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An interdecadal change in the influence of the Central Pacific ENSO on the subsequent north tropical Atlantic spring SST variability around the mid-1980s

  • Xiaoxue Yin
  • Lian-Tong ZhouEmail author
Article

Abstract

North tropical Atlantic (NTA) spring sea surface temperature (SST) tends to be warmer (cooler) than normal in Central Pacific (CP) El Niño decaying years during 1960s to mid-1980s. However, the relationship between the NTA spring SST and CP El Niño-Southern Oscillation (ENSO) is weakened after mid-1980s. This study presents this interdecadal change and investigates possible causes. Before the mid-1980s, above-normal NTA SST peaks in post-El Niño spring. The CP El Niño can affect NTA spring SST by inducing a negative phase of North Atlantic Oscillation (NAO) anomaly over North Atlantic from winter to spring. This negative NAO circulation weakens the Azores High and causes weaker than normal trade wind. As a result, less heat loses from the NTA Ocean and above-normal SST anomalies generated. In contrast, after the middle 1980s, the connection between CP ENSO and NAO-like anomaly has been disrupted. This leads to a weakening of CP ENSO influences on the NTA spring SST. The observed change in the relationship between NTA spring SST and CP ENSO is likely related to the state of the polar vortex. Before the middle 1980s, the polar vortex is weak, this favors the propagation of ENSO-related wave flux. The Rossby wave trains spread to the stratosphere during El Niño conditions and cause weaker than normal polar vortex, resulting in a negative NAO in the low levels. And the subtropical jet is enhanced and elongated which provides a potential waveguide for wave activity propagating to the Atlantic through a tropospheric way. However, the polar vortex is strong after mid-1980s, preventing the propagation of the ENSO-related wave trains through the stratosphere or the troposphere.

Keywords

North tropical Atlantic SST CP ENSO Interdecadal change NAO Polar vortex 

Notes

Acknowledgements

This paper was supported by the National Key Research and Development Program of China (Grant no. 2016YFA0600603), the National Natural Science Foundation of China (Grant no. 41475053).

