{"refrec":{"BRefID":391335,"RR":"<b>Nidheesh, A.G.; Lengaigne, M.; Vialard, J.; Izumo, T.; Unnikrishnan, A.S.; Krishnan, R.</b> (2019). Natural decadal sea-level variability in the Indian Ocean: lessons from CMIP models. <i>Clim. Dyn. 53(9-10)</i>: 5653-5673. <a href=\"https://dx.doi.org/10.1007/s00382-019-04885-z\" target=\"_blank\">https://dx.doi.org/10.1007/s00382-019-04885-z</a>","BEntID":389082,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Clim. Dyn. 53(9-10)</i>: 5653-5673. <a href=\"https://dx.doi.org/10.1007/s00382-019-04885-z\" target=\"_blank\">https://dx.doi.org/10.1007/s00382-019-04885-z</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Nidheesh, A.G.; Lengaigne, M.; Vialard, J.; Izumo, T.; Unnikrishnan, A.S.; Krishnan, R.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Nidheesh, A.G. <i>et al.</i>","Englishabstract":"Indian Ocean decadal sea-level variability is an active research area, with many unresolved questions due to inadequate observational coverage. In this study, we analyse 26 Coupled Model Intercomparison Project (CMIP) pre-industrial simulations and isolate two consistent modes of Indian Ocean variability, which collectively explain about 50% of the total decadal sea-level variance. With opposite sea-level signals in the southwestern and eastern Indian Ocean, the first mode is related to decadal modulation of the Indian Ocean Dipole (DIOD) and equatorial wind-driven dynamics. Though IOD is more independent of the El Niño–Southern Oscillation (ENSO) at decadal (r ~ 0.4) than interannual (r ~ 0.6) timescales, the DIOD–ENSO co-variability yields sea-level signals along the west coast of Australia, transmitted from the western Pacific via the Indonesian Throughflow. The second mode encompasses variability in the south Indian Ocean (SIODV), exhibiting a broad monopolar sea-level pattern east of Madagascar. In about half of the models, the SIODV is largely independent from DIOD (and decadal ENSO) and driven by south Indian Ocean wind-stress curl associated with meridional shifts in the Mascarene High (MH). In the other models, the SIODV lags the DIOD about 3&nbsp;years. In those models, in addition to MH forcing, the DIOD-related alongshore wind stress off the northwest Australian coast triggers Rossby waves that also contribute to the SIODV, further west. The DIOD and MH forcing are mutually independent (r ~ 0.2). The results are broadly consistent with sea-level variations derived from the short altimeter data, despite an underestimation of the Oceanic bridge signals in CMIP models.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Natural decadal sea-level variability in the Indian Ocean: lessons from CMIP models","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-04-30 01:32:11.271610","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"Natural decadal climate variability; Sea level; Indian Ocean; Indian Ocean Dipole (IOD); El Nino Southern Oscillation (ENSO); CMIP","OtherDescriptors":null,"Notes":null,"AnaPub":2019,"MonPub":null,"DateUpdate":"2024-03-26","DateCreate":"2024-03-26","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000493469900029","VABBcode":null,"OpenAcc":0,"DOI":"10.1007/s00382-019-04885-z"},"refs":null,"anarec":{"AnaID":391335,"PubliDate":2019,"Pagination":"5653-5673","XtraPublOfAnaID":null,"ISBN":null,"Volume":"53","Issue":"9-10","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":45579,"SerRR":"Climate Dynamics. Springer: Berlin; Heidelberg.  ISSN 0930-7575; e-ISSN 1432-0894","StandardTitleSer":"Climate Dynamics","ISSN":"0930-7575","AbbrevSer":"Clim. 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