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Decadal change in ENSO related seasonal precipitation over southern China under influences of ENSO and its combination mode

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Abstract

Existing researches have suggested that the meridionally quasisymmetric El Niño/Southern Oscillation (ENSO) mode and the antisymmetric combination mode (C-mode; reflecting the nonlinear atmospheric interaction between ENSO variability and the annual cycle) can significantly influence the seasonal precipitation over southern China during the boreal winter and spring. By using atmospheric reanalysis data and gridded precipitation observations, this study demonstrates that these influences have an obvious decadal change in their impact intensity and in the region over southern China around 2000, coincident with the climate shift that occurred over the tropical Pacific after the late 1990s. The precipitation anomalies dominantly influenced by ENSO mode shifted from southern China in winter during the 1980s–1990s to the Yangtze River Valley in spring after the 2000s. Additionally, the precipitation anomalies independently affected by C-mode were concentrated over southern China in spring, and their effects were further enhanced in the 2000s–2010s. The direct contribution of ENSO mode to southern China’s precipitation has declined. This decadal change in seasonal precipitation is largely due to different types of ENSO (eastern-Pacific/central-Pacific) accompanied by different atmospheric circulations over the western North Pacific (WNP) associated with C-mode responses. The understanding of this climate shift in the influences of ENSO mode and C-mode on affecting the seasonal precipitation over southern China indicates a potential opportunity for improving the ENSO mode/C-mode-related precipitation predictions over southern China.

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References

  • 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 15:2205–2231

    Google Scholar 

  • Battisti DS (1989) Interannual variability in a tropical atmosphere-ocean model: influence of the basic state, ocean geometry and nonlinearity. J Atmos Sci 46:1687–1712

    Google Scholar 

  • Bejarano L, Jin FF (2006) Coexistence of equatorial coupled modes of ENSO. J Clim 21:3051–3067

    Google Scholar 

  • Bjerknes J (1969) Atmospheric teleconnections from the equatorial Pacific. Mon Weather Rev 97:163–172

    Google Scholar 

  • Cai W et al (2012) More extreme swings of the South Pacific convergence zone due to greenhouse warming. Nature 488:365–369

    Google Scholar 

  • Cai W et al (2014) Increasing frequency of extreme El Niño events due to greenhouse warming. Nat Clim Change 4:111–116

    Google Scholar 

  • Capotondi A, Wittenberg AT, Newman M et al (2015) Understanding ENSO diversity. Bull Am Meteor Soc 96:921–938

    Google Scholar 

  • Dee DP et al (2011) The ERA-Interim reanalysis: configuration and performance of the data assimilation system. Q J R Meteorol Soc 137:553–597

    Google Scholar 

  • Deser C (1990) Large-scale atmospheric circulation features of warm and cold episodes in the tropical Pacific. J Clim 3:1254–1281

    Google Scholar 

  • Feng J, Wang L, Chen W, Fong SK, Leong KC (2010) Different impacts of two types of Pacific Ocean warming on Southeast Asian rainfall during boreal winter. J Geophys Res Atmos 115:D24122

    Google Scholar 

  • Gao T, Zhang Q, Luo M (2019) Intensifying effects of El Niño on winter precipitation extremes in southeastern China. Clim Dyn. https://doi.org/10.1007/s00382-019-05022-6

    Article  Google Scholar 

  • Gong D, Wang S (1999) Impacts of ENSO on rainfall of global land and China. Chin Sci Bull 44:852–857

    Google Scholar 

  • Harrison DE, Larkin NK (1970) The COADS sea level pressure signal: a near-global El Niño composite and time series view, 1946-1993. J Clim 9:3025–3055

    Google Scholar 

  • Hoskins BJ, Karoly DJ (1981) The steady linear response of a spherical atmosphere to thermal and orographic forcing. J Atmos Sci 38:1179–1196

    Google Scholar 

  • Huang R, Li W (1987) Influence of the heat source anomaly over the tropical western Pacific on the subtropical high over East Asia. In: Proceedings international conference on the general circulation of East Asia, Chengdu, China, 10–15 April 1987

