Abstract
The Madden–Julian oscillation (MJO) produces a region of enhanced precipitation that travels eastwards along the Equator in a 40–50 day cycle, perturbing tropical and high-latitude winds, and thereby modulating extreme weather events such as flooding, hurricanes and heat waves. Here, we synthesize current understanding on projected changes in the MJO under anthropogenic warming, demonstrating that MJO-related precipitation variations are likely to increase in intensity, whereas wind variations are likely to increase at a slower rate or even decrease. Nevertheless, future work should address uncertainties in the amplitude of precipitation and wind changes and the impacts of projected SST patterns, with the aim of improving predictions of the MJO and its associated extreme weather.
This is a preview of subscription content, access via your institution
Relevant articles
Open Access articles citing this article.
-
Climate-driven changes in the predictability of seasonal precipitation
Nature Communications Open Access 28 June 2023
-
Emergence of Madden-Julian oscillation precipitation and wind amplitude changes in a warming climate
npj Climate and Atmospheric Science Open Access 23 March 2023
-
On the future zonal contrasts of equatorial Pacific climate: Perspectives from Observations, Simulations, and Theories
npj Climate and Atmospheric Science Open Access 31 October 2022
Access options
Access Nature and 54 other Nature Portfolio journals
Get Nature+, our best-value online-access subscription
$29.99 / 30 days
cancel any time
Subscribe to this journal
Receive 12 print issues and online access
$209.00 per year
only $17.42 per issue
Rent or buy this article
Prices vary by article type
from$1.95
to$39.95
Prices may be subject to local taxes which are calculated during checkout





References
Madden, R. & Julian, P. R. in Intraseasonal Variability in the Atmosphere–Ocean Climate System (eds Lau, K. M. & Waliser, D. E.) Ch. 1 (Praxis, Springer, Berlin, 2005).
Maloney, E. D. & Hartmann, D. L. Modulation of eastern north Pacific hurricanes by the Madden-Julian oscillation. J. Clim. 13, 1451–1460 (2000).
Klotzbach, P. J. & Oliver, E. C. J. Modulation of Atlantic basin tropical cyclone activity by the Madden-Julian Oscillation (MJO) from 1905–2011. J. Clim. 28, 204–217 (2015).
McPhaden, M. J. Genesis and evolution of the 1997–98 El Niño. Science 283, 950–954 (1999).
Moore, A. M. & Kleeman, R. Stochastic forcing of ENSO by the intraseasonal oscillation. J. Clim. 12, 1199–1220 (1999).
Lin, H., Brunet, G. & Derome, J. An observed connection between the North Atlantic Oscillation and the Madden–Julian oscillation. J. Clim. 22, 364–380 (2009).
Zhang, C. Madden-Julian oscillation: bridging weather and climate. Bull. Am. Meteorol. Soc. 94, 1849–1870 (2013).
Guan, B., Waliser, D. E., Molotch, N. P., Fetzer, E. J. & Neiman, P. J. Does the Madden-Julian oscillation influence wintertime atmospheric rivers and snowpack in the Sierra Nevada? Mon. Weather Rev. 140, 325–342 (2012).
Ralph, F. M. & Dettinger, M. D. Historical and national perspectives on extreme West Coast precipitation associated with atmospheric rivers during December 2010. Bull. Am. Meteorol. Soc. 93, 783–790 (2012).
Mundhenk, B. D., Barnes, E. A., Maloney, E. D. & Baggett, C. F. Skillful subseasonal prediction of atmospheric river activity based on the Madden Julian oscillation and the Quasi-Biennial oscillation. npj Clim. Atmos. Sci 1, 20177 (2018).
Baggett, C. F., Barnes, E. A., Maloney, E. D. & Mundhenk, B. D. Advancing atmospheric river forecasts into subseasonal timescales. Geophys. Res. Lett. 44, 7528–7536 (2017).
Arnold, N. P., Branson, M., Kuang, Z., Randall, D. A. & Tziperman, E. MJO intensification with warming in the superparameterized CESM. J. Clim. 28, 2706–2724 (2015). This study used a gold standard model to demonstrate stronger MJO precipitation variability in a 4×CO 2 climate and features a detailed process oriented diagnosis that highlights the importance of an increased vertical moisture gradient.
Hand, E. The storm king. Science 350, 22–25 (2015).
Wolding, B. O., Maloney, E. D., Henderson, S. A. & Branson, M. Climate change and the Madden-Julianoscillation: a vertically resolved weak temperature gradient analysis 307-331. J. Adv. Model. Earth Syst. 9, 307–331 (2017). This modelling study provided a process-level diagnosis of the MJO in a 4×CO 2 climate through novel use of the moisture budget, and documented a potential weakening of MJO teleconnections to higher latitudes in a warmer climate.
