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Influence of winter Arctic sea ice concentration change on the El Niño–Southern Oscillation in the following winter

  • Shangfeng ChenEmail author
  • Renguang Wu
  • Wen Chen
  • Bin Yu
Article
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Abstract

The present study reveals a close connection between the winter Arctic sea ice concentration (ASIC) change over the Greenland–Barents Seas (GBS) and the El Niño–Southern Oscillation (ENSO) in the following winter. When there is more winter ASIC over the GBS, an El Niño-like sea surface temperature (SST) warming tends to occur in the tropical central-eastern Pacific (TCEP) during the following winter. It is found that the winter ASIC increase over the GBS triggers an atmospheric wave train propagating southeastward from the high latitude Eurasia towards the subtropical North Pacific, with cyclonic wind anomalies over the subtropical North Pacific. A barotropic model experiment with anomalous convergence prescribed around the GBS reproduces reasonably well the atmospheric wave train. The induced spring SST warming and associated anomalous atmospheric heating over the subtropical North Pacific play an essential role in the formation and maintenance of lower-level westerly wind anomalies over the western tropical Pacific. These westerly wind anomalies induce SST warming in the TCEP during the following summer via triggering an eastward propagating equatorial warm Kelvin wave. The summer TCEP SST warming further develops into an El Niño event in the following winter via a Bjerknes-like positive air–sea feedback process. This result suggests that the winter ASIC change around the GBS is a potential predictor of the ENSO events with a lead time of 1 year.

Keywords

Arctic sea ice ENSO Atmospheric wave train Westerly winds 

Notes

Acknowledgements

We thank two anonymous reviewers for their constructive suggestions and comments, which help to improve the paper. This study is supported by the National Natural Science Foundation of China Grants (41605050, 41530425, and 41775080), and the Young Elite Scientists Sponsorship Program by the China Association for Science and Technology (2016QNRC001).

Supplementary material

382_2019_5027_MOESM1_ESM.doc (1.7 mb)
Supplementary material 1 (DOC 1719 kb)

