Evaluation of seasonal teleconnections to remote drivers of Australian rainfall in CMIP5 and CMIP6 models
Christine Chung A * , Ghyslaine Boschat A , Andréa Taschetto B , Sugata Narsey A , Shayne McGregor C , Agus Santoso B and François Delage AA Bureau of Meteorology, 700 Collins Street, Docklands, Melbourne, Vic. 3008, Australia.
B Climate Change Research Centre, University of New South Wales, Sydney, NSW 2052, Australia.
C School of Earth, Atmosphere and Environment, Monash University, Clayton, Vic. 3800, Australia.
Abstract
This study describes how coupled climate models participating in the sixth phase of the Coupled Model Intercomparison Project (CMIP6) simulate the primary climate drivers that affect Australian climate, and their seasonal relationship to Australian rainfall, namely the El Niño–Southern Oscillation (ENSO), the Indian Ocean Dipole (IOD) and the Southern Annular Mode (SAM). As results from the earlier generation of models (CMIP5) are still in use, the CMIP6 multi-model mean teleconnections between climate drivers and seasonal Australian rainfall are compared to CMIP5. Collectively, an improvement is found in CMIP6 relative to CMIP5 in the representation of the relationship between ENSO and IOD events and Australia’s springtime rainfall. Overall, CMIP6 models are also able to reproduce the asymmetric relationship between ENSO and eastern Australian rainfall, which exhibits a more robust signal during La Niña than during El Niño years. Both CMIP5 and CMIP6 models are also generally able to capture the stronger relationship between Central Pacific La Niñas, compared to Eastern Pacific La Niñas. However, the large spread in model-to-model behaviour, and among ensemble members, remains a source of uncertainty. Although CMIP6 models have improved in their representation of SAM variability, the simulated relationship between SAM and Australian rainfall has not materially improved. Additionally, this study is accompanied by an extensive Appendix in which each model’s ENSO, IOD and SAM seasonal teleconnection patterns to rainfall are presented and ranked.
Keywords: climate drivers, climate models, CMIP, ENSO, IOD, model evaluation, SAM, seasonal rainfall.
References
Abram NJ, Wright NM, Ellis B, et al. (2020) Coupling of Indo-Pacific climate variability over the last millennium. Nature 579, 385-392.
| Crossref | Google Scholar |
Ashok K, Guan Z, Yamagata T (2003) Influence of the Indian Ocean Dipole on the Australian winter rainfall. Geophysical Research Letters 30(15), 1821.
| Crossref | Google Scholar |
Baker HS, Woollings T, Mbengue C (2017) Eddy‐driven jet sensitivity to diabatic heating in an idealized GCM. Journal of Climate 30(16), 6413-6431.
| Crossref | Google Scholar |
Barnes EA, Polvani L (2013) Response of the midlatitude jets, and of their variability, to increased greenhouse gases in the CMIP5 models. Journal of Climate 26, 7117-7135.
| Crossref | Google Scholar |
Boschat G, Purich A, Rudeva I, Arblaster J (2023) Impact of zonal and meridional atmospheric flow on surface climate and extremes in the Southern Hemisphere. Journal of Climate 36, 5041-5061.
| Crossref | Google Scholar |
Bracegirdle TJ, Holmes CR, Hosking JS, Marshall GJ, Osman M, Patterson M, Rackow T (2020) Improvements in circumpolar southern hemisphere extratropical atmospheric circulation in CMIP6 compared to CMIP5. Earth and Space Science 7, e2019EA001065.
| Crossref | Google Scholar |
Burgers G, Stephenson DB (1999) The “normality” of El Niño. Geophysical Research Letters 26, 1027-1030.
| Crossref | Google Scholar |
Cai W, Cowan T (2013) Why is the amplitude of the Indian Ocean Dipole overly large in CMIP3 and CMIP5 climate models? Geophysical Research Letters 40, 1200-1205.
| Crossref | Google Scholar |
Cai W, van Rensch P, Cowan T, Sullivan A (2010) Asymmetry in ENSO teleconnection with regional rainfall, its multidecadal variability, and impact. Journal of Climate 23(18), 4944-4955.