Adames, A. ́F. & Kim, D. The MJO as a dispersive, convectively coupled moisture wave: theory and observations. J. Atmos. Sci. 73, 913–941 (2016).
Slingo, J. M., Rowell, D. P., Sperber, K. R. & Nortley, F. On the predictability of the interannual behaviour of the Madden‐Julian oscillation and its relationship with El Nino. Q. J. R. Meteorol. Soc. 125, 583–609 (1999).
Jones, C. & Carvalho, L. M. V. Changes in the activity of the Madden–Julian oscillation during 1958–2004. J. Clim. 19, 6353–6370 (2006).
Lee, S.‐H. & Seo, K.-H. A multi‐scale analysis of the interdecadal change in the Madden–Julian Oscillation, Atmos. Korean Meteorol. 21, 143–149 (2011).
Oliver, E. C. & Thompson, K. R. A reconstruction of Madden–Julian Oscillation variability from 1905 to 2008. J. Clim. 25, 1996–2019 (2012).
Tao, L., Zhao, J. & Li, T. Trend analysis of tropical intraseasonal oscillations in the summer and winter during 1982–2009. Int. J. Climatol. 35, 3969–3978 (2015).
Yoo, C., Feldstein, S. & Lee, S. The impact of the Madden‐Julian oscillation trend on the Arctic amplification of surface air temperature during the 1979–2008 boreal winter. Geophys. Res. Lett. 38, L24804 (2011).
Pohl, B. & Matthews, A. J. Observed changes in the lifetime and amplitude of the Madden–Julian oscillation associated with interannual ENSO sea surface temperature anomalies. J. Clim. 20, 2659–2674 (2007).
Schubert, J. J., Stevens, B. & Crueger, T. Madden‐Julian oscillation as simulated by the Max Planck Institute for Meteorology Earth System Model: Over the last and into the next millennium. J. Adv. Model. Earth Syst. 5, 71–84 (2013).
Jones, C. & Carvalho, L. M. V. Will global warming modify the activity of the Madden–Julian oscillation? Q. J. R. Meteorol. Soc. 137, 544–552 (2010).
Xie, S.‐P. et al. Global warming pattern formation: Sea surface temperature and rainfall. J. Clim. 23, 966–986 (2010).
Benedict, J. J., Maloney, E. D., Sobel, A. H. & Frierson, D. M. Gross moist stability and MJO simulation skill in three full-physics GCMs. J. Atmos. Sci. 71, 3327–3349 (2014).
Raymond, D. J., Sessions, S. L., Sobel, A. H. & Fuchs, Z. The mechanics of gross moist stability. J. Adv. Model. Earth Syst. 1, 9 (2009).
Hannah, W. M. & Maloney, E. D. The moist static energy budget in NCAR CAM5 hindcasts during DYNAMO. J. Adv. Model. Earth Syst. 6, 420–440 (2014).
Maloney, E. D. & Xie, S.-P. Sensitivity of MJO activity to the pattern of climate warming. J. Adv. Model. Earth Syst. 5, 32–47 (2013). This modelling study explains why MJO wind variability may change at a different rate than precipitation variability with warming, and showed that changes in MJO amplitude depend strongly on the pattern of SST change.
Arnold, N. P., Kuang, Z. & Tziperman, E. Enhanced MJO-like variability at high SST. J. Clim. 26, 988–1001 (2013).
Takahashi, C., Sato, N., Seiki, A., Yoneyama, K. & Shirooka, R. Projected future change of MJO and its extratropical teleconnection in East Asia during the northern winter simulated in IPCC AR4 models. SOLA 7, 201–204 (2011). A comprehensive study that used a multimodel suite to demonstrate a wide spread in the strength of MJO convection changes in a warming climate that is dependent on the pattern of SST change.
Hendon, H. H., Zhang, C. & Glick, J. D. Interannual variation of the Madden–Julian oscillation during austral summer. J. Clim. 12, 2538–2550 (1999).
Hendon, H. H., Wheeler, M. C. & Zhang, C. Seasonal dependence of the MJO–ENSO relationship. J. Clim. 20, 531–543 (2007).
Yoo, C. & Son, S. W. Modulation of the boreal wintertime Madden‐Julian oscillation by the stratospheric quasi‐biennial oscillation. Geophys. Res. Lett. 43, 1392–1398 (2016).
