ENSO Change in Climate Projections: Forced Response or Internal Variability?
Open accessAbstract
Two large ensembles are used to quantify the extent to which internal variability can contribute to long‐term changes in El Niño‐Southern Oscillation (ENSO) characteristics. We diagnose changes that are externally forced and distinguish between multi‐model simulation results that differ by chance and those that differ due to different model physics. The range of simulated ENSO amplitude changes in the large ensemble historical simulations encompasses 90% of the Coupled Model Intercomparison Project 5 historical simulations and 80% of moderate (RCP4.5) and strong (RCP8.5) warming scenarios. When considering projected ENSO pattern changes, model differences are also important. We find that ENSO has high internal variability and that single realizations of a model can produce very different results to the ensemble mean response. Due to this variability, 30–40 ensemble members of a single model are needed to robustly compute absolute ENSO variance to a 10% error when 30‐year analysis periods are used.
The claims and statistics of this paper haven’t been checked yet.
Run the check — free, no account needed. It reads the open-access text and checks the sources it cites.
Integrity signals
Registry
Cites
Statistics
Claims the paper makes
The claims and statistics of this paper haven’t been checked yet.
Run the check — free, no account needed. It reads the open-access text and checks the sources it cites.
Claims other papers make about this one
Each is checked against this paper’s own text: does it say what the citing paper says it does?
Sampling ENSO SST variability over relatively short 30-year running periods is subject to a strong influence from decadal climate fluctuations such that stochastic noise and butterfly effect can obscure the impact of greenhouse forcing.
“However, sampling ENSO SST variability over relatively short 30-year running periods would be subject to a strong influence from decadal climate fluctuations such that stochastic noise and butterfly effect can obscure the impact of greenhouse forcing [14][15][16] .”
From Increased ENSO sea surface temperature variability under four IPCC emission scenarios (2022) · cites this paper as [14]
Self-check
Percentages, sums and reported differences re-computed from the paper’s own numbers.
The self-check needs the paper’s full text.
Cites
Cai, W., Santoso, A., Wang, G., Yeh, S.-W., An, S.-I., Cobb, K. M., Collins, M., Guilyardi, E., Jin, F.-F., Kug, J.-S., et al. (2015) · Nature Climate Change · doi:10.1038/nclimate2743 · Cited by 891 · see citing works
Interdecadal modulation of El Niño amplitude during the past millennium
Li, J., Xie, S.-P., Cook, E. R., Huang, G., D'Arrigo, R., Liu, F., Ma, J., & Zheng, X.-T. (2011) · Nature Climate Change · doi:10.1038/nclimate1086 · Cited by 349 · see citing works
Flagged first, then by citations
Research works printed but not linked: 38
- Bellenger, H., Guilyardi, E., Leloup, J., Lengaigne, M., & Vialard, J. (2014). ENSO representation in climate models: From CMIP3 to CMIP5. Climate Dynamics, 42(7-8), 1999-2018. https://doi.org/10.1007/s00382-013-1783-z · DOI
- Bittner, M., Schmidt, H., Timmreck, C., & Sienz, F. (2016). Using a large ensemble of simulations to assess the Northern Hemisphere stratospheric dynamical response to tropical volcanic eruptions and its uncertainty. Geophysical Research Letters, 43, 9324-9332. https://doi.org/10.1002/2016GL070587 · DOI
- Bjerknes, J. (1969). Atmospheric teleconnections from the equatorial Pacific. Monthly Weather Review, 97, 163-172.
