doi: 10.1029/2009GL038843 CrossRefGoogle Scholar
  26. Hartmann DL, Lo F (1998) Wave-driven zonal flow vacillation in the Southern Hemisphere. J Atmos Sci 55:1303–1315CrossRefGoogle Scholar
  27. He W, Feng G, Gao X, Li J (2006) Amplitude death in non-feedback coupled chaotic system (in Chinese). Acta Physica Sinica 55:6192–6196Google Scholar
  28. Hong CC, Chang TC, Hsu HH (2014) Enhanced relationship between the tropical Atlantic SST and the summertime western North Pacific subtropical high after the early 1980s. J Geophys Res 119:3715–3722. doi: 10.1002/2013JD021394 CrossRefGoogle Scholar
  29. Huang B, Shukla J (2005) Ocean-atmosphere interactions in the tropical and subtropical Atlantic Ocean. J Clim 18:1652–1672CrossRefGoogle Scholar
  30. Huang J, Higuchi K, Shabbar A (1998) The relationship between the North Atlantic oscillation and El Niño-Southern oscillation. Geophys Res Lett 25:2707–2710. doi: 10.1029/98GL01936 CrossRefGoogle Scholar
  31. Hurrell JW (1995) Decadal trends in the North Atlantic oscillation: regional temperatures and precipitation. Science 269:676–679CrossRefGoogle Scholar
  32. Hurrell JW, van Loon H (1997) Decadal variations in climate associated with the North Atlantic oscillation. Clim Change 36:301–326CrossRefGoogle Scholar
  33. Jeong JH, Ho CH (2005) Changes in occurrence of cold surges over East Asia in association with Arctic oscillation. Geophys Res Lett 32:L14704. doi: 10.1029/2005GL023024 CrossRefGoogle Scholar
  34. Kalnay E, Kanamitsu M, Kistler R, Collins W, Deaven D, Gandin L, Iredell M, Saha S, White G, Woolen J, Zhu Y, Chelliah M, Ebisuzaki W, Higgins W, Janowiak J, Mo KC, Ropelewski C, Wang J, Leetmaa A, Reynolds R, Jenne R, Joseph D (1996) The NCEP/NCAR 40-year reanalysis project. Bull Am Meteo Soc 77:437–471CrossRefGoogle Scholar
  35. Krishna Kumar K, Rajagopalan B, Cane MA (1999) On the weakening relationship between the Indian monsoon and ENSO. Science 284:2156–2159CrossRefGoogle Scholar
  36. Kucharski F, Bracco A, Yoo JH, Molteni F (2007) Low-frequency variability of the Indian monsoon–ENSO relationship and the tropical Atlantic: the ‘weakening’ of the 1980s and 1990s. J Clim 20:4255–4266CrossRefGoogle Scholar
  37. Kucharski F, Bracco A, Yoo JH, Molteni F (2008) Atlantic forced component of the Indian monsoon interannual variability. Geophys Res Lett 33:L04706. doi: 10.1029/2007GL033037 Google Scholar
  38. Kucharski F, Bracco A, Yoo JH, Tompkins AM, Feudale L, Ruti P, Dell’ Aquila A (2009) A Gill-Matsuno-type mechanism explains the tropical Atlantic influence on African and Indian monsoon rainfall. Q J Roy Meteor Soc 135:569–579CrossRefGoogle Scholar
  39. Kushnir Y, Robinson WA, Bladé I, Hall NMJ, Peng S, Sutton R (2002) Atmospheric GCM response to extratropical SST anomalies: synthesis and evaluation. J Clim 15:2233–2256CrossRefGoogle Scholar
  40. Li J, Wang JXL (2003) A new North Atlantic oscillation index and its variability. Adv Atmos Sci 20:661–676. doi: 10.1007/BF02690792 CrossRefGoogle Scholar
  41. Li J, Sun C, Jin F (2013) NAO implicated as a predictor of Northern Hemisphere mean temperature multidecadal variability. Geophys Res Lett 40:5497–5502. doi: 10.1002/2013GL057877 CrossRefGoogle Scholar
  42. Limpasuvan V, Hartmann DL (1999) Eddies and the annular modes of climate variability. Geophys Res Lett 26:3133–3136CrossRefGoogle Scholar
  43. Limpasuvan V, Hartmann DL (2000) Wave-maintained annular modes of climate variability. J Clim 13:4414–4429CrossRefGoogle Scholar
  44. Lo TT, Hsu HH (2008) The early 1950s regime shift in temperature in Taiwan and East Asia. Clim Dyn 31:449–461CrossRefGoogle Scholar