Nishimoto, E. & Yoden, S. Influence of the stratospheric quasi-biennial oscillation on the Madden-Julian oscillation during Austral summer. J. Atmos. Sci. 74, 1105–1125 (2017).
Son, S., Lim, Y., Yoo, C., Hendon, H. & Kim, J. Stratospheric control of Madden-Julian oscillation. J. Clim. 30, 1909–1922 (2017).
Zveryaev, I. I. Interdecadal changes in the zonal wind and the intensity of intraseasonal oscillations during boreal summer Asian monsoon. Tellus A 54, 288–298 (2002).
Meehl, G. A. et al. The WCRP CMIP3 multimodel dataset: a new era in climate change research. Bull. Am. Meteorol. Soc. 88, 1383–1394 (2007).
Adames, Á. F., Kim, D., Sobel, A. H., Del Genio, A. & Wu, J. Changes in the structure and propagation ofthe MJO with increasing CO2. J. Adv. Model. Earth Syst. 9, 1251–1268 (2017). Comprehensive model analysis of changes to MJO characteristics in a warmer climate, including not only amplitude changes, but also propagation speed, period and relationship to background intraseasonal variability.
Chang, C.‐W. J., Tseng, W.-L., Hsu, H.-H., Keenlyside, N. & Tsuang, B. J. The Madden‐Julian Oscillation in a warmer world. Geophys. Res. Lett. 42, 6034–6042 (2015).
Held, I. M. & Soden, B. J. Robust responses of the hydrological cycle to global warming. J. Clim. 19, 5686–5699 (2006).
Liu, P. Changes in a modeled MJO with idealized global warming. Clim. Dynam. 40, 761–773 (2013).
Liu, P. et al. MJO change with A1B global warming estimated by the 40-km ECHAM5. Clim. Dynam. 41, 1009–1023 (2013).
Bui, H. X. & Maloney, E. D. Changes in Madden-Julian Oscillation precipitation and wind variance under global warming. Geophys. Res. Lett. 45, 7148–7155 (2018).
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).
Henderson, S. A., Maloney, E. D. & Son, S. W. Madden-Julian oscillation teleconnections: the impact of the basic state and MJO representation in general circulation models. J. Clim. 30, 4567–4587 (2017).
Lee, S. Why are the climatological zonal winds easterly in the equatorial upper troposphere? J. Atmos. Sci. 56, 1353–1363 (1999).
Suarez, M. J. & Duffy, D. G. Terrestrial superrotation: A bifurcation of the general circulation. J. Atmos. Sci. 49, 1541–1554 (1992).
Caballero, R. & Huber, M. Spontaneous transition to superrotation in warm climates simulated by CAM3. Geophys. Res. Lett. 37, L11701 (2010).
Arnold, N. P. et al. The effects of explicit atmospheric convection at high CO2. Proc. Natl Acad. Sci. USA 111, 10943–10948 (2014).
Carlson, H. & Caballero, R. Enhanced MJO and transition to superrotation in warm climates. J. Adv. Model. Earth Syst. 8, 304–318 (2016). This modelling study highlights the transition to superrotation in a warmer climate and presents a novel hypothesis for how this transition supports a stronger MJO.
Pritchard, M. S. & Yang, D. Response of the superparameterized Madden‐Julian Oscillation to extreme climate and basic state variation challenges a moisture mode view. J. Clim. 29, 4995–5008 (2016).
Subramanian, A. et al. The MJO and global warming: a study in CCSM4. Clim. Dynam. 42, 2019–2031 (2014).
Kang, W. & Tziperman, E. More frequent sudden stratospheric warming events due to enhanced MJO forcing expected in a warmer climate. J. Clim. 30, 8727–8743 (2017).
Randall, D., Khairoutdinov, M., Arakawa, A. & Grabowski, W. Breaking the cloud parameterization deadlock. Bull. Am. Meteorol. Soc. 84, 1547–1564 (2003).
Zelinka, M. D. & Hartmann, D. L. Why is longwave cloud feedback positive? J. Geophys. Res. 115, D16117 (2010).
Song, E.‐J. & Seo, K.-H. Past‐ and present‐day Madden‐Julian Oscillation in CNRM‐CM5. Geophys. Res. Lett. 43, 4042–4048 (2016).
Sobel, A. H. & Bretherton, C. S. Modeling tropical precipitation in a single column. J. Clim. 13, 4378–4392 (2000).
Holloway, C. E. & Neelin, J. D. Moisture vertical structure, column water vapor, and tropical deep convection. J. Atmos. Sci. 66, 1665–1683 (2009).
