{"refrec":{"BRefID":355449,"RR":"<b>Yang, Y.; Wu, L.; Cai, W.; Jia, F.; Ng, B.; Wang, G.; Geng, T.</b> (2022). Suppressed Atlantic Niño/Niña variability under greenhouse warming. <i>Nat. Clim. Chang. 12(9)</i>: 814-821. <a href=\"https://dx.doi.org/10.1038/s41558-022-01444-z\" target=\"_blank\">https://dx.doi.org/10.1038/s41558-022-01444-z</a>","BEntID":353162,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Nat. Clim. Chang. 12(9)</i>: 814-821. <a href=\"https://dx.doi.org/10.1038/s41558-022-01444-z\" target=\"_blank\">https://dx.doi.org/10.1038/s41558-022-01444-z</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Yang, Y.; Wu, L.; Cai, W.; Jia, F.; Ng, B.; Wang, G.; Geng, T.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Yang, Y. <i>et al.</i>","Englishabstract":"The Atlantic Niño/Niña is a dominant mode of interannual variability peaking in boreal summer with substantial climate impacts. How the Atlantic Niño/Niña sea surface temperature (SST) variability may change under greenhouse warming remains unclear. Here we find a robust suppression in future Atlantic Niño/Niña variability in models that simulate a reasonable mean climatology of the equatorial Atlantic. Under greenhouse warming, the equatorial Atlantic atmosphere becomes more stable, reducing sensitivity of the equatorial zonal winds to the zonal SST gradient; further, weakened trade winds lead to a deepened thermocline in the east, reducing SST sensitivity to thermocline anomalies. These changes feed into Bjerknes feedback to cause suppression in Atlantic Niño/Niña SST variability. These findings are in stark contrast to the Pacific and the Indian Ocean where El Niño/La Niña SST variability and strong Indian Ocean Dipole variability are projected to increase.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Suppressed Atlantic Niño/Niña variability under greenhouse warming","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-06-13 01:31:56.731680","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2022,"MonPub":null,"DateUpdate":"2022-09-15","DateCreate":"2022-09-15","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000849293400002","VABBcode":null,"OpenAcc":0,"DOI":"10.1038/s41558-022-01444-z"},"refs":null,"anarec":{"AnaID":355449,"PubliDate":2022,"Pagination":"814-821","XtraPublOfAnaID":null,"ISBN":null,"Volume":"12","Issue":"9","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":218223,"SerRR":"Nature Climate Change. 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