| Crossref | Google Scholar |
Cai W, Cowan T, Sullivan A, Ribbe J, Shi G (2011) Are anthropogenic aerosols responsible for the northwest Australia summer rainfall increase? A CMIP3 perspective and implications. Journal of Climate 24, 2556-2564.
| Crossref | Google Scholar |
Cai W, van Rensch P, Cowan T, Hendon HH (2012) An asymmetry in the IOD and ENSO teleconnection pathway and its impact on Australian climate. Journal of Climate 25(18), 6318-6329.
| Crossref | Google Scholar |
Cai W, Ng B, Wang G, et al. (2022) Increased ENSO sea surface temperature variability under four IPCC emission scenarios. Nature Climate Change 12, 228-231.
| Crossref | Google Scholar |
Capotondi A, Wittenberg AT, Newman M, et al. (2015) Understanding ENSO diversity. Bulletin of the American Meteorological Society 96, 921-938.
| Crossref | Google Scholar |
Chung CTY, Power SB (2017) The non-linear impact of El Niño, La Niña and the Southern Oscillation on seasonal and regional Australian precipitation. Journal of Southern Hemisphere Earth Systems Science 67(1), 25-45.
| Crossref | Google Scholar |
Dätwyler C, Grosjean M, Steiger NJ, Neukom R (2020) Teleconnections and relationship between the El Niño–Southern Oscillation (ENSO) and the Southern Annular Mode (SAM) in reconstructions and models over the past millennium. Climate of the Past 16, 743-756.
| Crossref | Google Scholar |
Dhame S, Taschetto AS, Santoso A, Meissner KJ (2020) Indian Ocean warming modulates global atmospheric circulation trends. Climate Dynamics 55, 2053-2073.
| Crossref | Google Scholar |
Di Virgilio G, Ji F, Tam E, Nishant N, Evans JP, Thomas C, et al. (2022) Selecting CMIP6 GCMs for CORDEX dynamical downscaling: model performance, independence, and climate change signals. Earth’s Future 10, e2021EF002625.
| Crossref | Google Scholar |
Dong L, McPhaden MJ (2017) Why has the relationship between Indian and Pacific Ocean decadal variability changed in recent decades? Journal of Climate 30, 1971-1983.
| Crossref | Google Scholar |
Du Y, Xie S-P (2008) Role of atmospheric adjustments in the tropical Indian Ocean warming during the 20th century in climate models. Geophysical Research Letters 35, L08712.
| Crossref | Google Scholar |
Eyring V, Bony S, Meehl GA, Senior CA, Stevens B, Stouffer RJ, Taylor KE (2016) Overview of the Coupled Model Intercomparison Project Phase 6 (CMIP6) experimental design and organization. Geoscientific Model Development 9, 1937-1958.
| Crossref | Google Scholar |
Feng J, Lian T, Ying J, Li J, Li G (2020) Do CMIP5 models show El Niño diversity? Journal of Climate 33(5), 1619-1641.
| Crossref | Google Scholar |
Fogt RL, Marshall GJ (2020) The Southern Annular Mode: variability, trends, and climate impacts across the Southern Hemisphere. WIREs Clim Change 11, 1-24.
| Crossref | Google Scholar |
Freund MB, Henley BJ, Karoly DJ, et al. (2019) Higher frequency of Central Pacific El Niño events in recent decades relative to past centuries. Nature Geoscience 12, 450-455.
| Crossref | Google Scholar |
Garcia-Villada LP, Donat MG, Angélil O, et al. (2020) Temperature and precipitation responses to El Niño–Southern Oscillation in a hierarchy of datasets with different levels of observational constraints. Climate Dynamics 55, 2351-2376.
| Crossref | Google Scholar |
Gong D, Wang S (1999) Definition of Antarctic oscillation index. Geophysical Research Letters 26, 459-462.
| Crossref | Google Scholar |
Goyal R, Gupta AS, Jucker M, England MH (2021) Historical and projected changes in the Southern Hemisphere surface westerlies. Geophysical Research Letters 48, e2020GL090849.
| Crossref | Google Scholar |
Grose MR, Narsey S, Delage FP, Dowdy AJ, Bador M, Boschat G, et al. (2020) Insights from CMIP6 for Australia’s future climate. Earth’s Future 8, e2019EF001469.