References

  1. Alexander MA, Bladé I, Newman 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(16):2205–2231CrossRefGoogle Scholar
  2. Barbero R, Abatzoglou JT, Brown TJ (2015) Seasonal reversal of the influence of El Niño–Southern Oscillation on very large wildfire occurrence in the interior northwestern United States. Geophys Res Lett 42(9):3538–3545CrossRefGoogle Scholar
  3. Barnett T, Dümenil L, Schlese U, Roeckner E, Latif M (1989) The effect of Eurasian snow cover on regional and global climate variations. J Atmos Sci 46(5):661–686CrossRefGoogle Scholar
  4. Battisti DS (1988) Dynamics and thermodynamics of a warming event in a coupled tropical atmosphere-ocean model. J Atmos Sci 45:2889–2919CrossRefGoogle Scholar
  5. Bell GD, Halpert MS, Kousky VE, Gelman ME, Ropelewski CF, Douglas AV, Schnell RC (1999) Climate assessment for 1998. Bull Am Meteorol Soc 80(5):1040CrossRefGoogle Scholar
  6. Bjerknes J (1969) Atmospheric teleconnections from the equatorial Pacific. Mon Weather Rev 97:163–172CrossRefGoogle Scholar
  7. Burn DH, Whitfield PH (2015) Changes in floods and flood regimes in Canada. Can Water Resour J 41(1–2):139–150Google Scholar
  8. Cavalieri DJ, Parkinson CL (2012) Arctic sea ice variability and trends, 1979–2010. Cryosphere 6:881–889CrossRefGoogle Scholar
  9. Chan JCL (2005) Interannual and interdecadal variations of tropical cyclone activity over the western North Pacific. Meteorol Atmos Phys 89:143–152CrossRefGoogle Scholar
  10. Chan JCL, Zhou W (2005) PDO, ENSO and the summer monsoon rainfall over South China. Geophys Res Lett 32:L08810Google Scholar
  11. Chen S, Song L (2019) The leading interannual variability modes of winter surface air temperature over Southeast Asia. Clim Dyn 52:4715–4734CrossRefGoogle Scholar
  12. Chen S, Wu R (2018) Impacts of early autumn arctic sea ice concentration on subsequent spring Eurasian surface air temperature variations. Clim Dyn 51:2523–2542CrossRefGoogle Scholar
  13. 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 17:48–60CrossRefGoogle Scholar
  14. Chen S, Yu B, Chen W (2014a) An analysis on the physical process of the influence of AO on ENSO. Clim Dyn 42(3–4):973–989CrossRefGoogle Scholar
  15. Chen Z, Wu R, Chen W (2014b) Impacts of autumn Arctic sea ice concentration changes on the East Asian winter monsoon variability. J Clim 27:5433–5450CrossRefGoogle Scholar
  16. Chen S, Wu R, Chen W, Yu B (2015) Influence of the November Arctic Oscillation on the subsequent tropical Pacific sea surface temperature. Int J Climatol 35:4307–4317CrossRefGoogle Scholar
  17. Chen S, Wu R, Chen W, Yu B, Cao X (2016a) Genesis of westerly wind bursts over the equatorial western Pacific during the onset of the strong 2015–2016 El Niño. Atmos Sci Lett 17:384–391CrossRefGoogle Scholar
  18. Chen S, Wu R, Liu Y (2016b) Dominant modes of interannual variability in Eurasian surface air temperature during boreal spring. J Clim 29:1109–1125CrossRefGoogle Scholar
  19. Chen S, Wu R, Chen W (2018a) A strengthened impact of November Arctic oscillation on subsequent tropical Pacific sea surface temperature variation since the late-1970s. Clim Dyn 51:511–529CrossRefGoogle Scholar
  20. Chen S, Chen W, Yu B (2018b) Modulation of the relationship between spring AO and the subsequent winter ENSO by the preceding November AO. Sci Rep 8:6943CrossRefGoogle Scholar
  21. Chen S, Yu B, Chen W, Wu R (2018c) A review of atmosphere–ocean forcings outside the tropical Pacific on the El Nino–Southern oscillation occurrence. Atmosphere 9:439CrossRefGoogle Scholar