References

  1. Alexander MA, Blade I, Nerman M, Lanzante JR, Lau NC, Scott JD (2002) The atmospheric bridge: the influence of ENSO teleconnections on air–sea interaction over the global oceans. J Clim 15:2205–2231CrossRefGoogle Scholar
  2. Ashok K, Behera SK, Rao SA, Weng H, Yamagata T (2007) El Niño Modoki and its possible teleconnection. J Geophys Res 112:C11007.  https://doi.org/10.1029/2006JC003798 CrossRefGoogle Scholar
  3. Ayarzagüena B, López-Parages J, Iza M, Calvo N, Rodríguez-Fonseca B (2018) Stratospheric role in interdecadal changes of El Niño impacts over Europe. Clim Dyn.  https://doi.org/10.1007/s00382-018-4186-3 Google Scholar
  4. Branstator G (2002) Circumglobal teleconnections, the jet stream waveguide, and the North Atlantic oscillation. J Clim 15:1893–1910CrossRefGoogle Scholar
  5. Bretherton CS, Widmann M, Dymnikov VP, Wallace JM, Blad I (1999) The effective number of spatial degrees of freedom of a time-varying field. J Clim 12:1990–2009CrossRefGoogle Scholar
  6. Brönnimann S, Luterbacher J, Staehelin J, Svendby TM, Hansen G, Svenøe T (2004) Extreme climate of the global troposphere and stratosphere 1940–1942 related to El Niño. Nature 431:971–974CrossRefGoogle Scholar
  7. Brönnimann S, Xoplaki E, Casty C, Pauling A, Luterbacher J (2007) ENSO influence on Europe during the last centuries. Clim Dyn 28:181–197.  https://doi.org/10.1007/s00382-006-0175-z CrossRefGoogle Scholar
  8. Butler AH, Polvani LM, Deser C (2014) Separating the stratospheric and tropospheric pathways of El Niño Southern Oscillation teleconnections. Environ Res Lett 9(2):024014.  https://doi.org/10.1088/1748-9326/9/2/024014 CrossRefGoogle Scholar
  9. Calvo N, Iza M, Hurwitz M, Manzini E, Peña-Ortiz C, Butler A, Cagnazzo C, Ineson S, Garfinkel C (2017) Northern Hemisphere stratospheric pathway of different El Niño flavors in stratosphere-resolving CMIP5 models. J Clim 30:4351–4371CrossRefGoogle Scholar
  10. Cao X, Chen SF, Chen GH, Wu RG (2016) Intensified impact of northern tropical Atlantic SST on tropical cyclogenesis frequency over the western North Pacific after the late 1980s. Adv Atmos Sci 33:919–930.  https://doi.org/10.1007/s00376-016-5206-z CrossRefGoogle Scholar
  11. Capotondi A et al (2015) Understanding ENSO diversity. Bull Am Meteor Soc 96:921–938.  https://doi.org/10.1175/BAMS-D-13-00117.1 CrossRefGoogle Scholar
  12. Carton JA, Cao XH, Giese BS, daSilva AM (1996) Decadal and interannual SST variability in the tropical Atlantic Ocean. J Phys Oceanogr 26:1165–1175CrossRefGoogle Scholar
  13. Cassou C, Terray L (2001) Dual influence of Atlantic and Pacific SST anomalies on the North Atlantic/Europe winter climate. Geophys Res Lett 28:3195–3198.  https://doi.org/10.1029/2000GL012510 CrossRefGoogle Scholar
  14. Cassou C, Deser C, Terray L, Hurrell JW, Drevillon M (2004) Summer sea surface temperature conditions in the North Atlantic and their impact upon the atmospheric circulation in early winter. J Clim 17: 3349–3363.  https://doi.org/10.1175/1520-0442(2004)017,3349:SSSTCI.2.0.CO;2 CrossRefGoogle Scholar
  15. Chang P, Saravanan R, Ji L (2003) Tropical Atlantic seasonal predictability: the roles of El Niño remote influence and thermodynamic air-sea feedback. Geophys Res Lett 30:1501.  https://doi.org/10.10029/2002GL016119 Google Scholar
  16. Chang P, Fang Y, Saravanan R, Ji L, Seidel H (2006) The cause of the fragile relationship between the Pacific El Niño and the Atlantic Niño. Nature 443:324–328.  https://doi.org/10.1038/nature05053 CrossRefGoogle Scholar