  45. Lu R, Dong B, Ding H (2006) Impact of the Atlantic multidecadal oscillation on the Asian summer monsoon. Geophys Res Lett 33:24. doi: 10.1029/2006GL027655 Google Scholar
  46. Ogi M, Tachibana Y, Yamazaki K (2003) Impact of the wintertime North Atlantic oscillation (NAO) on the summertime atmospheric circulation. Geophys Res Lett 30:704. doi: 10.1029/2003GL017280 Google Scholar
  47. Ogi M, Tachibana Y, Yamazaki K (2004) The connectivity of thewinter North Atlantic oscillation (NAO) and the summer Okhotsk High. J Meteorol Soc Jpn 82:905–913CrossRefGoogle Scholar
  48. Pak G, Park YH, Vivier F, Kwon YO, Chang K (2014) Regime-dependent non-stationary relationship between the East Asian winter monsoon and North Pacific oscillation. J Clim 27:8185–8204CrossRefGoogle Scholar
  49. Park TW, Ho CH, Yang S (2011) Relationship between the Arctic oscillation and cold surges over East Asia. J Clim 24:68–83CrossRefGoogle Scholar
  50. Qian B, Saunders MA (2003) Summer UK temperature and its links to preceding Eurasian snow cover, North Atlantic SSTs, and the NAO. J Clim 16:4108–4120CrossRefGoogle Scholar
  51. Qiao S, Feng G (2016) Impact of the December North Atlantic oscillation on the following February East Asian trough. J Geophys Res 121:10074–10088. doi: 10.1002/2016JD025007 CrossRefGoogle Scholar
  52. Qiao S, Gong Z, Feng G, Qian Z (2015) Relationship between cold winters over Northern Asia and the subsequent hot summers over mid-lower reaches of the Yangtze River valley under global warming. Atmos Sci Lett 16:479–485. doi: 10.1002/asl.585 CrossRefGoogle Scholar
  53. Rodionov S, Overland JE (2004) Application of a sequential regime shift detection method to the Bering Sea ecosystem. ICES J Mar Sci Journal du Conseil 62:328–332CrossRefGoogle Scholar
  54. Smith TM, Reynolds RW (2003) Extended reconstruction of global sea surface temperatures based on COADS data (1854–1997). J Clim 16:1495–1510CrossRefGoogle Scholar
  55. Sun B, Sun S (1994) The analysis on the features of the atmospheric circulation in preceding winters for the summer drought and flooding in the Yangtze and Huaihe River valley. Adv Atmos Sci 11:79–90CrossRefGoogle Scholar
  56. Sung MK, Kwon WT, Baek HJ, Boo KO, Lim GH, Kug JS (2006) A possible impact of the North Atlantic oscillation on the east Asian summer monsoon precipitation. Geophys Res Lett 33:L21713. doi: 10.1029/2006GL027353 CrossRefGoogle Scholar
  57. Thompson DWJ, Wallace JM (1998) The Arctic oscillation signature in the wintertime geopotential height and temperature fields. Geophys Res Lett 25:1297–1300CrossRefGoogle Scholar
  58. Thompson DWJ, Wallace JM (2000) Annular modes in the extratropical circulation. Part I: month-to-month variability. J Clim 13:1000–1016CrossRefGoogle Scholar
  59. Wang L, Chen W (2010) Downward Arctic oscillation signal associated with moderate weak stratospheric polar vortex and the cold December 2009. Geophys Res Lett 37:L09707. doi: 10.1029/2010GL042659 Google Scholar
  60. Wang L, Wu R (2012) In-phase transition from the winter monsoon to the summer monsoon over East Asia: Role of the Indian Ocean. J Geophys Res 117:D11112. doi: 10.1029/2012JD017509 Google Scholar
  61. Wang B, Wu R, Fu X (2000) Pacific-East Asian teleconnection: How does ENSO affect East Asian climate? J Clim 13:1517–1536CrossRefGoogle Scholar
  62. Wang B, Wu R, Lau KM (2001) Interannual variability of the Asian summer monsoon: Contrasts between the Indian and the western North Pacific-east Asian monsoons. J Clim 14:4073–4090CrossRefGoogle Scholar