  22. Chen S, Wu R, Chen W (2019a) Enhanced impact of Arctic sea ice change during boreal autumn on the following spring Arctic oscillation since the mid-1990s. Clim Dyn.  https://doi.org/10.1007/s00382-019-04886-y CrossRefGoogle Scholar
  23. Chen S, Wu R, Song L, Chen W (2019b) Interannual variability of surface air temperature over mid-high latitudes of Eurasia during boreal autumn. Clim Dyn 53:1805–1821.  https://doi.org/10.1007/s00382-019-04738-9 CrossRefGoogle Scholar
  24. Chiang JCH, Vimont DJ (2004) Analogous Pacific and Atlantic meridional modes of tropical atmosphere–ocean variability. J Clim 17(21):4143–4158CrossRefGoogle Scholar
  25. Cohen J, Entekhabi D (1999) Eurasian snow cover variability and Northern Hemisphere climate predictability. Geophys Res Lett 26(3):345–348CrossRefGoogle Scholar
  26. Cohen J, Entekhabi D (2001) The influence of snow cover on Northern Hemisphere climate variability. Atmos Ocean 39:35–53CrossRefGoogle Scholar
  27. Cohen J, Barlow MA, Kushner PJ, Saito K (2007) Stratosphere–troposphere coupling and links with Eurasian land surface variability. J Clim 20(21):5335–5343CrossRefGoogle Scholar
  28. Cohen JL, Furtado JC, Barlow MA, Alexeev VA, Cherry JE (2012) Arctic warming, increasing snow cover and widespread boreal winter cooling. Environ Res Lett 7(1):014007CrossRefGoogle Scholar
  29. Comiso JC, Parkinson CL, Gersten R, Stock L (2008) Accelerated decline in the Arctic sea ice cover. Geophys Res Lett 35:L01703CrossRefGoogle Scholar
  30. Ding S, Chen W, Graf HF, Guo Y, Nath D (2018) Distinct winter patterns of tropical Pacific convection anomaly and the associated extratropical wave trains in the Northern Hemisphere. Clim Dyn 51:2003–2022CrossRefGoogle Scholar
  31. Duchon CE (1979) Lanczos filtering in one and two dimensions. J Appl Meteorol 18:1016–1022CrossRefGoogle Scholar
  32. Francis JA, Chan W, Leathers DJ, Miller JR, Veron DE (2009) Winter Northern Hemisphere weather patterns remember summer Arctic sea-ice extent. Geophys Res Lett 36:L07503CrossRefGoogle Scholar
  33. Gao Y, Sun J, Li F, He S, Stein S, Yan Q, Zhang Z, Katja L, Noel K, Tore F, Suo L (2015) Arctic sea ice and Eurasian climate: a review. Adv Atmos Sci 32:92–114CrossRefGoogle Scholar
  34. Gill AE (1980) Some simple solutions for heat-induced tropical circulation. Q J R Meteorol Soc 106:447–462CrossRefGoogle Scholar
  35. Glynn PW, de Weerdt WH (1991) Elimination of two reef-building hydrocorals following the 1982–83 El Niño warming event. Science 253(5015):69–71CrossRefGoogle Scholar
  36. Graf HF, Zanchettin D (2012) Central Pacific El Niño, the “subtropical bridge” and Eurasian climate. J Geophys Res 117:D01102CrossRefGoogle Scholar
  37. Gray WM (1984) Atlantic seasonal hurricane frequency. Part I: El Niño and 30 mb quasi-biennial oscillation influences. Mon Weather Rev 112:1649–1668CrossRefGoogle Scholar
  38. Ham YG, Kug JS, Park JY, Jin FF (2013) Sea surface temperature in the north tropical Atlantic as a trigger for El Nino/Southern Oscillation events. Nat Geosci 6:112–116CrossRefGoogle Scholar
  39. He S (2015) Asymmetry in the Arctic Oscillation teleconnection with January Cold extremes in Northeast China. Atmos Ocean Sci Lett 8:386–391Google Scholar
  40. He S, Gao Y, Furevik T, Wang H, Li F (2018) Teleconnection between sea ice in the Barents Sea in June and the Silk Road, Pacific-Japan and East Asian rainfall patterns in August. Adv Atmos Sci 35:52–64CrossRefGoogle Scholar