  • Huang R, Wu Y (1989) The influence of ENSO on the summer climate change in China and its mechanism. Adv Atmos Sci 6:21–32

    Google Scholar 

  • Ineson S, Scaife AA (2009) The role of the stratosphere in the European climate response to El Niño. Nat Geosci 2:32–36

    Google Scholar 

  • Jia X, Ge J (2017) Interdecadal changes in the relationship between ENSO, EAWM, and the wintertime precipitation over China at the end of the twentieth century. J Clim 30:1923–1937

    Google Scholar 

  • Jin FF (1997) An equatorial ocean recharge paradigm for ENSO. Part II: a stripped-down coupled model. J Atmos Sci 54:830–847

    Google Scholar 

  • Jin FF (2000) An Equatorial ocean recharge paradigm for ENSO. Part I: conceptual model. J Atmos Sci 54:811–829

    Google Scholar 

  • Jo H-S, Yeh S-W, Kim C-H (2013) A possible mechanism for the North Pacific climate transitions of the winter of 1998/99. Geophys Res Lett 40:4380–4385

    Google Scholar 

  • Jones PD, Osborn TJ, Briffa KR (2001) The evolution of climate over the last millennium. Science 292:662–667

    Google Scholar 

  • Kao HY, Yu JY (2009) Contrasting eastern-Pacific and central-Pacific types of ENSO. J Clim 22:615–632

    Google Scholar 

  • Kug JS, Jin FF, An SI (2009) Two-types of El Niño events: cold tongue El Niño and warm Pool El Niño. J Clim 22:1499–1515

    Google Scholar 

  • Land C, Feichter J (2003) Stratosphere–troposphere exchange in a changing climate simulated with the general circulation model MAECHAM4. J Geophys Res 108:8523

    Google Scholar 

  • Lau NC, Nath MJ (2006) ENSO modulation of the interannual and intraseasonal variability of the East Asian monsoon-A model study. J Clim 19:4508–4530

    Google Scholar 

  • Li H, Zhang W, He JH (2016) Influences of ENSO and its combination mode on seasonal precipitation over eastern China. Acta Meteorol Sin 74:322–334 (in Chinese)

    Google Scholar 

  • Li T, Wang B, Wu B, Zhou TJ, Chang CP, Zhang RH (2017) Theories on formation of an anomalous anticyclone in western north Pacific during El Niño: a review. Journal of Meteorological Research 31:987–1006

    Google Scholar 

  • Luo M, Lau N-C (2019) Amplifying effect of ENSO on heat waves in China. Clim Dyn 52:3277–3289

    Google Scholar 

  • Luo JJ, Yuan CX, Sasaki W et al (2015) Current status of intraseasonal-seasonal-to-interannual prediction of the Indo-Pacific climate. In: Yamagata T, Behera S (eds) Chapter 3 in The Indo-Pacific climate variability and predictability, Asia-Pacific weather and climate book series, vol 7. The World Scientific Publisher, Singapore

    Google Scholar 

  • Luo M, Leung Y, Graf HF, Herzog M, Zhang W (2016) Interannual variability of the onset of the South China Sea summer monsoon. Int J Climatol 36:550–562

    Google Scholar 

  • Lyon B, Barnston AG, DeWitt DG (2013) Tropical pacific forcing of a 1998-1999 climate shift: observational analysis and climate model results for the boreal spring season. Clim Dyn 43:893–909

    Google Scholar 

  • Mcgregor S, Timmermann A, Schneider N, Stuecker MF, England MH (2012) The effect of the south Pacific convergence zone on the termination of El Niño events and the meridional asymmetry of ENSO. J Clim 25:5566–5586

    Google Scholar 

  • Mcgregor S, Ramesh N, Spence P, England MH, Mcphaden MJ, Santoso A (2013) Meridional movement of wind anomalies during ENSO events and their role in event termination. Geophys Res Lett 40:749–754