  17. Charney JG, Drazin PG (1961) Propagation of planetary-scale disturbances from the lower into the upper atmosphere. J Geophys Res 66:83–109CrossRefGoogle Scholar
  18. Chen W, Wei K (2009) Anomalous propagation of the quasi-stationary planetary waves in the atmosphere and its roles in the impact of the stratosphere on the East Asian winter climate. Adv Earth Sci 24(3):272–285.  https://doi.org/10.3321/j.issn:1001-8166.2009.03.006 (in Chinese) Google Scholar
  19. Chen SF, Wu RG (2017) Interdecadal changes in the relationship between interannual variations of spring North Atlantic SST and Eurasian surface air temperature. J Clim 30:3771–3787.  https://doi.org/10.1175/JCLI-D-16-0477.1 CrossRefGoogle Scholar
  20. Chen SF, Wu RG, Chen W (2015) The changing relationship between interannual variations of the North Atlantic Oscillation and Northern Tropical Atlantic SST. J Clim 28:485–504.  https://doi.org/10.1175/JCLI-D-14-00422.1 CrossRefGoogle Scholar
  21. Chiang JCH, Sobel AH (2002) Tropical tropospheric temperature variations caused by ENSO and their influence on the remote tropical climate. J Clim 15:2616–2631.  https://doi.org/10.1175/1520-0442(2002)015,2616:TTTVCB.2.0.CO;2 CrossRefGoogle Scholar
  22. Czaja A, Van der Vaart P, Marshall J (2002) A diagnostic study of the role of remote forcing in tropical Atlantic variability. J Clim 15:3280–3290CrossRefGoogle Scholar
  23. Dommenget D, Latif M (2000) Interannual to decadal variability in the tropical Atlantic. J Clim 13:777–792CrossRefGoogle Scholar
  24. Enfield DB, Mayer DA (1997) Tropical Atlantic sea surface temperature variability and its relation to El Niño-Southern Oscillation. J Geophys Res 102(C1):929–945.  https://doi.org/10.1029/96JC03296 CrossRefGoogle Scholar
  25. Feng J, Chen W, Li YJ (2017) Asymmetry of the winter extra–tropical teleconnections in the Northern Hemisphere associated with two types of ENSO. Clim Dyn 48:2135–2151.  https://doi.org/10.1007/s00382-016-3196-2 CrossRefGoogle Scholar
  26. Folland C, Palmer T, Parker D (1986) Sahel rainfall and worldwide sea temperatures 1901–85. Nature 320:602–607.  https://doi.org/10.1038/320602a0 CrossRefGoogle Scholar
  27. García-Herrera R, Calvo N, Garcia RR, Giorgetta MA (2006) Propagation of ENSO temperature signals into the middle atmosphere: a comparison of two general circulation models and ERA-40 reanalysis data. J Geophys Res 111:D06101.  https://doi.org/10.1029/2005JD006061 Google Scholar
  28. García-Serrano J, Cassou C, Douville H, Giannini A, Doblas-Reyes FJ (2017) Revisiting the ENSO teleconnection to the tropical North Atlantic. J Clim 30:6945–6957.  https://doi.org/10.1175/JCLI-D-16-0641.1 CrossRefGoogle Scholar
  29. Garfinkel CI, Hurwitz MM, Waugh DW, Butler AH (2013) Are the teleconnections of central Pacific and eastern Pacific El Niño distinct in boreal wintertime? Clim Dyn 41:1835–1852.  https://doi.org/10.1007/s00382-012-1570-2 CrossRefGoogle Scholar
  30. Giannini A, Kushnir Y, Cane MA (2000) Interannual variability of Caribbean rainfall, ENSO, and the Atlantic Ocean. J Clim 13: 297–311.  https://doi.org/10.1175/1520-0442(2000)013,0297:IVOCRE.2.0.CO;2 CrossRefGoogle Scholar
  31. Giannini A, Chiang JCH, Cane MA, Kushnir Y, Seager R (2001) The ENSO teleconnection to the tropical Atlantic Ocean: contributions of the remote and local SSTs to rainfall variability in the tropical Americas. J Clim 14:4530–4544CrossRefGoogle Scholar
  32. Graf HF, Zanchettin D (2012) Central Pacific El Niño, the “subtropical bridge,” and Eurasian climate. J Geophys Res Atmos 117:D01102.  https://doi.org/10.1029/2011JD016493 CrossRefGoogle Scholar