| Crossref | Google Scholar |
Grose MR, Narsey S, Trancoso R, Mackallah C, Delage F, Dowdy A, Di Virgilio G, Watterson I, Dobrohotoff P, Rashid HA, Rauniyar S, Henley B, Thatcher M, Syktus J, Abramowitz G, Evans JP, Su C-H, Takbash A (2023) A CMIP6-based multi-model downscaling ensemble to underpin climate change services in Australia. Climate Services 30, 100368.
| Crossref | Google Scholar |
Halder S, Parekh A, Chowdary JS, Gnanaseelan C, Kulkarni A (2021) Assessment of CMIP6 models’ skill for tropical Indian Ocean sea surface temperature variability. International Journal of Climatology 41, 2568-2588.
| Crossref | Google Scholar |
Heidemann H, Ribbe J, Cowan T, Henley BJ, Pudmenzky C, Stone R, Cobon DH (2022) The influence of interannual and decadal Indo-Pacific sea surface temperature variability on Australian monsoon rainfall. Journal of Climate 35, 425-444.
| Crossref | Google Scholar |
Hendon HH, Thompson DWJ, Wheeler MC (2007) Australian rainfall and surface temperature variations associated with the Southern Hemisphere annular mode. Journal of Climate 20, 2452-2467.
| Crossref | Google Scholar |
Henley BJ, Gergis J, Karoly DJ, et al. (2015) A tripole index for the interdecadal Pacific Oscillation. Climate Dynamics 45, 3077-3090.
| Crossref | Google Scholar |
Holgate C, Evans JP, Taschetto AS, Gupta AS, Santoso A (2022) The impact of interacting climate modes on east Australian precipitation moisture sources. Journal of Climate 35(10), 3147-3159.
| Crossref | Google Scholar |
Hou M, Tang Y (2022) Recent progress in simulating two types of ENSO – from CMIP5 to CMIP6. Frontiers in Marine Science 9, 986780.
| Crossref | Google Scholar |
Huang Y, Wu B, Li T, Zhou T, Liu B (2019) Interdecadal Indian Ocean Basin mode driven by interdecadal Pacific oscillation: a season-dependent growth mechanism. Journal of Climate 32(7), 2057-2073.
| Crossref | Google Scholar |
Jiang W, Huang P, Huang G, Ying J (2021) Origins of the excessive westward extension of ENSO SST simulated in CMIP5 and CMIP6 models. Journal of Climate 34(8), 2839-2851.
| Crossref | Google Scholar |
Jourdain NC, Gupta AS, Taschetto AS, et al. (2013) The Indo-Australian monsoon and its relationship to ENSO and IOD in reanalysis data and the CMIP3/CMIP5 simulations. Climate Dynamics 41, 3073-3102.
| Crossref | Google Scholar |
Kajtar JB, Santoso A, Collins M, Taschetto AS, England MH, Frankcombe LM (2021) CMIP5 intermodel relationships in the baseline Southern Ocean climate system and with future projections. Earth’s Future 9, e2020EF001873.
| Crossref | Google Scholar |
Kidston J, Gerber EP (2010) Intermodel variability of the poleward shift of the austral jet stream in the CMIP3 integrations linked to biases in 20th century climatology. Geophysical Research Letters 37, L09708.
| Crossref | Google Scholar |
Kim ST, Jeong H-I, Jin F-F (2017) Mean bias in seasonal forecast model and ENSO prediction error. Scientific Reports 7, 6029.
| Crossref | Google Scholar |
King AD, Donat MG, Alexander LV, Karoly DJ (2014) The ENSO-Australian rainfall teleconnection in reanalysis and CMIP5. Climate Dynamics 44, 2623-2635.
| Crossref | Google Scholar |
King AD, Pitman AJ, Henley BJ, et al. (2020) The role of climate variability in Australian drought. Nature Climate Change 10, 177-179.
| Crossref | Google Scholar |
Kociuba G, Power SB (2015) Inability of CMIP5 models to simulate recent strengthening of the Walker Circulation: implications for projections. Journal of Climate 28(1), 20-35.
