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Future Changes in ENSO Discussion Mat Collins College of Engineering, Mathematics and Physical Sciences, University of Exeter, UK © Yann Arthus-Bertrand / Altitude Joint Met Office Chair in Climate Change @mat_collins Chapter 14: Climate Phenomena and their Relevance for Future Regional Climate Change • El Niño-Southern Oscillation very likely remains as the dominant mode of interannual variability in the future and due to increased moisture availability, the associated precipitation variability on regional scales likely intensifies….. natural modulations of the variance and spatial pattern of El Niño-Southern Oscillation are so large in models that confidence in any specific projected change in its variability in the 21st century remains low. Extreme El Niños Cai, Borlce, Lengaigne, van Rensch, Collins, Vecchi, Timmermann, Santoso, McPhaden, Wu, England, Guilyardi, Jin. Increasing frequency of extreme El Niño events due to greenhouse warming. Nature Climate Change, 2014 Changing El Niño Teleconnections Chung, Power, Arblaster, Rashid, Roff, Climate Dynamics, 2014 CMIP5 Atmosphere model simulations Power, Delange, Chung, Kociuba, Keay, Nature 2013 Relationship Between ENSO and Mean Precip Uncertainty in the ENSO amplitude change from the past to the future Masahiro Watanabe, Jong-Seong Kug, Fei-Fei Jin,Mat Collins, Masamichi Ohba, and Andrew T. Wittenberg Changes in Mean Rainfall • Rainfall change anchored to an equatorial peak in SST warming across the Pacific • SST change related to the pattern of latent heat flux in present-day simulations (Xie et al., 2010) • Although the models agree, there are common SST biases in this region. Model agreement ≠ robustness http://climexp.knmi.nl/plot_atlas_form.py Tropical Precipitation Changes: Chadwick et al., 2013 circulation changes moisture availability RH changes circulation weakening Some Open Questions • To what extent do errors and biases in present-day mean climate in models affect the pattern of SST formation under climate change? • How do different patterns of SST change affect patterns of rainfall change, specifically how far the rainfall extends into the east? • Are the ENSO rainfall response results of Power et al. model dependent? • How much is the result of Power et al. dependent upon the spatial pattern of mean SST change? • What are the physical mechanisms underlying the change in ENSO rainfall patterns? • What about different type of ENSO events e.g. central vs east Pacific events? Discussion - Coordinated Experiments (CMIP6)? • Use Power et al./Chung et al. experimental setup. Atmosphere model experiments: • Present day fixed SSTs • Future SST pattern specified from coupled models (like CFMIP) • Future SSTs + ENSOs with different amplitudes • Additional diagnostics specific to ENSO Open Questions • Uncertainties in mean SST changes? • Canonical vs central Pacific ENSOs?