  33. Ham YG, Kug JS, Park JY, Jin FF (2013) Sea surface temperature in the north tropical Atlantic as a trigger for El Niño/Southern Oscillation events. Nat Geosci 6:112–116.  https://doi.org/10.1038/ngeo1686 CrossRefGoogle Scholar
  34. Ham YG, Sung MK, An SI, Schubert S, Kug JS (2014) Role of tropical Atlantic SST variability as a modulator of El Niño teleconnections. Asia Pac J Atmos Sci 50:247–261.  https://doi.org/10.1007/s13143-014-0013-x CrossRefGoogle Scholar
  35. Handoh IC, Bigg GR (2000) A self-sustaining climate mode in the tropical Atlantic, 1995–1997: observations and modelling. Q J Roy Meteor Soc 126:807–821CrossRefGoogle Scholar
  36. Handoh IC, Matthews AJ, Bigg GR, Steven DP (2006) Interannual variability of tropical Atlantic independent of or associated with ENSO: part 1. The North Tropical Atlantic. Int J Climatol 26:1937–1956.  https://doi.org/10.1002/joc.1343 CrossRefGoogle Scholar
  37. Hatzaki M, Wu RG (2015) The south-eastern Europe winter precipitation variability in relation to the North Atlantic SST. Atmos Res 152:61–68.  https://doi.org/10.1016/j.atmosres.2013.10.008 CrossRefGoogle Scholar
  38. Hegyi BM, Deng Y (2011) A dynamical fingerprint of tropical Pacific sea surface temperatures on the decadal-scale variability of cool-season Arctic precipitation. J Geophys Res 116:D20121.  https://doi.org/10.1029/2011JD016001 CrossRefGoogle Scholar
  39. Hegyi BM, Deng Y, Black RX, Zhou R (2014) Initial transient response of the winter polar stratospheric vortex to idealized equatorial Pacific sea surface temperature anomalies in the NCAR WACCM. J Clim 27:2699–2713.  https://doi.org/10.1175/JCLI-D-13-00289.1 CrossRefGoogle Scholar
  40. Huang B, Shukla J (2005) Ocean-atmosphere interactions in the tropical and subtropical Atlantic Ocean. J Clim 18:1652–1672.  https://doi.org/10.1175/JCLI3368.1 CrossRefGoogle Scholar
  41. Huang JP, Higuchi K, Shabbar A (1998) The relationship between the North Atlantic Oscillation and El Niño-Southern Oscillation. Geophys Res Lett 25:2707–2710.  https://doi.org/10.1029/98GL01936 CrossRefGoogle Scholar
  42. Huang B, Schopf PS, Pan Z (2002) The ENSO effect on the tropical Atlantic variability: a regionally coupled model study. Geophys Res Lett 29:2039.  https://doi.org/10.1029/2002GL014872 CrossRefGoogle Scholar
  43. Huang B, Schopf PS, Shukla J (2004) Intrinsic ocean–atmosphere variability of the tropical Atlantic Ocean. J Clim 17:2058–2077.  https://doi.org/10.1175/1520-0442(2004)017,2058:IOVOTT.2.0.CO;2 CrossRefGoogle Scholar
  44. Huo LW, Guo PW, Hameed SN, Jin DC (2015) The role of tropical Atlantic SST anomalies in modulating western North Pacific tropical cyclone genesis. Geophys Res Lett 42:2378–2384.  https://doi.org/10.1002/2015GL063184 CrossRefGoogle Scholar
  45. Jimenez-Esteve B, Domeisen DIV (2018) The tropospheric pathway of the ENSO-North Atlantic teleconnection. J Clim 31:4563–4584.  https://doi.org/10.1175/JCLI-D-17-0716.1 CrossRefGoogle Scholar
  46. Kalnay E et al (1996) The NCEP/NCAR 40-year reanalysis project. Bull Am Meteor Soc 77:437–471  https://doi.org/10.1175/1520-0477(1996)077,0437:TNYRP.2.0.CO;2 CrossRefGoogle Scholar
  47. Kao HY, Yu JY (2009) Contrasting eastern-Pacific and central-Pacific types of ENSO. J Clim 22:615–632.  https://doi.org/10.1175/2008JCLI2309.1 CrossRefGoogle Scholar
  48. Klein SA, Soden BJ, Lau NC (1999) Remote sea surface temperature variations during ENSO: evidence for a tropical atmospheric bridge. J Clim 12: 917–932.  https://doi.org/10.1175/1520-0442(1999)012%3C0917:RSSTVD%3E2.0.CO;2 CrossRefGoogle Scholar