  63. Wang B, Wu R, Li T (2003) Atmosphere-warm ocean interaction and its impacts on Asian–Australian monsoon variation. J Clim 16:1195–1211CrossRefGoogle Scholar
  64. Wang L, Chen W, Huang RH (2007) Changes in the variability of North Pacific oscillation around 1975/76 and its relationship with East Asian winter climate. J Geophys Res 112:D11110. doi: 10.1029/2006JD008054 CrossRefGoogle Scholar
  65. Wang L, Huang R, Gu L, Chen W, Kang L (2009a) Interdecadal variations of the East Asian winter monsoon and their association with quasi-stationary planetary wave activity. J Clim 22:4860–4872CrossRefGoogle Scholar
  66. Wang Y, Li S, Luo D (2009b) Seasonal response of Asian monsoonal climate to the Atlantic Multidecadal oscillation. J Geophys Res 114:D02112. doi: 10.1029/2008JD010929 Google Scholar
  67. Wang H, Wang B, Huang F, Ding QH, Lee JY (2012) Interdecadal change of the boreal summer circumglobal teleconnection (1958–2010). Geophys Res Lett 39:L12704. doi: 10.1029/2012GL052371 Google Scholar
  68. Watanabe M (2004) Asian jet waveguide and a downstream extension of the North Atlantic oscillation. J Clim 17:4674–4691CrossRefGoogle Scholar
  69. Webster PJ, Moore AM, Loschnigg JP, Leben RR (1999) Coupled ocean-atmosphere dynamics in the Indian Ocean during 1997–98. Nature 401:356–360CrossRefGoogle Scholar
  70. Wu R (2002) A mid-latitude Asian circulation anomaly pattern in boreal summer and its connection with the Indian and east Asian summer monsoons. Int J Climatol 22:1879–1895CrossRefGoogle Scholar
  71. Wu R, Kirtman BP, Pegion K (2006) Local air–sea relationship in observations and model simulations. J Clim 19:4914–4932CrossRefGoogle Scholar
  72. Wu Z, Wang B, Li J, Jin F (2009) An empirical seasonal prediction model of the East Asian summer monsoon using ENSO and NAO. J Geophys Res 114:D18120. doi: 10.1029/2009JD011733 CrossRefGoogle Scholar
  73. Xu T, Shi Z, Wang H, An Z (2016) Nonstationary impact of the winter North Atlantic oscillation and the response of mid-latitude Eurasian climate. Theor Appl Climatol 124:1–14CrossRefGoogle Scholar
  74. Zhang R (2015) Changes in East Asian summer monsoon and summer rainfall over eastern China during recent decade. Sci Bull 60:1222–1224CrossRefGoogle Scholar
  75. Zheng F, Li J, Li Y, Zhao S, Deng D (2016) Influence of the summer NAO on the spring-NAO-based predictability of the east Asian summer monsoon. J Appl Meteorol Clim 55:1459–1476. doi: 10.1175/JAMC-D-15-0199.1 CrossRefGoogle Scholar
  76. Zuo J, Li W, Sun C, Xu L, Ren H (2013) Impact of the North Atlantic sea surface temperature tripole on the East Asian summer monsoon. Adv Atmos Sci 30:1173–1186CrossRefGoogle Scholar
  77. Zuo J, Ren H, Li W (2015) Contrasting impacts of the Arctic oscillation on surface air temperature anomalies in southern China between early and middle-to-late winter. J Clim 28:4015–4026CrossRefGoogle Scholar
  78. Zuo J, Ren H, Li W, Wang L (2016) Interdecadal variations in the relationship between the Winter North Atlantic oscillation and temperature in South-Central China. J Clim 29:7477–7493CrossRefGoogle Scholar

Copyright information

© Springer-Verlag GmbH Germany 2017

Authors and Affiliations

  • Shaobo Qiao
    • 1
  • Po Hu
    • 1
  • Taichen Feng
    • 1
  • Jianbo Cheng
    • 1
  • Zixuan Han
    • 1
  • Zhiqiang Gong
    • 2
  • Rong Zhi
    • 2
  • Guolin Feng
    • 2
    • 3
  1. 1.College of Atmospheric SciencesLanzhou UniversityLanzhouChina
  2. 2.National Climate CenterChina Meteorological AdministrationBeijingChina
  3. 3.College of Physical Science and TechnologyYangzhou UniversityYangzhouChina

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