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• W4290052202 endingPage "5572" @default.
• W4290052202 startingPage "5555" @default.
• W4290052202 abstract "Abstract An interesting aspect of the El Niño–Southern Oscillation (ENSO) phenomenon is the asymmetry between its two phases. This paper evaluates the simulations of this property of ENSO by the Coupled Model Intercomparison Project phase 6 (CMIP6) models. Both the surface and subsurface signals of ENSO are examined for this purpose. The results show that the models still underestimate ENSO asymmetry as shown in the SST field, but do a better job in the subsurface. A much weaker negative feedback from the net surface heat flux during La Niña in the models is identified as a factor causing the degradation of the ENSO asymmetry at the surface. The simulated asymmetry in the subsurface is still weaker than the observations owing to a weaker dynamic coupling between the atmosphere and ocean. Consistent with the finding of a weaker dynamic coupling strength, the precipitation response to the SST changes is also found to be weaker in the models. The results underscore that a more objective assessment of the simulation of ENSO by climate models may have to involve the examination of the subsurface signals. Future improvements in simulating ENSO will likely require a better simulation of the surface heat flux feedback from the atmosphere as well as the dynamical coupling strength between the atmosphere and ocean. Significance Statement The ENSO phenomenon affects weather and climate worldwide. An interesting aspect of this phenomenon is the asymmetry between its two phases. Previous studies have reported a weaker asymmetry in the simulations by climate models. But these studies have focused on the ENSO asymmetry at the surface. Here by examining the ENSO asymmetry at the surface and the subsurface, we have found that ENSO asymmetry is better simulated in the subsurface than at the surface. We have also identified factors that are responsible for the degradation of the ENSO asymmetry at the surface as well as the remaining weakness in the subsurface, pointing out specific pathways to take to further improve ENSO simulations by coupled climate models." @default.
• W4290052202 created "2022-08-06" @default.
• W4290052202 creator A5019056704 @default.
• W4290052202 creator A5043470879 @default.
• W4290052202 date "2022-09-01" @default.
• W4290052202 modified "2023-10-12" @default.
• W4290052202 title "ENSO Asymmetry in CMIP6 Models" @default.
• W4290052202 cites W1493970646 @default.
• W4290052202 cites W1683974079 @default.
• W4290052202 cites W1805642797 @default.
• W4290052202 cites W1869458723 @default.
• W4290052202 cites W1910754480 @default.
• W4290052202 cites W1963966696 @default.
• W4290052202 cites W1967031773 @default.
• W4290052202 cites W1967753047 @default.
• W4290052202 cites W1979615854 @default.
• W4290052202 cites W1980121541 @default.
• W4290052202 cites W1983066276 @default.
• W4290052202 cites W1985369177 @default.
• W4290052202 cites W1987445306 @default.
• W4290052202 cites W1988559412 @default.
• W4290052202 cites W1992576706 @default.
• W4290052202 cites W1992780005 @default.
• W4290052202 cites W1993196883 @default.
• W4290052202 cites W1996417708 @default.
• W4290052202 cites W1997183890 @default.
• W4290052202 cites W2005810380 @default.
• W4290052202 cites W2006165291 @default.
• W4290052202 cites W2007098680 @default.
• W4290052202 cites W2021705657 @default.
• W4290052202 cites W2022124898 @default.
• W4290052202 cites W2022139274 @default.
• W4290052202 cites W2023372691 @default.
• W4290052202 cites W2024966118 @default.
• W4290052202 cites W2025751122 @default.
• W4290052202 cites W2026257927 @default.
• W4290052202 cites W2030797143 @default.
• W4290052202 cites W2031682224 @default.
• W4290052202 cites W2033484571 @default.
• W4290052202 cites W2037344034 @default.
• W4290052202 cites W2037621887 @default.
• W4290052202 cites W2041976924 @default.
• W4290052202 cites W2042793679 @default.
• W4290052202 cites W2046589183 @default.
• W4290052202 cites W2047604301 @default.
• W4290052202 cites W2051708308 @default.
• W4290052202 cites W2051986510 @default.
• W4290052202 cites W2062217294 @default.
• W4290052202 cites W2062354157 @default.
• W4290052202 cites W2064817469 @default.
• W4290052202 cites W2071925930 @default.
• W4290052202 cites W2072228305 @default.
• W4290052202 cites W2072418905 @default.
• W4290052202 cites W2072747025 @default.
• W4290052202 cites W2073759294 @default.
• W4290052202 cites W2084843069 @default.
• W4290052202 cites W2086031127 @default.
• W4290052202 cites W2089010948 @default.
• W4290052202 cites W2090249381 @default.
• W4290052202 cites W2096587785 @default.
• W4290052202 cites W2099402554 @default.
• W4290052202 cites W2103763236 @default.
• W4290052202 cites W2105541671 @default.
• W4290052202 cites W2107672168 @default.
• W4290052202 cites W2119968725 @default.
• W4290052202 cites W2132649926 @default.
• W4290052202 cites W2136798118 @default.
• W4290052202 cites W2137240689 @default.
• W4290052202 cites W2138271320 @default.
• W4290052202 cites W2138408594 @default.
• W4290052202 cites W2139558540 @default.
• W4290052202 cites W2150897391 @default.
• W4290052202 cites W2152243413 @default.
• W4290052202 cites W2152514748 @default.
• W4290052202 cites W2157333173 @default.
• W4290052202 cites W2157807748 @default.
• W4290052202 cites W2161074445 @default.
• W4290052202 cites W2167623001 @default.
• W4290052202 cites W2169466525 @default.
• W4290052202 cites W2175550040 @default.
• W4290052202 cites W2175816372 @default.
• W4290052202 cites W2176956584 @default.
• W4290052202 cites W2177885470 @default.
• W4290052202 cites W2193503481 @default.
• W4290052202 cites W2217189261 @default.
• W4290052202 cites W2222753719 @default.
• W4290052202 cites W2348951245 @default.
• W4290052202 cites W2507318219 @default.
• W4290052202 cites W2511044748 @default.
• W4290052202 cites W2532641604 @default.
• W4290052202 cites W2583890331 @default.
• W4290052202 cites W2601443869 @default.
• W4290052202 cites W2613365221 @default.
• W4290052202 cites W2616382558 @default.
• W4290052202 cites W2626504202 @default.
• W4290052202 cites W2735472493 @default.
• W4290052202 cites W2751507746 @default.
• W4290052202 cites W2772362219 @default.

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