  49. 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 135:569–579.  https://doi.org/10.1002/qj.406 CrossRefGoogle Scholar
  50. Kug JS, Jin FF, An SI (2009) Two types of El Niño events: cold tongue El Niño and warm pool El Niño. J Clim 22:1499–1515CrossRefGoogle Scholar
  51. Lee SK, Enfield DB, Wang C (2008) Why do some El Niños have no impact on tropical North Atlantic SST? Geophys Res Lett 35:L16705.  https://doi.org/10.1029/2008GL034734 CrossRefGoogle Scholar
  52. Liu Z, Zhang Q, Wu L (2004) Remote impact on tropical Atlantic climate variability: statistical assessment and dynamic assessment. J Clim 17: 1529–1549.  https://doi.org/10.1175/1520-0442(2004)017%3C1529:RIOTAC%3E2.0.CO;2 CrossRefGoogle Scholar
  53. López-Parages J, Rodríguez-Fonseca B, Terray L (2015) A mechanism for the multidecadal modulation of ENSO teleconnection with Europe. Clim Dyn 45:867–880CrossRefGoogle Scholar
  54. López-Parages J, Rodríguez-Fonseca B, Dommenget D, Frauen C (2016a) ENSO influence on the North Atlantic European climate: a non-linear and non-stationary approach. Clim Dyn 47:2071–2084CrossRefGoogle Scholar
  55. López-Parages J, Rodríguez-Fonseca B, Mohino E, Losada T (2016b) Multidecadal modulation of ENSO teleconnection with Europe in late winter: analysis of CMIP5 models. J Clim 29:8067–8081CrossRefGoogle Scholar
  56. Manzini E, Giorgetta MA, Esch M, Kornblueh L, Roeckner E (2006) The influence of sea surface temperatures on the northern winter stratosphere: ensemble simulations with the MAECHAM5 model. J Clim 19:3863–3881CrossRefGoogle Scholar
  57. Marshall J, Kushnir Y, Battisti D, Chang P, Czaja A, Dockson R, Hurrell J, McCartney M, Saravanan R, Bisbeck M (2001) North Atlantic climate variability: phenomena, impacts and mechanisms. Int J Climatol 21:1863–1898.  https://doi.org/10.1002/joc.693 CrossRefGoogle Scholar
  58. Martin-Rey M, Rodriguez-Fonseca B, Polo I (2015) Atlantic opportunities for ENSO prediction. Geophys Res Lett 42:6802–6810.  https://doi.org/10.1002/2015GL065062 CrossRefGoogle Scholar
  59. Mo KC, Hakkinen S (2001) Interannual variability in the tropical Atlantic and linkages to the Pacific. J Clim 14:2740–2762CrossRefGoogle Scholar
  60. Nobre P, Shukla J (1996) Variations of sea surface temperature, wind stress, and rainfall over the tropical Atlantic and South America. J Clim 9:2464–2479CrossRefGoogle Scholar
  61. Perlwitz J, Graf HF (1995) The statistical connection between tropospheric and stratospheric circulation of the Northern Hemisphere in winter. J Clim 8: 2281–2295.  https://doi.org/10.1175/1520-0442(1995)008%3C2281:TSCBTA%3E2.0.CO;2 CrossRefGoogle Scholar
  62. Rayner NA, Parker DE, Horton EB, Folland CK, Alexander LV, Rowell DP, Kent EC, Kaplan A (2003) Global analyses of sea surface temperature, sea ice, and night marine air temperature since the late nineteenth century. J Geophys Res 108:4407.  https://doi.org/10.1029/2002JD002670 CrossRefGoogle Scholar
  63. Rodrigues RR, McPhaden MJ (2014) Why did the 2011–2012 La Niña cause a severe drought in the Brazilian Northeast? Geophys Res Lett 41:1012–1018.  https://doi.org/10.1002/2013GL058703 CrossRefGoogle Scholar
  64. Rodrigues RR, Haarsma RJ, Campos EJD, Ambrizzi T (2011) The impacts of Inter-El Niño variability on the Tropical Atlantic and Northeast Brazil climate. J Clim 24:3402–3422CrossRefGoogle Scholar
