{"refrec":{"BRefID":345706,"RR":"<b>Liu, M.; Vecchi, G.A.; Soden, B.; Yang, W.; Zhang, B.</b> (2021). Enhanced hydrological cycle increases ocean heat uptake and moderates transient climate change. <i>Nat. Clim. Chang. 11(10)</i>: 848-853. <a href=\"https://dx.doi.org/10.1038/s41558-021-01152-0\" target=\"_blank\">https://dx.doi.org/10.1038/s41558-021-01152-0</a>","BEntID":342341,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Nat. Clim. Chang. 11(10)</i>: 848-853. <a href=\"https://dx.doi.org/10.1038/s41558-021-01152-0\" target=\"_blank\">https://dx.doi.org/10.1038/s41558-021-01152-0</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Liu, M.; Vecchi, G.A.; Soden, B.; Yang, W.; Zhang, B.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Liu, M. <i>et al.</i>","Englishabstract":"The large-scale moistening of the atmosphere in response to increasing greenhouse gases amplifies the existing patterns of precipitation minus evaporation (<i>P</i> − <i>E</i>), which, in turn, amplifies the spatial contrast in sea surface salinity. Here, by performing a series of transient CO<sub>2</sub> doubling experiments, we demonstrate that surface salinification driven by the amplified dry conditions (<i>P</i> − <i>E</i> &lt; 0), primarily in the subtropical ocean, accelerates ocean heat uptake. The salinification also drives the sequestration of upper-level heat into the deeper ocean, reducing the thermal stratification and increasing the heat uptake through positive feedback. The change in Atlantic Meridional Overturning Circulation due to salinification has a secondary role in heat uptake. Consistent with the heat uptake changes, the transient climate response would increase by approximately 0.4 K without this process. Observed multidecadal changes in subsurface temperature and salinity resemble those simulated, indicating that anthropogenically forced changes in salinity are probably enhancing ocean heat uptake.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Enhanced hydrological cycle increases ocean heat uptake and moderates transient climate change","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-06-16 01:33:28.235597","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2021,"MonPub":null,"DateUpdate":"2021-10-08","DateCreate":"2021-10-08","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000698572600003","VABBcode":null,"OpenAcc":0,"DOI":"10.1038/s41558-021-01152-0"},"refs":null,"anarec":{"AnaID":345706,"PubliDate":2021,"Pagination":"848-853","XtraPublOfAnaID":null,"ISBN":null,"Volume":"11","Issue":"10","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":218223,"SerRR":"Nature Climate Change. 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