  41. Honda M, Inoue J, Yamane S (2009) Influence of low Arctic sea-ice minima on anomalously cold Eurasian winters. Geophys Res Lett 36:L08707CrossRefGoogle Scholar
  42. Hu C, Yang S, Wu Q, Li Z, Chen J, Deng K, Zhang T, Zhang C (2016) Shifting El Niño inhibits summer Arctic warming and Arctic sea ice melting over the Canada Basin. Nat Commun 7:11721CrossRefGoogle Scholar
  43. Hu C, Zhang C, Song Yang, Chen D, He S (2018) Perspective on the northwestward shift of autumn tropical cyclogenesis locations over the western North Pacific from shifting ENSO. Clim Dyn 51:2455–2465CrossRefGoogle Scholar
  44. Huang B et al (2017) Extended Reconstructed Sea Surface Temperature version 5 (ERSSTv5), Upgrades, validations, and intercomparisons. J Clim 30:8179–8205CrossRefGoogle Scholar
  45. Jevrejeva S, Moore JC, Grinsted A (2003) Influence of the Arctic Oscillation and El Niño–Southern Oscillation (ENSO) on ice conditions in the Baltic Sea: the wavelet approach. J Geophys Res 108:D21CrossRefGoogle Scholar
  46. Jin FF (1997) An equatorial ocean recharge paradigm for ENSO. Part I: Conceptual model. J Atmos Sci 54:811–829CrossRefGoogle Scholar
  47. Jin FF, Kim ST, Bejarano L (2006) A coupled-stability index for ENSO. Geophys Res Lett 33:L23708CrossRefGoogle Scholar
  48. Kalnay E, Kanamitsu M, Kistler R, Collins W, Deaven D, Gandin L, Iredell M, Saha S, White G, Woollen J (1996) The NCEP/NCAR 40-year reanalysis project. Bull Am Meteorol Soc 77:437–471CrossRefGoogle Scholar
  49. Kim SY, Son HY, Kug JS (2018) Relative roles of equatorial central Pacific and western North Pacific precipitation anomalies in ENSO teleconnection over the North Pacific. Clim Dyn 51:4345–4355CrossRefGoogle Scholar
  50. Kug JS, Jeong JH, Jang YS, Kim BM, Folland CK, Min SK, Son SW (2015) Two distinct influences of Arctic warming on cold winters over North America and East Asia. Nat Geosci 8:759–762.  https://doi.org/10.1038/ngeo2517 CrossRefGoogle Scholar
  51. Latif M et al (1998) A review of the predictability and prediction of ENSO. J Geophys Res 14:375–393Google Scholar
  52. Lau NC, Nath MJ (1996) The role of the ‘‘atmospheric bridge’’ in linking tropical Pacific ENSO events to extratropical SST anomalies. J Clim 9:2036–2057CrossRefGoogle Scholar
  53. Lengaigne M, Guilyardi E, Boulanger J-P, Menkes C, Delecluse P, Inness P, Cole J, Slingo J (2004) Triggering of El Niño by westerly wind events in a coupled general circulation model. Clim Dyn 23:601–620CrossRefGoogle Scholar
  54. Lewis SL, Brando PM, Phillips OL, van der Heijden GMF, Nepstad D (2011) The 2010 Amazon drought. Science 331(6017):554CrossRefGoogle Scholar
  55. Li CY (1990) Interaction between anomalous winter monsoon in East Asia and EI Niño Events. Adv Atmos Sci 7:36CrossRefGoogle Scholar
  56. Li F, Wang HJ (2013) Relationship between Bering Sea ice cover and East Asian winter monsoon year-to-year variations. Adv Atmos Sci 30:48–56CrossRefGoogle Scholar
  57. Li JP, Wu ZW (2012) Importance of autumn Arctic sea ice to northern winter snowfall. Proc Natl Acad Sci USA 109:E1898CrossRefGoogle Scholar
  58. Li X, Wu ZW, Li Y (2019) A link of China warming hiatus with the winter sea ice loss in Barents-Kara Seas. Clim Dyn 53:2625–2642.  https://doi.org/10.1007/s00382-019-04645-z CrossRefGoogle Scholar
  59. Liu J, Curry JA, Martinson DG (2004) Interpretation of recent Antarctic sea ice variability. Geophys Res Lett 31:L02205Google Scholar