- Burgman, R. J., Schopf, P. S., & Kirtman, B. P. (2008). Decadal modulation of ENSO in a hybrid coupled model. Journal of Climate, 21(21), 5482-5500. https://doi.org/10.1175/2008JCLI1933. · DOI
- Cai, W., Borlace, S., Lengaigne, M., van Rensch, P., Collins, M., Vecchi, G., et al. (2014). Increasing frequency of extreme El Niño events due to greenhouse warming. Nature Climate Change, 4(2), 111-116. https://doi.org/10.1038/nclimate2100 · DOI · Paper page
- Chowdary, J. S., Xie, S.-P., Tokinaga, H., Okumura, Y. M., Kubota, H., Johnson, N., & Zheng, X.-T. (2012). Interdecadal variations in ENSO teleconnection to the Indo-western pacific for 1870-2007. Journal of Climate, 25(5), 1722-1744. https://doi.org/10.1175/JCLI-D-11-00070. · DOI
- Christensen, J. H., Krishna Kumar, K., Aldrian, E., An, S.-I., Cavalcanti, I. F. A., de Castro, M., et al. (2013). Climate Phenomena and their Rele- vance for Future Regional Climate Change. In T. F. Stocker, et al. (Eds.), Climate Change 2013: The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge, United Kingdom and New York, NY: Cambridge University Press.
- Chung, C. T. Y., & Power, S. B. (2016). Modelled impact of global warming on ENSO-driven precipitation changes in the tropical Pacific. Climate Dynamics, 47(3-4), 1303-1323. https://doi.org/10.1007/s00382-015-2902-9 · DOI
- Collins, M., An, S.-I., Cai, W., Ganachaud, A., Guilyardi, E., Jin, F.-F., et al. (2010). The impact of global warming on the tropical Pacific Ocean and El Niño. Nature Geoscience, 3(6), 391-397. https://doi.org/10.1038/ngeo868 · DOI · Paper page
- Deser, C., Phillips, A., Bourdette, V., & Teng, H. (2012). Uncertainty in climate change projections: The role of internal variability. Climate Dynamics, 38(3-4), 527-546. https://doi.org/10.1007/s00382-010-0977-x · DOI
- Frankcombe, L. M., England, M. H., Mann, M. E., & Steinman, B. A. (2015). Separating internal variability from the externally forced climate response. Journal of Climate, 28(20), 8184-8202. https://doi.org/10.1175/JCLI-D-15-0069. · DOI
- Guilyardi, E., Bellenger, H., Collins, M., Ferrett, S., Cai, W., & Wittenberg, A. (2012). A first look at ENSO in CMIP5. CLIVAR Exchanges, 17(58), 29-32.
- Guilyardi, E., Braconnot, P., Jin, F.-F., Kim, S. T., Kolasinski, M., Li, T., & Musat, I. (2009). Atmosphere feedbacks during ENSO in a coupled GCM with a modified atmospheric convection scheme. Journal of Climate, 22(21), 5698-5718. https://doi.org/10.1175/2009JCLI2815. · DOI
- Ham, Y.-G., & Kug, J.-S. (2016). ENSO amplitude changes due to greenhouse warming in CMIP5: Role of mean tropical precipitation in the twentieth century. Geophysical Research Letters, 43, 422-430. https://doi.org/10.1002/2015GL066864 · DOI
- Hawkins, E., & Sutton, R. (2009). Decadal predictability of the Atlantic Ocean in a coupled GCM: Forecast skill and optimal perturbations using linear inverse modeling. Journal of Climate, 22(14), 3960-3978. https://doi.org/10.1175/2009JCLI2720. · DOI
- Hawkins, E., & Sutton, R. (2012). Time of emergence of climate signals. Geophysical Research Letters, 39, L01702. https://doi.org/10.1029/2011GL050087 · DOI
- Jungclaus, J. H., Fischer, N., Haak, H., Lohmann, K., Marotzke, J., Matei, D., et al. (2013). Characteristics of the ocean simulations in the Max Planck Institute Ocean Model (MPIOM) the ocean component of the MPI-Earth system model. Journal of Advancesd Modelling of the Earth System, 5, 422-446. https://doi.org/10.1002/jame.20023 · DOI
- Kay, J. E., Deser, C., Phillips, A., Mai, A., Hannay, C., Strand, G., et al. (2015). The Community Earth System Model (CESM) large ensemble project: A community resource for studying climate change in the presence of internal climate variability. Bulletin of American Meteorological Society, 96(8), 1333-1349. https://doi.org/10.1175/BAMS-D-13-00255. · DOI
