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Asymmetric impact of Central Pacific ENSO on the reduction of tropical cyclone genesis frequency over the western North Pacific since the late 1990s

  • Han-Kyoung Kim
  • Kyong-Hwan Seo
  • Sang-Wook Yeh
  • Nam-Young Kang
  • Byung-Kwon MoonEmail author
Article
  • 34 Downloads

Abstract

Tropical cyclone (TC) genesis frequency over the western North Pacific (WNP) is significantly reduced since the late 1990s, coinciding with a Pacific decadal oscillation (PDO) phase transition from positive to negative. In this study, the underlying mechanism for this change is investigated through analysis of asymmetric central Pacific (CP) El Niño-Southern Oscillation (ENSO) properties induced by the negative PDO phase. Our results suggest that the significant reduction is caused by asymmetric CP ENSO properties, in which the CP La Niña is more frequent than the CP El Niño during negative PDO phases; furthermore, stronger CP La Niña occurs during a negative PDO phase than during a positive PDO phase. CP La Niña (El Niño) events generate an anticyclonic (cyclonic) Rossby wave response over the eastern WNP, leading to a significant decrease (increase) in eastern WNP TC genesis. Therefore, more frequent CP La Niña events and the less frequent CP El Niño events reduce the eastern WNP mean TC genesis frequency during a negative PDO phase. In addition, stronger CP La Niña events during a negative PDO phase reinforce the reduction in eastern WNP TC genesis. The dependency of CP ENSO properties on the PDO phase is confirmed using a long-term climate model simulation, which supports our observational results. Our results will also improve understanding of TC in other basins, since both PDO and CP ENSO variability influence global dynamics.

Keywords

Tropical cyclone Pacific decadal oscillation Central Pacific El Niño-Southern oscillation 

Notes

Acknowledgements

This work was supported by a National Research Foundation of Korea (NRF) grant funded by the Korea government (MSIT; No. 2019R1A2C1008549).

