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Modulation of the Tibetan Plateau snow cover on the interannual variations of the MJO-Related winter surface air temperature anomalies over East Asia

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Abstract

Previous studies have revealed that the Madden–Julian oscillation (MJO) can exert a profound impact on the surface air temperature (SAT) anomalies over East Asia during winter (December–February). In this study, it is found that such MJO-related winter SAT anomalies can be modulated by the interannual variability of the Tibetan Plateau snow cover (TPSC). During the excessive TPSC (ETPSC) winters, the MJO-related East Asian SAT anomalies in phase 3 are significantly colder than normal. However, during the reduced TPSC (RTPSC) winters, such SAT anomalies are close to normal. A linear baroclinic model is used to examine the possible physical mechanisms. During the ETPSC winters, the more energetic MJO can excite stronger poleward Rossby waves and intensify the upper level cyclonic anomalies over East Asia and lead to the significantly colder SAT anomalies. While during the RTPSC winters, the suppressed MJO convection excites weaker poleward Rossby waves and cannot make colder SAT anomalies over East Asia. The numerical evidences also show that the variation of the mean state could affect the teleconnections but it does not benefit a stronger Rossby wave train over East Asia in ETPSC winters. These results confirm that the TPSC can exert a profound modulation effect on the MJO teleconnection and further impact on the winter SAT anomalies over East Asia.

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References

  • Cassou C (2008) Intraseasonal interaction between the Madden–Julian oscillation and the North Atlantic oscillation. Nature 455:523–527

    Article  Google Scholar 

  • Chen G (2021) Diversity of the global teleconnections associated with the Madden–Julian Oscillation. J Clim 34:397–414

    Article  Google Scholar 

  • Cui J, Yang S, Li T (2020) The influence of the Madden-Julian oscillation on high-latitude surface air temperature during boreal winter. Dyn Atmos Oceans 90:101141

    Article  Google Scholar 

  • He J, Lin H, Wu Z (2011) Another look at influences of the Madden–Julian oscillation on the wintertime East Asian weather. J Geophys Res Atmos 116:D03109

    Article  Google Scholar 

  • Hendon HH, Salby ML (1994) The life cycle of the Madden–Julian oscillation. J Atmos Sci 51:2225–2237

    Article  Google Scholar 

  • Hu W, Liu P, Zhang Q, He B (2019) Dominant patterns of winter-time intraseasonal surface air temperature over the CONUS in response to MJO convections. Clim Dyn 53:3917–3936

    Article  Google Scholar 

  • Huang Y, Qian Y (2007) Analysis of the simulated climatic characters of the South Asia High with a flexible coupled ocean–atmosphere GCM. Adv Atmos Sci 24:136–146

    Article  Google Scholar 

  • Jin F, Hoskins BJ (1995) The direct response to tropical heating in a baroclinic atmosphere. J Atmos Sci 52:307–319

    Article  Google Scholar 

  • Kikuchi K, Wang B, Kajikawa Y (2011) Bimodal representation of the tropical intraseasonal oscillation. Clim Dyn 38:1–12

    Google Scholar 

  • Kim H, Son SW, Yoo C (2020) QBO modulation of the MJO-related precipitation in East Asia. J Geophys Res Atmos 125:e2019JD031929

    Article  Google Scholar 

  • L’Heureux ML, Higgins RW (2008) Boreal winter links between the Madden–Julian oscillation and the Arctic oscillation. J Clim 21:3040–3050

    Article  Google Scholar 

  • Lee J et al (2013) Real-time multivariate indices for the boreal summer intraseasonal oscillation over the Asian summer monsoon region. Clim Dyn 40:493–509

    Article  Google Scholar 

  • Li C, Long Z, Zhang Q (2001) Strong/weak summer monsoon activity over the South China Sea and atmospheric intraseasonal oscillation. Adv Atmos Sci 18:1146–1160

    Article  Google Scholar 

  • Lin H, Wu Z (2011) Contribution of the autumn Tibetan Plateau snow cover to seasonal prediction of North American winter temperature. J Clim 24:2801–2813

    Article  Google Scholar 

  • Lin H, Brunet G, Derome J (2009) An observed connection between the North Atlantic Oscillation and the Madden-Julian Oscillation. J Clim 22:364–380