  65. Saravanan R, Chang P (2000) Interaction between tropical Atlantic variability and El Niño-Southern Oscillation. J Clim 13: 2177–2194.  https://doi.org/10.1175/1520-0442(2000)013%3C2177:IBTAVA%3E2.0.CO;2 CrossRefGoogle Scholar
  66. Smith TM, Reynolds RW, Peterson TC, Lawrimore L (2008) Improvements to NOAA’s historical merged land–ocean surface temperature analysis (1880–2006). J Clim 21:2283–2296.  https://doi.org/10.1175/2007JCLI2100.1 CrossRefGoogle Scholar
  67. Sutton RT, Jewson SP, Rowell DP (2000) The elements of climate variability in the tropical Atlantic region. J Clim 13:3261–3284CrossRefGoogle Scholar
  68. Takaya K, Nakamura H (2001) A formulation of a phase-independent wave-activity flux for stationary and migratory quasi-geostrophic eddies on a zonally varying basic flow. J Atmos Sci 58(6):608–627.  https://doi.org/10.1175/1520-0469(2001)058%3C0608:AFOAPI%3E2.0.CO;2 CrossRefGoogle Scholar
  69. Taschetto AS, Rodrigues RR, Meehl GA, McGregor S, England MH (2016) How sensitive are the Pacific-North Atlantic teleconnections to the position and intensity of El Niño-related warming. Clim Dyn 46:1841–1860CrossRefGoogle Scholar
  70. Wang CZ (2005) ENSO, Atlantic climate variability and the Walker and Hadley circulations. In: Diaz HF, Bradley RS (eds) The Hadley circulation: present, past and future. Cambridge University Press, Cambridge, pp 173–202Google Scholar
  71. Wang X, Wang CZ, Zhou W, Wang DX, Song J (2011) Teleconnected influence of North Atlantic sea surface temperature on the El Niño onset. Clim Dyn 37:663–676.  https://doi.org/10.1007/s00382-010-0833-z CrossRefGoogle Scholar
  72. Wei K, Takahashi M, Chen W (2015) Long-term changes in the relationship between stratospheric circulation and East Asian winter monsoon. Atmos Sci Let 16:359–365.  https://doi.org/10.1002/asl2.568 CrossRefGoogle Scholar
  73. Weng H, Ashok K, Behera SK, Rao SA, Yamagata T (2007) Impacts of recent El Niño Modoki dry/wet conditions in the Pacific Rim during boreal summer. Clim Dyn 29(2–3):113–129.  https://doi.org/10.1007/s00382-007-0234-0 CrossRefGoogle Scholar
  74. Wu RG, Kirtman BP (2011) Caribbean Sea rainfall variability during the rainy season and relationship to the equatorial Pacific and tropical Atlantic SST. Clim Dyn 37:1533–1550.  https://doi.org/10.1007/s00382-010-0927-7 CrossRefGoogle Scholar
  75. Wu LX, Liu ZY (2002) Is tropical Atlantic variability driven by the North Atlantic Oscillation? Geophys Res Lett 29:1653.  https://doi.org/10.1029/2002GL014939 CrossRefGoogle Scholar
  76. Wu RG, Yang S, Liu S, Sun L, Lian L, Gao ZT (2011) Northeast China summer temperature and North Atlantic SST. J Geophys Res 116:D16116.  https://doi.org/10.1029/2011JD015779 CrossRefGoogle Scholar
  77. Xie SP, Philander SGH (1994) A coupled ocean-atmosphere model of relevance to the ITCZ in the eastern Pacific. Tellus 46A:340–350CrossRefGoogle Scholar
  78. Yeh SW, Kug JS, Dewitte B, Kwon MH, Kirkman BP, Jin FF (2009) El Niño in a changing climate. Nature 461:511–514.  https://doi.org/10.1038/nature08316 CrossRefGoogle Scholar
  79. Zhou LT, Wu RG (2015) Interdecadal variability of winter precipitation in NWC and its association with the North Atlantic SST change. Int J Climatol 35:1172–1179.  https://doi.org/10.1002/joc.4047 CrossRefGoogle Scholar

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Authors and Affiliations

  1. 1.Center for Monsoon System Research, Institute of Atmospheric PhysicsChinese Academy of SciencesBeijingChina
  2. 2.College of Earth and Planetary SciencesUniversity of Chinese Academy of SciencesBeijingChina

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