    Google Scholar 

  • Pedhazur EJ (1997) Multiple regression in behavioural research: explanation and prediction, 3rd edn. Holt, Rinchart, and Winston, Austin

    Google Scholar 

  • Philander SGH (1983) El Niño Southern oscillation phenomena. Nature 302:295–301

    Google Scholar 

  • Rasmusson EM, Carpenter TH (1982) Variations in tropical sea surface temperature and surface wind fields associated with the Southern Oscillation/El Niño. Mon Weather Rev 110:354–384

    Google Scholar 

  • Ren HL, Jin FF (2011) Niño indices for two types of ENSO. Geophys Res Lett 38:L04704. https://doi.org/10.1029/2010GL046031

    Article  Google Scholar 

  • Ren HL, Jin FF, Stuecker M (2013) ENSO regime change since the late 1970s as manifested by two types of ENSO. J Meteorol Soc Jpn 91:835–842

    Google Scholar 

  • Spiegel MR (1997) Schaum’s outline of theory and problems of statistics. McGraw-Hill, New York

    Google Scholar 

  • Stuecker MF, Timmermann A, Jin FF, Mcgregor S, Ren HL (2013) A combination mode of the annual cycle and the El Niño/Southern Oscillation. Nat Geosci 6:540–544

    Google Scholar 

  • Stuecker MF, Jin FF, Timmermann A, Mcgregor S (2015) Combination mode dynamics of the anomalous northwest Pacific anticyclone. J Clim 28:1093–1111

    Google Scholar 

  • Wallace JM, Gutzler DS (1981) Teleconnections in the geopotential height field during the northern Hemisphere winter. Mon Weather Rev 109:784–812

    Google Scholar 

  • Wallace JM, Rasmusson EM, Mitchell TP, Kousky VE, Sarachik ES, Storch H (1998) On the structure and evolution of ENSO-related climate variability in the tropical Pacific: lessons from TOGA. J Geophys Res Oceans 103:14241–14259

    Google Scholar 

  • Wang C, Wang X (2013) Classifying El Niño Modoki I and II by different impacts on rainfall in southern China and typhoon tracks. J Clim 26:1322–1338

    Google Scholar 

  • Wang B, Wu R, Fu X (2013) Pacific-East Asian teleconnection: how does ENSO affect East Asian climate? J Clim 13:1517–1536

    Google Scholar 

  • Wang W, Zhou W, Chen D (2014) Summer high temperature extremes in southeast China: bonding with the El Niño-Southern Oscillation and East Asian summer monsoon coupled system. J Clim 27:4122–4138

    Google Scholar 

  • Wu J, Gao XJ (2013) A gridded daily observation dataset over China region and comparison with the other datasets. Chin J Geophys 56:1102–1111

    Google Scholar 

  • Wu R, Hu ZZ, Kirtman BP (2003) Evolution of ENSO-Related rainfall anomalies in East Asia. J Clim 16:3742–3758

    Google Scholar 

  • Wu B, Zhou T, Li T (2017a) Atmospheric dynamic and thermodynamic processes driving the western North Pacific anomalous anticyclone during El Niño. Part I: maintenance mechanisms. J Clim 30:9623–9635

    Google Scholar 

  • Wu B, Zhou T, Li T (2017b) Atmospheric dynamic and thermodynamic processes driving the western North Pacific anomalous anticyclone during El Niño. Part II: formation processes. J Clim 30:9637–9650

    Google Scholar 

  • Xie SP, Hafner J, Tokinaga H, Du Y, Sampe T, Hu KM, Huang G (2009) Indian ocean capacitor effect on Indo-western Pacific climate during the summer following El Niño. J Clim 22:730–747

    Google Scholar 

  • Xu K, Huang QL, Tam CY, Wang W, Chen S, Zhu C (2019) Roles of tropical SST patterns during two types of ENSO in modulating wintertime rainfall over southern China. Clim Dyn 52:523–538