- Keupp, L., Pollinger, F., & Paeth, H. (2017). Assessment of future ENSO changes in a CMIP3/CMIP5 multi-model and multi-index framework. International Journal of Climatology, 37(8), 3439-3451. https://doi.org/10.1002/joc.4928 · DOI
- Kim, S. T., Cai, W., Jin, F.-F., Santoso, A., Wu, L., Guilyardi, E., & An, S.-I. (2014). Response of El Niño sea surface temperature variability to greenhouse warming. Nature Climate Change, 4(9), 786-790. https://doi.org/10.1038/nclimate2326 · DOI
- Maher, N., McGregor, S., England, M. H., & Alexander, S. (2015). Effects of volcanism on tropical variability. Geophysical Research Letters, 42, 6024-6033. https://doi.org/10.1002/2015GL064751 10.1029/2018GL079764 · DOI
- Marotzke, J., & Forster, P. M. (2015). Forcing, feedback and internal variability in global temperature trends. Nature, 517(7536), 565-570. https://doi.org/10.1038/nature14117 · DOI
- Ogata, T., Xie, S.-P., Wittenberg, A., & Sun, D.-Z. (2013). Interdecadal amplitude modulation of El Niño-Southern Oscillation and its impact on tropical Pacific decadal variability. Journal of Climate, 26(18), 7280-7297. https://doi.org/10.1175/JCLI-D-12-00415. · DOI
- Power, S., Delage, F., Chung, C., Kociuba, G., & Keay, K. (2013). Robust twenty-first-century projections of El Niño and related precipitation variability. Nature, 502(7472), 541-545. https://doi.org/10.1038/nature12580 · DOI · Paper page
- Power, S. B., Delage, F. P. D., Chung, C. T. Y., Ye, H., & Murphy, B. F. (2017). Humans have already increased the risk of major disruptions to Pacific rainfall. Nature Communications, 8(14), 368. https://doi.org/10.1038/ncomms14368 · DOI
- Rashid, H. A., Hirst, A. C., & Marsland, S. J. (2016). An atmospheric mechanism for ENSO amplitude changes under an abrupt quadrupling of CO2 concentration in CMIP5 models. Geophysical Research Letters, 43, 1687-1694. https://doi.org/10.1002/2015GL066768 · DOI
- Rayner, N. A. (2003). Global analyses of sea surface temperature, sea ice, and night marine air temperature since the late nineteenth century. Journal of Geophysical Research, 108(D14), 4407. https://doi.org/10.1029/2002JD002670 · DOI
- Sanderson, B. M., Oleson, K. W., Strand, W. G., Lehner, F., & O'Neill, B. C. (2015). A new ensemble of GCM simulations to assess avoided impacts in a climate mitigation scenario. Climatic Change, 146(3), 303-318. https://doi.org/10.1007/s10584-015-1567-z · DOI
- Smith, T. M., Reynolds, R. W., Peterson, T. C., & Lawrimore, J. (2008). Improvements to NOAA's historical merged land-ocean surface temperature analysis (1880-2006). Journal of Climate, 21(10), 2283-2296. https://doi.org/10.1175/2007JCLI2100. · DOI
- Stevens, B. (2015). Rethinking the lower bound on aerosol radiative forcing. Journal of Climate, 28(12), 4794-4819. https://doi.org/10.1175/JCLI-D-14-00656. · DOI
- Stevenson, S. L. (2012). Significant changes to ENSO strength and impacts in the twenty-first century: Results from CMIP5. Geophysical Research Letters, 39, L17703. https://doi.org/10.1029/2012GL052759 · DOI
- Sun, C., Liu, L., Li, L.-J., Wang, B., Zhang, C., Liu, Q., & Li, R.-Z. (2018). Uncertainties in simulated El Niño-Southern Oscillation arising from internal climate variability. Atmospheric Science Letters, 19(3), e805. https://doi.org/10.1002/asl.805 · DOI
- Takahashi, K., Montecinos, A., Goubanova, K., & Dewitte, B. (2011). ENSO regimes: Reinterpreting the canonical and Modoki El Niño. Geophysical Research Letters, 38, L10704. https://doi.org/10.1029/2011GL047364 · DOI
- Timmermann, A. (1999). Detecting the nonstationary response of ENSO to greenhouse warming. Journal of Atmospheric Science, 56(14), 2313-2325. https://doi.org/10.1175/1520-0469(1999)056<2313:DTNROE>2.0.CO;2 · DOI
- Wittenberg, A. T. (2009). Are historical records sufficient to constrain ENSO simulations? Geophysical Research Letters, 36, L12702. https://doi.org/10.1029/2009GL038710 · DOI
- Zebiak, S., & Cane, M. (1987). A model El Niño-Southern Oscillation. Monthly Weather Review, 97(3), 163-172.
