Abstract
Internally generated decadal variability influences global mean surface temperature (GMST), inducing acceleration and slowdown of the warming rate under anthropogenic radiative forcing1,2,3,4. While tropical eastern Pacific variability is important for annual-mean GMST2,5,6,7,8, the cold ocean–warm land (COWL) pattern9,10 also contributes to continental temperature variability11,12,13 in the boreal cold season. Although the two contributors are physically independent10,12, here we show that, after the mid-1980s, their decadal components vary in phase by chance to strengthen internal GMST trends, contributing to the early 2000s slowdown and early 2010s acceleration. The synchronized tropical Pacific and COWL variability explains the striking seasonality of the recent slowdown and acceleration during which the GMST trend in the boreal cold season is markedly negative and positive, respectively. Climate models cannot simulate the exact timing of the tropical Pacific and COWL correlations because they are physically independent, random-phased modes of internal variability.
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Data availability
GISTEMP is from https://data.giss.nasa.gov/gistemp/; BEST is from http://berkeleyearth.org/data/; ERA–20C and ERA–Interim are from https://apps.ecmwf.int/datasets/; CESM1 PI, HIST, POGA and GOGA runs have been obtained from the Earth System Grid (http://www.earthsystemgrid.org); CMIP5 data have been obtained from https://pcmdi.llnl.gov/?cmip5/; CM2.1 PI, HIST and POGA runs are available upon request.
Code availability
The scripts used to produce the main figures, along with the code for the CM2.1 Pacific pacemaker experiment, are available from the corresponding author upon reasonable request.
References
Trenberth, K. E. Has there been a slowdown? Science 349, 691–692 (2015).
Kosaka, Y. & Xie, S.-P. The tropical Pacific as a key pacemaker of the variable rates of global warming. Nat. Geosci. 9, 669–673 (2016).
Dong, L. & McPhaden, M. J. The role of external forcing and internal variability in regulating global mean surface temperatures on decadal timescales. Environ. Res. Lett. 12, 034011 (2017).
Chen, X. & Tung, K.-K. Global surface warming enhanced by weak Atlantic overturning circulation. Nature 559, 387–391 (2018).
Kosaka, Y. & Xie, S.-P. Recent global-warming slowdown tied to equatorial Pacific surface cooling. Nature 501, 403–407 (2013).
England, M. H. et al. Recent intensification of wind-driven circulation in the Pacific and the ongoing warming slowdown. Nat. Clim. Change 4, 222–227 (2014).
Dai, A., Fyfe, J. C., Xie, S.-P. & Dai, X. Decadal modulation of global surface temperature by internal climate variability. Nat. Clim. Change 5, 555–559 (2015).
Meehl, G. A., Hu, A., Santer, B. D. & Xie, S.-P. Contribution of the Interdecadal Pacific Oscillation to twentieth-century global surface temperature trends. Nat. Clim. Change 6, 1005–1008 (2016).
Wallace, J., Zhang, Y. & Renwick, J. Dynamic contribution to hemispheric mean temperature trends. Science 270, 780–783 (1995).
Molteni, F., Farneti, R., Kucharski, F. & Stockdale, T. N. Modulation of air–sea fluxes by extratropical planetary waves and its impact during the recent surface warming slowdown. Geophys. Res. Lett. 44, 1494–1502 (2017).
Li, C., Stevens, B. & Marotzke, J. Eurasian winter cooling in the warming slowdown of 1998–2012. Geophys. Res. Lett. 42, 8131–8139 (2015).
Deser, C., Guo, R. & Lehner, F. The relative contributions of tropical Pacific sea surface temperatures and atmospheric internal variability to the recent global warming slowdown. Geophys. Res. Lett. 44, 7945–7954 (2017).
Huang, J., Xie, Y., Guan, X., Li, D. & Ji, F. The dynamics of the warming slowdown over the Northern Hemisphere. Clim. Dynam. 48, 429–446 (2017).
Sigmond, M. & Fyfe, J. C. Tropical Pacific impacts on cooling North American winters. Nat. Clim. Change 6, 970–974 (2016).