| Crossref | Google Scholar |
Kripalani RH, Kumar P (2004) Northeast monsoon rainfall variability over south peninsular India vis-à-vis the Indian Ocean dipole mode. International Journal of Climatology 24, 1267-1282.
| Crossref | Google Scholar |
Kug JS, Jin F-F, An SI (2009) Two types of El Niño events: cold tongue El Niño and warm pool El Niño. Journal of Climate 22, 1499-1515.
| Crossref | Google Scholar |
Lee J, Planton YY, Gleckler PJ, Sperber KR, Guilyardi E, Wittenberg AT, et al. (2021) Robust evaluation of ENSO in climate models: how many ensemble members are needed? Geophysical Research Letters 48, e2021GL095041.
| Crossref | Google Scholar |
Li G, Xie S-P (2014) Tropical biases in CMIP5 multimodel ensemble: the excessive Equatorial Pacific cold tongue and double ITCZ problems. Journal of Climate 27, 1765-1780.
| Crossref | Google Scholar |
Liguori G, McGregor S, Singh M, Arblaster J, Di Lorenzo E (2022) Revisiting ENSO and IOD contributions to Australian precipitation. Geophysical Research Letters 49, e2021GL094295.
| Crossref | Google Scholar |
Lim E-P, Hendon HH, Arblaster JM, Delage F, Nguyen H, Min S-K, Wheeler MC (2016) The impact of the Southern Annular Mode on future changes in Southern Hemisphere rainfall. Geophysical Research Letters 43, 7160-7167.
| Crossref | Google Scholar |
Lim EP, Hendon HH, Boschat G, et al. (2019) Australian hot and dry extremes induced by weakenings of the stratospheric polar vortex. Nature Geoscience 12, 896-901.
| Crossref | Google Scholar |
Limpasuvan V, Hartmann DL (1999) Eddies and the annular modes of climate variability. Geophysical Research Letters 26, 3133-3136.
| Crossref | Google Scholar |
Ma Y, Sun J, Dong T, et al. (2022) More profound impact of CP ENSO on Australian spring rainfall in recent decades. Climate Dynamics 60, 3065-3079.
| Crossref | Google Scholar |
McGregor S, Cassou C, Kosaka Y, Phillips AS (2022) Projected ENSO teleconnection changes in CMIP6. Geophysical Research Letters 49, e2021GL097511.
| Crossref | Google Scholar |
McKenna S, Santoso A, Gupta AS, et al. (2020) Indian Ocean Dipole in CMIP5 and CMIP6: characteristics, biases, and links to ENSO. Scientific Reports 10, 11500.
| Crossref | Google Scholar |
Marshall GJ (2003) Trends in the southern annular mode from observations and reanalyses. Journal of Climate 16(24), 4134-4143.
| Crossref | Google Scholar |
Masson-Delmotte V, Zhai P, Pirani A, Connors SL, Péan C, Berger S, Caud N, Chen Y, Goldfarb L, Gomis MI, Huang M, Leitzell K, Lonnoy E, Matthews JBR, Maycock TK, Waterfield T, Yelekçi O, Yu R, Zhou B (2021) ‘Climate Change 2021: The Physical Science Basis. Contribution of Working Group I to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change.’ (Cambridge University Press: Cambridge, UK, and New York, NY, USA) doi:10.1017/9781009157896
Meneghini B, Simmonds I, Smith IN (2007) Association between Australian rainfall and the Southern Annular Mode. International Journal of Climatology 27, 109-121.
| Crossref | Google Scholar |
Meyers G, McIntosh P, Pigot L, Pook M (2007) The years of El Niño, La Niña, and interactions with the tropical Indian Ocean. Journal of Climate 20, 2872-2880.
| Crossref | Google Scholar |
Morgenstern O (2021) The Southern Annular Mode in 6th Coupled Model Intercomparison Project models. Journal of Geophysical Research: Atmospheres 126(5),.
| Crossref | Google Scholar |
Parsons LA, Brennan MK, Wills RCJ, Proistosescu C (2020) Magnitudes and spatial patterns of interdecadal temperature variability in CMIP6. Geophysical Research Letters 47, e2019GL086588.
