{"refrec":{"BRefID":295117,"RR":"<b>Zhao, J.; Bower, A.; Yang, J.; Lin, X.</b> (2018). Meridional heat transport variability induced by mesoscale processes in the subpolar North Atlantic. <i>Nature Comm. 9(1)</i>: 1124. <a href=\"https://dx.doi.org/10.1038/s41467-018-03134-x\" target=\"_blank\">https://dx.doi.org/10.1038/s41467-018-03134-x</a>","BEntID":287194,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Nature Comm. 9(1)</i>: 1124. <a href=\"https://dx.doi.org/10.1038/s41467-018-03134-x\" target=\"_blank\">https://dx.doi.org/10.1038/s41467-018-03134-x</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Zhao, J.; Bower, A.; Yang, J.; Lin, X.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Zhao, J. <i>et al.</i>","Englishabstract":"The ocean’s role in global climate change largely depends on its heat transport. Therefore, understanding the oceanic meridional heat transport (MHT) variability is a fundamental issue. Prevailing observational and modeling evidence suggests that MHT variability is primarily determined by the large-scale ocean circulation. Here, using new in situ observations in the eastern subpolar North Atlantic Ocean and an eddy-resolving numerical model, we show that energetic mesoscale eddies with horizontal scales of about 10–100 km profoundly modulate MHT variability on time scales from intra-seasonal to interannual. Our results reveal that the velocity changes due to mesoscale processes produce substantial variability for the MHT regionally (within sub-basins) and the subpolar North Atlantic as a whole. The findings have important implications for understanding the mechanisms for poleward heat transport variability in the subpolar North Atlantic Ocean, a key region for heat and carbon sequestration, ice–ocean interaction, and biological productivity.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Meridional heat transport variability induced by mesoscale processes in the subpolar North Atlantic","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-06-15 01:33:03.754612","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2018,"MonPub":null,"DateUpdate":"2019-04-17","DateCreate":"2018-04-30","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000427696500001","VABBcode":null,"OpenAcc":1,"DOI":"10.1038/s41467-018-03134-x"},"refs":null,"anarec":{"AnaID":295117,"PubliDate":2018,"Pagination":"1124","XtraPublOfAnaID":null,"ISBN":null,"Volume":"9","Issue":"1","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":198717,"SerRR":"Nature Communications. 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