Johnson, N. C., Xie, S.-P., Kosaka, Y. & Li, X. Increasing occurrence of cold and warm extremes during the recent global warming slowdown. Nat. Commun. 9, 1724 (2018).
Karl, T. R. et al. Possible artifacts of data biases in the recent global surface warming slowdown. Science 348, 1469–1472 (2015).
Santer, B. D. et al. Volcanic contribution to decadal changes in tropospheric temperature. Nat. Geosci. 7, 185–189 (2014).
Thompson, D., Kennedy, J., Wallace, J. & Jones, P. A large discontinuity in the mid-twentieth century in observed global-mean surface temperature. Nature 453, 646–649 (2008).
Broccoli, A. J., Lau, N. C. & Nath, M. J. The cold ocean–warm land pattern: model simulation and relevance to climate change detection. J. Clim. 11, 2743–2763 (1998).
Wang, C.-Y., Xie, S.-P., Kosaka, Y., Liu, Q. & Zheng, X.-T. Global influence of tropical Pacific variability with implications for global warming slowdown. J. Clim. 30, 2679–2695 (2017).
Zhao, P., Yang, S., Jian, M. & Chen, J. Relative controls of Asian–Pacific summer climate by Asian land and tropical–North Pacific sea surface temperature. J. Clim. 24, 4165–4188 (2011).
Mori, M., Kosaka, Y., Watanabe, M., Nakamura, H. & Kimoto, M. A reconciled estimate of the influence of Arctic sea-ice loss on recent Eurasian cooling. Nat. Clim. Change 9, 123–129 (2019).
Kay, J. E. et al. The Community Earth System Model (CESM) large ensemble project: a community resource for studying climate change in the presence of internal climate variability. Bull. Am. Meteorol. Soc. 96, 1333–1349 (2015).
Power, S., Casey, T., Folland, C., Colman, A. & Mehta, V. Interdecadal modulation of the impact of ENSO on Australia. Clim. Dynam. 15, 319–324 (1999).
Taylor, K. E., Stouffer, R. J. & Meehl, G. A. An overview of CMIP5 and the experiment design. Bull. Am. Meteorol. Soc. 93, 485–498 (2012).
Zhang, R., Delworth, T. L. & Held, I. M. Can the Atlantic Ocean drive the observed multidecadal variability in Northern Hemisphere mean temperature? Geophys. Res. Lett. 34, L02709 (2007).
Cohen, J. L., Furtado, J. C., Barlow, M., Alexeev, V. A. & Cherry, J. E. Asymmetric seasonal temperature trends. Geophys. Res. Lett. 39, L04705 (2012).
Saffioti, C., Fischer, E. M. & Knutti, R. Contributions of atmospheric circulation variability and data coverage bias to the warming slowdown. Geophys. Res. Lett. 42, 2385–2391 (2015).
Trenberth, K. E., Fasullo, J. T., Branstator, G. & Phillips, A. S. Seasonal aspects of the recent pause in surface warming. Nat. Clim. Change 4, 911–916 (2014).
Meehl, G. A., Hu, A. & Teng, H. Initialized decadal prediction for transition to positive phase of the Interdecadal Pacific Oscillation. Nat. Commun. 7, 11718 (2016).
Hansen, J., Ruedy, R., Sato, M. & Lo, K. Global surface temperature change. Rev. Geophys. 48, RG4004 (2010).
Rohde, R., Muller, R. A., Jacobsen, R., Muller, E. & Wickham, C. A new estimate of the average earth surface land temperature spanning 1753 to 2011. Geoinform. Geostat.: An Overview 1, 1000101 (2013).
Poli, P. et al. ERA–20C: an atmospheric reanalysis of the twentieth century. J. Clim. 29, 4083–4097 (2016).
Dee, D. P. et al. The ERA–Interim reanalysis: configuration and performance of the data assimilation system. Q. J. R. Meteorol. Soc. 137, 553–597 (2011).