    Article  Google Scholar 

  • Liu F, Wang B, Ouyang Y, Wang H, Qiao S, Chen G, Dong W (2022) Intraseasonal variability of global land monsoon precipitation and its recent trend. NPJ Clim Atmos Sci 5:30. https://doi.org/10.1038/s41612-022-00253-7

    Article  Google Scholar 

  • Lyu M, Wen M, Wu Z (2018) Possible contribution of the inter-annual Tibetan Plateau snow cover variation to the Madden–Julian oscillation convection variability. Int J Climatol 38:3787–3800

    Article  Google Scholar 

  • Madden R, Julian P (1971) Detection of a 40–50 day oscillation in the zonal wind in the tropical Pacific. J Atmos Sci 28:702–708

    Article  Google Scholar 

  • Madden R, Julian P (1972) Description of global-scale circulation cells in the tropics with a 40–50 day period. J Atmos Sci 29:1109–1123

    Article  Google Scholar 

  • Qian Y, Zhang Q, Yao Y, Zhang X (2002) Seasonal variation and heat preference of the South Asia High. Adv Atmos Sci 19:821–836

    Article  Google Scholar 

  • Seo KH, Son SW (2012) The global atmospheric circulation response to tropical diabatic heating associated with the Madden–Julian oscillation during northern winter. J Atmos Sci 69:79–96

    Article  Google Scholar 

  • Seo KH, Lee HJ, Frierson DMW (2016) Unraveling the teleconnection mechanisms that induce wintertime temperature anomalies over the Northern Hemisphere continents in response to the MJO. J Atmos Sci 73:3557–3571

    Article  Google Scholar 

  • Sobel AH, Maloney ED (2000) Effect of ENSO and the MJO on Western North Pacific tropical cyclones. Geophys Res Lett 27:1739–1742

    Article  Google Scholar 

  • Song L, Wu R (2020) Distinct Eurasian climate anomalies associated with strong and weak MJO events. Int J Climatol 40:6666–6674

    Article  Google Scholar 

  • Stan C, Straus DM, Frederiksen JS, Lin H, Maloney ED, Schumacher C (2017) Review of tropical-extratropical teleconnections on intraseasonal time scales. Rev Geophys 55:902–937

    Article  Google Scholar 

  • 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 58:608–627

    Article  Google Scholar 

  • Tseng K-C, Maloney ED, Barnes EA (2019) The consistency of MJO teleconnection patterns: an explanation using linear Rossby wave theory. J Clim 32:531–548

    Article  Google Scholar 

  • Vitart F, Molteni F (2010) Simulation of the Madden–Julian Oscillation and its teleconnections in the ECMWF forecast system. Q J R Meteorol Soc 136:842–855

    Article  Google Scholar 

  • Wang B, Rui H (1990) Dynamics of the coupled moist Kelvin– Rossby wave on an equatorial b-plane. J Atmos Sci 47:397–413

    Article  Google Scholar 

  • Wheeler MC, Hendon HH (2004) An all-season real-time multivariate MJO index: development of an index for monitoring and prediction. Mon Weather Rev 132:1917–1932

    Article  Google Scholar 

  • Yanai M, Esbensen S, Chu J (1973) Determination of bulk properties of tropical cloud clusters from large-scale heat and moisture budgets. J Atmos Sci 30:611–627

    Article  Google Scholar 

  • Zhang C (2013) Madden–Julian oscillation: bridging weather and climate. Bull Am Meteorol Soc 94:1849–1870

    Article  Google Scholar 

  • Zhou W, Yang D, Xie S, Ma J (2021) Amplified Madden-Julian oscillation impacts in the Pacific-North America region. Nat Clim Change 10:1–7

    Google Scholar 

Download references

Acknowledgements

This research was jointly supported by National Natural Science Foundation of China (NSFC) Major Research Plan on West-Pacific Earth System Multi-spheric Interactions (project number: 92158203), the Second Tibetan Plateau Scientific Expedition and Research (STEP) program (Grant No. 2019QZKK0102) and NSFC (Grant Nos. 91937302 and 41790475).

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Correspondence to Zhiwei Wu.

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Cao, C., Wu, Z. Modulation of the Tibetan Plateau snow cover on the interannual variations of the MJO-Related winter surface air temperature anomalies over East Asia. Clim Dyn 59, 3427–3437 (2022). https://doi.org/10.1007/s00382-022-06275-4

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  • DOI: https://doi.org/10.1007/s00382-022-06275-4

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