  60. Liu JP, Curry JA, Wang HJ, Song MR, Horton RM (2012) Impact of declining Arctic sea ice on winter snowfall. Proc Natl Acad Sci USA 109:4074–4079CrossRefGoogle Scholar
  61. McPhaden MJ, Zebiak SE, Glantz MH (2006) ENSO as an integrating concept in Earth science. Science 314(5806):1740–1745CrossRefGoogle Scholar
  62. Nakamura T, Tachibana Y, Honda M, Yamane S (2006) Influence of the Northern Hemisphere annular mode on ENSO by modulating westerly wind bursts. Geophys Res Lett 33:L07709Google Scholar
  63. Nakamura T, Tachibana Y, Shimoda H (2007) Importance of cold and dry surges in substantiating the NAM and ENSO relationship. Geophys Res Lett 34:L22703CrossRefGoogle Scholar
  64. Nakamura T, Yamazaki K, Iwamoto K, Honda M, Miyoshi Y, Ogawa Y, Ukita J (2015) A negative phase shift of the winter AO/NAO due to the recent Arctic sea-ice reduction in late autumn. J Geophys Res 120:3209–3227CrossRefGoogle Scholar
  65. Overland JE, Adams JM, Bond NA (1999) Decadal variability of the Aleutian Low and its relation to high-latitude circulation. J Clim 12:1542–1548CrossRefGoogle Scholar
  66. Park JY, Yeh SW, Kug JS, Yoon J (2013) Favorable connections between seasonal footprinting mechanism and El Niño. Clim Dyn 40:1169–1181CrossRefGoogle Scholar
  67. Peixoto JP, Oort AH (1992) Physics of climate. Springer, New YorkCrossRefGoogle Scholar
  68. Philander SG (1985) El Niño and La Niña. J Atmos Sci 42:2652–2662CrossRefGoogle Scholar
  69. 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 108:4407CrossRefGoogle Scholar
  70. Rogers JC (1981) The North Pacific oscillation. J Climatol 1(1):39–57CrossRefGoogle Scholar
  71. Ropelewski CF, Halpert MS (1987) Global and regional scale precipitation patterns associated with the El Niño/Southern Oscillation. Mon Wea Rev 115(8):1606–1626CrossRefGoogle Scholar
  72. Sardeshmukh PD, Hoskins BJ (1988) The generation of global rotational flow by steady idealized tropical divergence. J Atmos Sci 45:1228–1251CrossRefGoogle Scholar
  73. Schopf MJ, Suares PS (1988) A delayed action oscillator for ENSO. J Atmos Sci 45:3283–3287CrossRefGoogle Scholar
  74. Screen JA, Deser C, Simmonds I, Tomas R (2014) Atmospheric impacts of Arctic sea-ice loss, 1979–2009: Separating forced change from atmospheric internal variability. Clim Dyn 43:333–344CrossRefGoogle Scholar
  75. Smith TM, Reynolds RW, Peterson TC, Lawrimore J (2008) Improvements to NOAA’s historical merged land-ocean surface temperature analysis (1880–2006). J Clim 21:2283–2296CrossRefGoogle Scholar
  76. Son HY, Park JY, Kug JS, Yoo J, Kim CH (2014) Winter Precipitation variation over Korean Peninsula associated with ENSO. Clim Dyn 42:3171–3186CrossRefGoogle Scholar
  77. Song LY, Chen S, Chen W, Chen X (2017) Distinct impacts of two types of La Niña events on Australian Summer rainfall. Int J Climatol 37:2532–2544CrossRefGoogle Scholar
  78. Takaya K, Nakamura H (1997) A formulation of a wave activity flux for stationary Rossby waves on a zonally varying basic flow. Geophys Res Lett 24:2985–2988CrossRefGoogle Scholar
  79. Takaya K, Nakamura H (2001) A formulation of a phase-independent wave activity flux for stationary and migratory quasigeostrophic eddies on a zonally varying basic flow. J Atmos Sci 58:608–627CrossRefGoogle Scholar
  80. Thompson DW, Wallace JM (1998) The Arctic Oscillation signature in the wintertime geopotential height and temperature fields. Geophys Res Lett 25(9):1297–1300CrossRefGoogle Scholar
  81. Vimont DJ, Battisti DS, Hirst AC (2001) Footprinting: a seasonal connection between the tropics and mid-latitudes. Geophys Res Lett 28:3923–3926CrossRefGoogle Scholar