References

  1. An S-I (2018) Impact of Pacific Decadal Oscillation on frequency asymmetry of El Niño and La Niña events. Adv Atmos Sci 35(5):493–494.  https://doi.org/10.1007/s00376-018-8024-7 CrossRefGoogle Scholar
  2. Camargo SJ, Emanuel KA, Sobel AH (2007) Use of a genesis potential index to diagnose ENSO effects on tropical cyclone genesis. J Clim 20:4819–4834.  https://doi.org/10.1175/JCLI4282.1 CrossRefGoogle Scholar
  3. Chan JCL (2008) Decadal variations of intense typhoon occurrence in the western North Pacific. Proc R Soc A 464:249–272CrossRefGoogle Scholar
  4. Chen GH, Tam CY (2010) Different impacts of two kinds of Pacific Ocean warming on tropical cyclone frequency over the western North Pacific. Geophys Res Lett 37:L01803.  https://doi.org/10.1029/2009GL041708 CrossRefGoogle Scholar
  5. Choi YM, Ha K-J, Ho C-H, Chung CE (2015) Interdecadal change in typhoon genesis condition over the western North Pacific. Clim Dyn 45:3243–3255CrossRefGoogle Scholar
  6. Collins WD et al (2006) The community climate system model version 3 (CCSM3). J Clim 19:2122–2143.  https://doi.org/10.1175/JCLI3761.1 CrossRefGoogle Scholar
  7. Deser C, Capotondi A, Saravanan R, Phillips A (2006) Tropical Pacific and Atlantic variability in CCSM3. J Clim 19:2451–2481CrossRefGoogle Scholar
  8. Di Lorenzo E, Cobb KM, Furtado JC, Schneider N, Anderson BT, Bracco A, Alexander MA, Vimont DJ (2010) Central Pacific El Niño and decadal climate change in the North Pacific Ocean. Nat Geosci.  https://doi.org/10.1038/NGEO0984 CrossRefGoogle Scholar
  9. Di Lorenzo E, Liguori G, Schneider N, Furtado JC, Anderson BT, Alexander MA (2015) ENSO and meridional modes: a null hypothesis for Pacific climate variability. Geophys Res Lett 42:9440–9448CrossRefGoogle Scholar
  10. Eisenman I, Yu L, Tziperman E (2005) Westerly wind bursts: ENSO’s tail rather than the dog? J Clim 18:5224–5237.  https://doi.org/10.1175/JCLI3588.1 CrossRefGoogle Scholar
  11. Gill AE (1980) Some simple solutions for heat-induced tropical circulations. Q J Roy Meteor Soc 106:447–462.  https://doi.org/10.1002/qj.49710644905 CrossRefGoogle Scholar
  12. He H, Yang J, Gong D, Mao R, Wang Y, Gao M (2015) Decadal changes in tropical cyclone activity over the western North Pacific in the late 1990s. Clim Dyn 45:3317–3329CrossRefGoogle Scholar
  13. Hsu PC, Chu PS, Murakami H, Zhao X (2014) An abrupt decrease in the late-season typhoon activity over the western North Pacific. J Clim 27:4296–4313CrossRefGoogle Scholar
  14. Huang B, Banzon VF, Freeman E, Lawrimore J, Liu W, Peterson TC, Smith TM, Thorne PW, Woodruff SD, Zhang HM (2014) Extended reconstructed sea surface temperature version 4 (ERSST.v4): Part I. Upgrades and intercomparisons. J Clim 28:911–930.  https://doi.org/10.1175/JCLI-D-14-00006.1 CrossRefGoogle Scholar
  15. Jin C-S, Ho C-H, Kim J-H, Lee D-K, Yeh S-W (2013) Impact of central Pacific El Niño on tropical cyclone tracks over the East China Sea using WRF-based global and regional climate model. J Clim 26:2534–2545CrossRefGoogle Scholar
  16. Kalnay E, Kanamitsu M, Kistler R, Collins W, Deaven D, Gandin L, Iredell M, Saha S, White G, Woollen 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 Amer Meteorol Soc 77:437–471.  https://doi.org/10.1175/1520-0477(1996)077%3c0437:TNYRP%3e2.0.CO;2 CrossRefGoogle Scholar
  17. Kao H-Y, Yu J-Y (2009) Contrasting Eastern-Pacific and Central-Pacific types of ENSO. J Clim 22:615–632.  https://doi.org/10.1175/2008JCLI2309.1 CrossRefGoogle Scholar
  18. Kim H-K, Seo K-H (2016) Cluster analysis of tropical cyclone tracks over the western North Pacific using a self-organizing map. J Clim 29:3731–3751.  https://doi.org/10.1175/JCLI-D-15-0380.1 CrossRefGoogle Scholar
  19. Kim ST, Yu J-Y (2012) The two types of ENSO in CMIP5 models. Geophys Res Lett 39:L11704.  https://doi.org/10.1029/2012GL052006 CrossRefGoogle Scholar
  20. Li RCY, Zhou W (2013a) Modulation of western North Pacific tropical cyclone activity by the ISO. Part I: Genesis and intensity. J Clim 26:2904–2918.  https://doi.org/10.1175/JCLI-D-12-00210.1 CrossRefGoogle Scholar
  21. Li RCY, Zhou W (2013b) Modulation of Western North Pacific tropical cyclone activity by the ISO. Part II: Tracks and landfalls. J Clim 26:2919–2930.  https://doi.org/10.1175/JCLI-D-12-00211.1 CrossRefGoogle Scholar
  22. Lin RP, Zheng F, Dong X (2018) ENSO frequency asymmetry and the Pacific Decadal Oscillation in observations and 19 CMIP5 models. Adv Atmos Sci 35(5):495–506.  https://doi.org/10.1007/s00376-017-7133-z CrossRefGoogle Scholar
  23. Liu KS, Chan JCL (2013) Inactive period of Western North Pacific tropical cyclone activity in 1998–2011. J Clim 26:2614–2630CrossRefGoogle Scholar
  24. Liu Y, Chen GH (2018) Intensified influence of the ENSO modoki on boreal summer tropical cyclone genesis over the western North Pacific since the early 1990s. Int J Climatol.  https://doi.org/10.1002/joc.5347 CrossRefGoogle Scholar
  25. Liu W, Huang B, Thorne RW, Banzon VF, Zhang H-M, Freeman E, Lawrimore J, Peterson TC, Smith TM, Woodruff SD (2015) Extended reconstructed sea surface temperature version 4 (ERSST.v4): Part II. Parametric and structural uncertainty estimations. J Clim 28:931–951.  https://doi.org/10.1175/JCLI-D-14-00007.1 CrossRefGoogle Scholar