Deser, C., Simpson, I. R., McKinnon, K. A. & Phillips, A. S. The Northern Hemisphere extratropical atmospheric circulation response to ENSO: how well do we know it and how do we evaluate models accordingly? J. Clim. 30, 5059–5082 (2017).
Smith, T. M., Reynolds, R. W., Peterson, T. C. & Lawrimore, J. Improvements to NOAA’s historical merged land–ocean surface temperature analysis (1880–2006). J. Clim. 21, 2283–2296 (2008).
Huang, B. et al. Extended reconstructed sea surface temperature version 4 (ERSST.v4): part I. Upgrades and intercomparisons. J. Clim. 28, 911–930 (2015).
Liu, W. et al. Extended reconstructed sea surface temperature version 4 (ERSST.v4): part II. Parametric and structural uncertainty estimations. J. Clim. 28, 931–951 (2015).
Huang, B. et al. Further exploring and quantifying uncertainties for Extended Reconstructed Sea Surface Temperature (ERSST) version 4 (v4). J. Clim. 29, 3119–3142 (2016).
Rayner, N. A. et al. Global analyses of sea surface temperature, sea ice, and night marine air temperature since the late nineteenth century. J. Geophys. Res. 108, 4407 (2003).
Yao, S.-L., Luo, J.-J., Huang, G. & Wang, P. Distinct global warming rates tied to multiple ocean surface temperature changes. Nat. Clim. Change 7, 486–491 (2017).
Thoma, M., Greatbatch, R. J., Kadow, C. & Gerdes, R. Decadal hindcasts initialized using observed surface wind stress: evaluation and prediction out to 2024. Geophys. Res. Lett. 42, 6454–6461 (2015).
Meehl, G. A., Hu, A., Arblaster, J. M., Fasullo, J. & Trenberth, K. E. Externally forced and internally generated decadal climate variability associated with the Interdecadal Pacific Oscillation. J. Clim. 26, 7298–7310 (2013).
Hu, S. & Fedorov, A. V. The extreme El Niño of 2015–2016 and the end of global warming hiatus. Geophys. Res. Lett. 44, 3816–3824 (2017).
Su, J., Zhang, R. & Wang, H. Consecutive record-breaking high temperatures marked the handover from hiatus to accelerated warming. Sci. Rep. 7, 43735 (2017).
Sen, P. K. Estimates of the regression coefficient based on Kendall’s tau. J. Am. Stat. Assoc. 63, 1379–1389 (1968).
Acknowledgements
X.L. was supported by the national key research and development project of China (grant no. 2016YFA0601803), the National Natural Science Foundation of China (grant nos. 41925025 and U1606402) and the Qingdao National Laboratory for Marine Science and Technology (grant no. 2017ASKJ01). J.-C.Y. was supported by the Fundamental Research Funds for the Central Universities (grant no. 202013029) and the National Natural Science Foundation of China (grant no. 41806007). Y.Z. was supported by the China Scholarship Council (grant no. 201706330016). Y.K. was supported by the Japanese Ministry of Education, Culture, Sports, Science and Technology (‘the Integrated Research Program for Advancing Climate Models’ and ‘the Arctic Challenge for Sustainability’ projects), by the Japan Society for the Promotion of Science (grant nos. 18H01278, 19H01964 and 19H05703) and by the Japan Science and Technology Agency (Belmont Forum CRA ‘InterDec’). Z.L. was supported by the National Natural Science Foundation of China (grant no. 41806007).
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J.-C.Y., X.L., S.-P.X. and Y.Z. conceived the analysis. J.-C.Y. performed the data analysis and prepared all figures. Y.K. ran CM2.1 simulations. Z.L. processed CMIP5 data. All authors wrote and reviewed the manuscript.
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Supplementary Figs. 1–10 and Table 1.
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Yang, JC., Lin, X., Xie, SP. et al. Synchronized tropical Pacific and extratropical variability during the past three decades. Nat. Clim. Chang. 10, 422–427 (2020). https://doi.org/10.1038/s41558-020-0753-9
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DOI: https://doi.org/10.1038/s41558-020-0753-9