| Crossref | Google Scholar |
Pepler A, Timbal B, Rakich C, Coutts-Smith A (2014) Indian Ocean Dipole Overrides ENSO’s influence on cool season rainfall across the Eastern Seaboard of Australia. Journal of Climate 27(10), 3816-3826.
| Crossref | Google Scholar |
Planton YY, Guilyardi E, Wittenberg AT, Lee J, Gleckler PJ, Bayr T, McGregor S, McPhaden MJ, Power S, Roehrig R, Vialard J, Voldoire A (2021) Evaluating climate models with the CLIVAR 2020 ENSO Metrics Package. Bulletin of the American Meteorological Society 102(2), E193-E217.
| Crossref | Google Scholar |
Power SB, Delage FPD (2018) El Niño–Southern Oscillation and associated climatic conditions around the world during the latter half of the twenty-first century. Journal of Climate 31, 6189-6207.
| Crossref | Google Scholar |
Power S, Casey T, Folland C, et al. (1999) Inter-decadal modulation of the impact of ENSO on Australia. Climate Dynamics 15, 319-324.
| Crossref | Google Scholar |
Power S, Haylock M, Colman R, Wang X (2006) The predictability of interdecadal changes in ENSO activity and ENSO teleconnections. Journal of Climate 19, 4755-4771.
| Crossref | Google Scholar |
Rayner NA, Parker DE, Horton EB, Folland CK, Alexander LV, Rowell DP, Kent EC, Kaplan A (2003) Global analyses of sea surface temperature, sea ice, and night marine air temperature since the late nineteenth century. Journal of Geophysical Research: Atmospheres 108, 4407.
| Crossref | Google Scholar |
Risbey JS, Pook MJ, McIntosh PC, Wheeler MC, Hendon HH (2009) On the remote drivers of rainfall variability in Australia. Monthly Weather Review 137, 3233-3253.
| Crossref | Google Scholar |
Roxy MK, Ritika K, Terray P, Masson S (2014) The curious case of Indian Ocean warming. Journal of Climate 27, 8501-8509.
| Crossref | Google Scholar |
Saji NH, Goswami BN, Vinayachandran PN, Yamagata T (1999) A dipole mode in the tropical Indian Ocean. Nature 401, 360-363.
| Crossref | Google Scholar |
Salinger MJ, Renwick JA, Mullan AB (2001) Interdecadal Pacific Oscillation and South Pacific climate. International Journal of Climatology 21, 1705-1721.
| Crossref | Google Scholar |
Santoso A, Mcphaden MJ, Cai W (2017) The defining characteristics of ENSO extremes and the strong 2015/2016 El Niño. Reviews of Geophysics 55, 1079-1129.
| Crossref | Google Scholar |
Santoso A, Hendon H, Watkins A, Power S, Dommenget D, England MH, Frankcombe L, Holbrook NJ, Holmes R, Hope P, Lim E-P, Luo J-J, McGregor S, Neske S, Nguyen H, Pepler A, Rashid H, Gupta AS, Taschetto AS, et al. (2019) Dynamics and predictability of El Niño–Southern Oscillation: an Australian perspective on progress and challenges. Bulletin of the American Meteorological Society 100(3), 403-420.
| Crossref | Google Scholar |
Screen JA, Eade R, Smith DM, Thomson S, Yu H (2022) Net equatorward shift of the jet streams when the contribution from sea-ice loss is constrained by observed eddy feedback. Geophysical Research Letters 49, e2022GL100523.
| Crossref | Google Scholar |
Sullivan A, Luo JJ, Hirst AC, et al. (2016) Robust contribution of decadal anomalies to the frequency of central-Pacific El Niño. Scientific Reports 6, 38540.
| Crossref | Google Scholar |
Taschetto AS, England MH (2009) El Niño Modoki impacts on Australian rainfall. Journal of Climate 22, 3167-3174.
| Crossref | Google Scholar |
Taschetto AS, Haarsma RJ, Gupta AS, Ummenhofer CC, Hill KJ, England MH (2010) Australian monsoon variability driven by a Gill–Matsuno-type response to central west Pacific warming. Journal of Climate 23, 4717-4736.