- Zelle, H., Jan van Oldenborgh, G., Burgers, G., & Dijkstra, H. (2005). El Niño and greenhouse warming: Results from ensemble simulations with the NCAR CCSM. Journal of Climate, 18(22), 4669-4683. https://doi.org/10.1175/JCLI3574. · DOI
- Zheng, X.-T., Hui, C., & Yeh, S.-W. (2018). Response of ENSO amplitude to global warming in CESM large ensemble: Uncertainty due to internal variability. Climate Dynamics, 50, 4019. https://doi.org/10.1007/s00382-017-3859-7 · DOI · Paper page
Cited by
Sorted by citations
Increased ENSO sea surface temperature variability under four IPCC emission scenarios
Cai, W., Ng, B., Wang, G., Santoso, A., Wu, L., & Yang, K. (2022) · Nature Climate Change · doi:10.1038/s41558-022-01282-z · Cited by 263 · see citing works
Fiedler, S., Crueger, T., D’Agostino, R., Peters, K., Becker, T., Leutwyler, D., Paccini, L., Burdanowitz, J., Buehler, S. A., Cortes, A. U., et al. (2020) · Monthly Weather Review · doi:10.1175/mwr-d-19-0404.1 · Cited by 166 · see citing works
Self-citationRobust decrease in El Niño/Southern Oscillation amplitude under long-term warming
Callahan, C. W., Chen, C., Rugenstein, M., Bloch-Johnson, J., Yang, S., & Moyer, E. J. (2021) · Nature Climate Change · doi:10.1038/s41558-021-01099-2 · Cited by 87 · see citing works
- Authors
- Maher, N., Matei, D., Milinski, S., & Marotzke, J.
- Affiliations
- Alexander von Humboldt Foundation (DE)
- Max Planck Institute for Meteorology (DE)
- Corresponding author
- Maher, N.
- Venue
- Geophysical Research Letters
- Publisher
- American Geophysical Union (AGU)
- Published
- 2018-10-27
- Volume
- 45
- Issue
- 20
- ISSN
- 0094-8276 (ISSN-L)
- 1944-8007
- OpenAlex
- W2897065843
- Cited by
- 170
- References
- 2
- Citations by year
- 2026: 9 · 2025: 19 · 2024: 20 · 2023: 30 · 2022: 27 · 2021: 32 · 2020: 21 · 2019: 11 · 2018: 1
- FWCI
- 9.50
- Type
- journal article
- Language
- en
- Open access
- bronze
- doi.org
- Locations
- Geophysical Research Letters (publishedVersion)
- Funders
- Alexander von Humboldt-Stiftung
- Bundesministerium für Bildung und Forschung (FKZ:01LP1609A)
- Topics
- Physical Sciences › Environmental Science › Global and Planetary Change › Climate variability and models
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Meteorological Phenomena and Simulations
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
- Keywords
- ENSO, ENSO variability, natural climate variability, climate change projections, large ensembles, ENSO amplitude, model intercomparison, RCP scenarios, ensemble size
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
What counts as a claim ›How we measure confidence ›How we check this ›
Are you an author, or do you see a problem with this page? Request a review