  82. Vimont DJ, Wallace JM, Battisti DS (2003) The seasonal footprinting mechanism in the Pacific: implications for ENSO. J Clim 16:2668–2675CrossRefGoogle Scholar
  83. Walker GT, Bliss E (1932) World weather. V Mem R Meteorol Soc 4:53–84Google Scholar
  84. Wang B, Wu R, Fu X (2000) Pacific-East Asian teleconnection: how does ENSO affect East Asian climate? J Clim 13(9):1517–1536CrossRefGoogle Scholar
  85. Wang B, Yang J, Zhou T, Wang B (2008) Interdecadal changes in the major modes of Asian-Australian monsoon variability: strengthening relationship with ENSO since the late 1970s. J Clim 21:1771–1789CrossRefGoogle Scholar
  86. 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(3–4):663–676CrossRefGoogle Scholar
  87. Wang SY, L’Heureux M, Chia HH (2012) ENSO prediction one year in advance using western North Pacific sea surface temperatures. Geophys Res Lett 39:L05702Google Scholar
  88. Watanabe M (2004) Asian jet waveguide and a downstream extension of the North Atlantic Oscillation. J Clim 17(24):4674–4691CrossRefGoogle Scholar
  89. Wu R, Hu ZZ, Kirtman BP (2003) Evolution of ENSO-related rainfall anomalies in East Asia. J Clim 16:3742–3758CrossRefGoogle Scholar
  90. Wu BY, Su JZ, Zhang RH (2011) Effects of autumn-winter Arctic sea ice on winter Siberian High. Chin Sci Bull 56:3220–3228CrossRefGoogle Scholar
  91. Wu ZW, Li XX, Li YJ, Li Y (2016) Potential influence of Arctic sea ice to the interannual variations of East Asian spring precipitation. J Clim 29:2797–2813CrossRefGoogle Scholar
  92. Xie SP, Philander SGH (1994) A coupled ocean-atmosphere model of relevance to the ITCZ in the eastern Pacific. Tellus Ser A Dyn Meteorol Oceanol 46:340–350CrossRefGoogle Scholar
  93. Xu X, He S, Li F, Wang H (2018) Impact of northern Eurasian snow cover in autumn on the warm Arctic–cold Eurasia pattern during the following January and its linkage to stationary planetary waves. Clim Dyn 50:1993–2006CrossRefGoogle Scholar
  94. Yang X, Yuan X, Ting M (2016) Dynamical link between the Barents-Kara sea ice and the Arctic Oscillation. J Clim 29:5103–5122CrossRefGoogle Scholar
  95. Yu L, Rienecker MM (1998) Evidence of an extratropical atmospheric influence during the onset of the 1997–98 El Niño. Geophys Res Lett 25:3537–3540CrossRefGoogle Scholar
  96. Yu B, Zwiers F (2007) The impact of combined ENSO and PDO on the PNA climate: a 1,000-year climate modeling study. Clim Dyn 29:837–851CrossRefGoogle Scholar
  97. Yu L, Weller RA, Liu WT (2003) Case analysis of a role of ENSO in regulating the generation of westerly wind bursts in the western equatorial Pacific. J Geophys Res 108(C4):3128CrossRefGoogle Scholar
  98. Zhang Y, Wallace JM, Battisti DS (1997) ENSO-like interdecadal variability: 1900–93. J Clim 10(5):1004–1020CrossRefGoogle Scholar
  99. Zhang R, Sumi A, Kimoto M (1999) A diagnostic study of the impact of El Niño on the precipitation in China. Adv Atmos Sci 16:229–241CrossRefGoogle Scholar

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© Springer-Verlag GmbH Germany, part of Springer Nature 2019

Authors and Affiliations

  1. 1.Center for Monsoon System Research, Institute of Atmospheric PhysicsChinese Academy of SciencesBeijingChina
  2. 2.School of Earth SciencesZhejiang UniversityHangzhouChina
  3. 3.Climate Research DivisionEnvironment and Climate Change CanadaTorontoCanada
  4. 4.University of Chinese Academy of SciencesBeijingChina

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