Adames, Á. F., Kim, D., Sobel, A. H., Del Genio, A. & Wu, J. Characterization of moist processes associated with changes in the propagation of the MJO with increasing CO2. J. Adv. Model. Earth Syst. 9, 2946–2967 (2017).This modelling study presents a detailed process-oriented diagnosis of changes in MJO amplitude and propagation speed in a warmer climate in the context of modern theory.
Chikira, M. Eastward‐propagating intraseasonal oscillation represented by Chikira–Sugiyama cumulus parameterization. Part II: understanding moisture variation under weak temperature gradient balance. J. Atmos. Sci. 71, 615–639 (2014).
Wolding, B. O., Maloney, E. D. & Branson, M. Vertically resolved weak temperature gradient analysis of the Madden-Julian oscillation in SP-CESM. J. Adv. Model. Earth. Syst. 8, 1586–1619 (2016).
Maloney, E. D. The moist static energy budget of a composite tropical intraseasonal oscillation in a climate model. J. Clim. 22, 711–729 (2009).
Sardeshmukh, P. D. & Hoskins, B. J. The generation of global rotational flow by steady idealized tropical divergence. J. Atmos. Sci. 45, 1228–1251 (1988).
Hoskins, B. J. & Karoly, D. J. The steady linear response of a spherical atmosphere to thermal and orographic forcing. J. Atmos. Sci. 38, 1179–1196 (1981).
Coats, S. & Karnauskas, K. B. Are simulated and observed twentieth century tropical Pacific sea surface temperature trends significant relative to internal variability? Geophys. Res. Lett. 44, 9928–9937 (2017).
Eyring, V. et al. Overview of the Coupled Model Intercomparison Project Phase 6 (CMIP6) experimental design and organization. Geosci. Model Dev. 9, 1937–1958 (2016).
Neelin, J. D., Langenbrunner, B., Meyerson, J. E., Hall, A. & Berg, N. California winter precipitation change under global warming in the Coupled Model Intercomparison Project 5 ensemble. J. Clim. 26, 6238–6256 (2013).
Raymond, D. J. A new model of the Madden–Julian oscillation. J. Atmos. Sci. 58, 2807–2819 (2001).
Sobel, A. H. & Maloney, E. D. An idealized semi-empirical framework for modeling the Madden–Julian oscillation. J. Atmos. Sci. 69, 1691–1705 (2012).
Allen, M. R. & Ingram, W. J. Constraints on future changes in climate and the hydrologic cycle. Nature 419, 224–228 (2002).
Deser, C. & Phillips, A. S. Atmospheric circulation trends, 1950–2000: The relative roles of sea surface temperature forcing and direct atmospheric radiative forcing. J. Clim. 22, 396–413 (2009).
Bony, S. et al. Thermodynamic control of anvil-cloud amount. Proc. Natl Acad. Sci. USA 113, 8927–8932 (2016).
Acknowledgements
We thank H. Liu and the Lamont-Doherty Earth Observatory for providing the CMIP5 data, and the World Climate Research Programme’s Working Group on Coupled Modelling, which is responsible for CMIP. E.D.M. and H.X.B. were supported by the National Science Foundation under grant no. AGS-1441916, and the NOAA MAPP program under grant nos NA15OAR4310098 and NA15OAR4310099.
Author information
Authors and Affiliations
Contributions
H.X.B. generated Figs. 1–4, and contributed to the writing and editing of the manuscript. A.F.A. contributed to the writing and editing of the manuscript, and generated Fig. 5. E.D.M. led the organization and drafting of the manuscript.
Corresponding author
Ethics declarations
Competing interests
The authors declare no competing interests.
Additional information
Publisher’s note: Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
Rights and permissions
About this article
Cite this article
Maloney, E.D., Adames, Á.F. & Bui, H.X. Madden–Julian oscillation changes under anthropogenic warming. Nature Clim Change 9, 26–33 (2019). https://doi.org/10.1038/s41558-018-0331-6
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1038/s41558-018-0331-6
This article is cited by
-
Emergence of Madden-Julian oscillation precipitation and wind amplitude changes in a warming climate
npj Climate and Atmospheric Science (2023)
-
Climate-driven changes in the predictability of seasonal precipitation
Nature Communications (2023)
-
Projected future changes in equatorial wave spectrum in CMIP6
Climate Dynamics (2023)
-
Madden–Julian Oscillation-induced extreme rainfalls constrained by global warming mitigation
npj Climate and Atmospheric Science (2022)
-
On the future zonal contrasts of equatorial Pacific climate: Perspectives from Observations, Simulations, and Theories
npj Climate and Atmospheric Science (2022)