    Google Scholar 

  • Yang J, Liu Q, Xie SP, Liu Z, Wu L (2007) Impact of the Indian Ocean SST basin mode on the Asian summer monsoon. Geophys Res Lett 34:155–164

    Google Scholar 

  • Yeh S-W, Wang X, Wang C-Z, Dewitte B (2015) On the relationship between the North Pacific climate variability and Central Pacific El Niño. J Clim 28:663–677

    Google Scholar 

  • Yeh SW, Cai W, Min SK et al (2018) ENSO atmospheric teleconnections and their response to greenhouse gas forcing. Rev Geophys 56:185–206

    Google Scholar 

  • Yuan Y, Yang S, Zhang Z (2011) Different evolutions of the Philippine Sea anticyclone between the eastern and central Pacific El Niño: possible effects of Indian Ocean SST. J Clim 25:7867–7883

    Google Scholar 

  • Zhang R, Sumi A, Kimoto M (1996) Impact of El Niño on the East Asian monsoon: a diagnostic study of the 86/87 and 91/92 events. J Meteorol Soc Jpn 74:49–62

    Google Scholar 

  • Zhang R, Sumi A, Kimoto M (1999) A diagnostic study of the impact of El Niño on the precipitation in China. Adv Atmos Sci 16:229–241

    Google Scholar 

  • Zhang W, Jin FF, Li J, Ren HL (2011) Contrasting impacts of two-type El Niño over the eastern north Pacific during boreal autumn. J Meteorol Soc Jpn 89:563–569

    Google Scholar 

  • Zhang W, Li H, Jin FF, Stuecker MF, Turner AG, Klingaman NP (2015a) The annual-cycle modulation of meridional asymmetry in ENSO’s atmospheric response and its dependence on ENSO zonal structure. J Clim 28:5795–5812

    Google Scholar 

  • Zhang W, Chen QL, Zheng F (2015b) Bias corrections of the heat flux damping process to improve the simulation of ENSO post-2000. SOLA 11:181–185

    Google Scholar 

  • Zhang W, Li H, Stuecker MF, Jin FF, Turner AG (2016) A new understanding of El Niño’s impact over East Asia: dominance of the ENSO combination mode. J Clim 29:4347–4359

    Google Scholar 

  • Zhang W, Wang Z, Stuecker MF, Turner A, Jin F-F, Geng X (2019) Impact of ENSO longitudinal position on teleconnections to the NAO. Clim Dyn 52:257–274

    Google Scholar 

  • Zheng F, Yu J-Y (2017) Contrasting the skills and biases of deterministic predictions for the two types of El Niño. Adv Atmos Sci 34:1395–1403

    Google Scholar 

  • Zheng F, Zhu J (2010) Coupled assimilation for an intermediated coupled ENSO prediction model. Ocean Dyn 60:1061–1073

    Google Scholar 

  • Zheng F, Zhu J (2016) Improved ensemble-mean forecasting of ENSO events by a zero-mean stochastic error model of an intermediate coupled model. Clim Dyn 47:3901–3915

    Google Scholar 

  • Zheng F, Fang XH, Yu JY, Zhu J (2014) Asymmetry of the Bjerknes positive feedback between the two types of El Niño. Geophys Res Lett 41:7651–7657

    Google Scholar 

  • Zhou W, Chan JCL (2007) ENSO and the South China Sea summer monsoon onset. Int J Climatol 27:157–167

    Google Scholar 

Download references

Acknowledgements

The authors wish to thank anonymous reviewers for their very helpful comments and suggestions. This work was supported by the National Key R&D Program of China (Grant No. 2017YFA0604201) and the National Natural Science Foundation of China (Grant No. 41576019; 41876012; 41861144015).

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Zheng, F., Wang, H., Luo, H. et al. Decadal change in ENSO related seasonal precipitation over southern China under influences of ENSO and its combination mode. Clim Dyn 54, 1973–1986 (2020). https://doi.org/10.1007/s00382-019-05096-2

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