| Crossref | Google Scholar |
Taschetto AS, Gupta AS, Jourdain NC, Santoso A, Ummenhofer CC, England MH (2014) Cold tongue and warm pool ENSO Events in CMIP5: mean state and future projections. Journal of Climate 27, 2861-2885.
| Crossref | Google Scholar |
Taschetto AS, Ummenhofer CC, Stuecker MF, Dommenget D, Ashok K, Rodrigues RR, Yeh S-W (2020) ENSO atmospheric teleconnections. In ‘El Niño Southern Oscillation in a Changing Climate’. (Eds MJ McPhaden, A Santoso, W Cai) pp. 309–335. (American Geophysical Union) 10.1002/9781119548164.ch14
Taylor KE, Stouffer RJ, Meehl GA (2012) An overview of CMIP5 and the experiment design. Bulletin of the American Meteorological Society 93, 485-498.
| Crossref | Google Scholar |
Ummenhofer CC, England MH, McIntosh PC, Meyers GA, Pook MJ, Risbey JS, Gupta AS, Taschetto AS (2009) What causes southeast Australia’s worst droughts? Geophysical Research Letters 36, L04706.
| Crossref | Google Scholar |
Ummenhofer CC, Gupta AS, Briggs PR, et al. (2011) Indian and Pacific Ocean influences on southeast Australian drought and soil moisture. Journal of Climate 24, 1313-1336.
| Crossref | Google Scholar |
Ummenhofer CC, Sen Gupta A, England MH, Taschetto AS, Briggs PR, Raupach MR (2015) How did ocean warming affect Australian rainfall extremes during the 2010/2011 La Niña event? Geophysical Research Letters 42(22), 9942-9951.
| Crossref | Google Scholar |
Wang G, Cai W (2020) Two-year consecutive concurrences of positive Indian Ocean Dipole and Central Pacific El Niño preconditioned the 2019/2020 Australian “Black Summer” bushfires. Geoscience Letters 7, 19.
| Crossref | Google Scholar |
Wang G, Cai W, Santoso A (2017b) Assessing the impact of model biases on the projected increase in frequency of extreme positive Indian Ocean Dipole events. Journal of Climate 30(8), 2757-2767.
| Crossref | Google Scholar |
Wang B, Luo X, Yang YM, Sun W, Cane MA, Cai W, Yeh SW, Liu J (2019) Historical change of El Niño properties sheds light on future changes of extreme El Niño. Proceedings of the National Academy of Sciences of the United States of America 116(45), 22512-22517.
| Crossref | Google Scholar |
Wang G, Cai W, Santoso A (2021) Simulated thermocline tilt over the tropical Indian Ocean and its influence on future sea surface temperature variability. Geophysical Research Letters 48, e2020GL091902.
| Crossref | Google Scholar |
Webster PJ, Moore AM, Loschnigg JP, Leben RR (1999) Coupled ocean–atmosphere dynamics in the Indian Ocean during 1997–98. Nature 401, 356-360.
| Crossref | Google Scholar |
Weller E, Cai W (2013) Realism of the Indian Ocean Dipole in CMIP5 models: the implications for climate projections. Journal of Climate 26, 6649-6659.
| Crossref | Google Scholar |
Wu X, Okumura YM, DiNezio PN, Yeager SG, Deser C (2022) The Equatorial Pacific cold tongue bias in CESM1 and its influence on ENSO forecasts. Journal of Climate 35(11), 3261-3277.
| Crossref | Google Scholar |
Yeh S-W, Cai W, Min S-K, McPhaden MJ, Dommenget D, Dewitte B, et al. (2018) ENSO atmospheric teleconnections and their response to greenhouse gas forcing. Reviews of Geophysics 56, 185-206.
| Crossref | Google Scholar |
Zhang X, He B, Liu Y, Bao Q, Zheng F, Li J, Hu W, Wu G (2021) Evaluation of the seasonality and spatial aspects of the Southern Annular Mode in CMIP6 models. International Journal of Climatology 42, 3820-3837.
| Crossref | Google Scholar |
Zhao Y, Sun D-Z (2022) ENSO asymmetry in CMIP6 models. Journal of Climate 35(17), 5555-5572.
| Crossref | Google Scholar |