  26. Mantua NJ, Hare SR, Zhang Y, Wallace JM, Francis RC (1997) A Pacific interdecadal climate oscillation with impacts on salmon production. Bull Amer Meteor Soc 78:1069–1079CrossRefGoogle Scholar
  27. Moon I-J, Kim S-H, Chan JCL (2019) Climate change and tropical cyclone trend. Nature 570:E3–E5CrossRefGoogle Scholar
  28. Rodionov SN (2004) A sequential algorithm for testing climate regime shifts. Geophys Res Lett 31:L09204.  https://doi.org/10.1029/2004GL019448 CrossRefGoogle Scholar
  29. Wang B, Chan JCL (2002) How strong ENSO events affect tropical storm activity over the western North Pacific. J Clim 15:1643–1658.  https://doi.org/10.1175/1520-0442(2002)015%3c1643:HSEEAT%3e2.0.CO;2 CrossRefGoogle Scholar
  30. Wang B, Xiang B, Lee J-Y (2013a) Subtropical High predictability establishes a promising way for monsoon and tropical storm prediction. PNAS 110(8):2718–2722CrossRefGoogle Scholar
  31. Wang C, Li C, Mu M, Duan W (2013b) Seasonal modulations of different impacts of two types of ENSO events on tropical cyclone activity in the western North Pacific. Clim Dyn 11–12:2887–2902.  https://doi.org/10.1007/s00382-012-1434-9 CrossRefGoogle Scholar
  32. Yeh S-W, Kang S-K, Kirtman BP, Kim J-H, Kwon M-H, Kim C-H (2010) Decadal change in relationship between western North Pacific tropical cyclone frequency and the tropical Pacific SST. Meteorol Atmos Phys 106(3–4):179–189CrossRefGoogle Scholar
  33. Yeh S-W, Cai W, Min S-K, McPhaden MJ, Dommenget D, Dewitte B, Collins M, Ashok K, An S-I, Yim B-Y, Kug J-S (2018) ENSO atmospheric teleconnections and their response to greenhouse gas forcing. Rev Geophys 56:185–206.  https://doi.org/10.1002/2017RG000568 CrossRefGoogle Scholar
  34. Yu J-Y, Kim ST (2010) Identification of central-Pacific and eastern-Pacific types of El Niño in CMIP3 models. Geophys Res Lett 37:L15705.  https://doi.org/10.1029/2010GL044082 CrossRefGoogle Scholar
  35. Yu J-Y, Kao P-K, Paek H, Hsu H-H, Hung C-W, Lu M-M, An S-I (2015) Linking emergence of the Central Pacific El Niño to the Atlantic multidecadal oscillation. J Clim 28(2):651–662.  https://doi.org/10.1175/JCLI-D-14-00347.1 CrossRefGoogle Scholar
  36. Yu J, Li T, Tan Z, Zhu Z (2016) Effects of tropical North Atlantic SST on tropical cyclone genesis in the western North Pacific. Clim Dyn 46(3):865–877.  https://doi.org/10.1007/s00382-015-2618-x CrossRefGoogle Scholar
  37. Zhang W, Leung Y, Min J (2013) North Pacific Gyre Oscillation and the occurrence of western North Pacific tropical cyclones. Geophys Res Lett 40:5205–5211CrossRefGoogle Scholar
  38. Zhang W, Vecchi GA, Murakami H, Villarini G, Delworth TL, Yang X, Jia L (2016) The Pacific meridional mode and the occurrence of tropical cyclones in the Western North Pacific. J Clim 29(1):381–398.  https://doi.org/10.1175/JCLI-D-15-0282.1 CrossRefGoogle Scholar
  39. Zhang W, Vecchi GA, Murakami H, Villarini G, Delworth TL, Yang X, Jia L (2018) Dominant role of Atlantic multidecadal oscillation in the recent decadal changes in Western North Pacific tropical cyclone activity. Geophys Res Lett 45:354–362CrossRefGoogle Scholar
  40. Zhao H, Wang C (2016) Interdecadal modulation on the relationship between ENSO and typhoon activity during the late season in the Western North Pacific. Clim Dyn 47(1):315–328CrossRefGoogle Scholar
  41. Zhao H, Wang C (2019) On the relationship between ENSO and tropical cyclones in the western North Pacific during the boreal summer. Clim Dyn.  https://doi.org/10.1007/s00382-018-4136-0 CrossRefGoogle Scholar
  42. Zhao H, Duan X, Raga GB, Klotzbach PJ (2018) Changes in characteristics of rapidly intensifying western North Pacific tropical cyclones related to climate regime shifts. J Clim 31:8163–8179CrossRefGoogle Scholar
  43. Zhao H, Chen S, Klotzbach PJ (2019a) Recent strengthening of the relationship between the Western North Pacific monsoon and Western North Pacific tropical cyclone activity during the Boreal summer. J Clim.  https://doi.org/10.1175/JCLI-D-19-0016.1 CrossRefGoogle Scholar
  44. Zhao H, Zhang J, Klotzbach PJ, Chen S (2019b) Recent increased co-variability of tropical cyclogenesis latitude-longitude over the western North Pacific during the extended boreal summer. J Clim.  https://doi.org/10.1175/JCLI-D-19-0009.1 CrossRefGoogle Scholar

Copyright information

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

Authors and Affiliations

  1. 1.Division of Science Education/Institute of Fusion ScienceJeonbuk National UniversityJeonjuSouth Korea
  2. 2.Department of Atmospheric Sciences, Division of Earth Environmental SystemPusan National UniversityBusanSouth Korea
  3. 3.Marine Sciences and Convergent Technology, ERICAHanyang UniversityAnsanSouth Korea
  4. 4.National Typhoon CenterKorea Meteorological AdministrationJejuSouth Korea
  5. 5.Department of Geography, College of Social SciencesKyungpook National UniversityDaeguSouth Korea

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