{"refrec":{"BRefID":354196,"RR":"<b>Mignot, A.; von Schuckmann, K.; Landschützer, P.; Gasparin, F.; van Gennip, S.; Perruche, C.; Lamouroux, J.; Amm, T.</b> (2022). Decrease in air-sea CO<sub>2</sub> fluxes caused by persistent marine heatwaves. <i>Nature Comm. 13(1)</i>: 4300. <a href=\"https://dx.doi.org/10.1038/s41467-022-31983-0\" target=\"_blank\">https://dx.doi.org/10.1038/s41467-022-31983-0</a>","BEntID":351909,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Nature Comm. 13(1)</i>: 4300. <a href=\"https://dx.doi.org/10.1038/s41467-022-31983-0\" target=\"_blank\">https://dx.doi.org/10.1038/s41467-022-31983-0</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Mignot, A.; von Schuckmann, K.; Landschützer, P.; Gasparin, F.; van Gennip, S.; Perruche, C.; Lamouroux, J.; Amm, T.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Mignot, A. <i>et al.</i>","Englishabstract":"Regional processes play a key role in the global carbon budget. Major ocean CO<sub>2</sub> uptake at mid-latitudes counteracts CO<sub>2</sub> release in the tropics, which is modulated by episodes of marine heatwaves. Yet, we lack essential knowledge on persistent marine heatwaves, and their effect on the CO<sub>2</sub> sensitive areas. Here we show, using a 1985–2017 joint analysis of reconstructions, ocean reanalysis and in situ and satellite data, that persistent marine heatwaves occur in major CO<sub>2</sub> uptake and release areas. Average air-sea CO<sub>2</sub> flux density changes from persistent marine heatwaves are strongest in the Pacific Ocean with a 40 ± 9% reduction in CO<sub>2</sub> release in the tropics linked to ENSO, and a reduction in CO<sub>2</sub> uptake of 29 ± 11% in the North Pacific over the study period. These results provide new insights into the interplay of extreme variability and a critical regulating ocean ecosystem service, and pave the way for future investigations on its evolution under climate change.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Decrease in air-sea CO<sub>2</sub> fluxes caused by persistent marine heatwaves","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-04-18 01:32:30.147375","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2022,"MonPub":null,"DateUpdate":"2022-07-27","DateCreate":"2022-07-27","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:001043209100001","VABBcode":null,"OpenAcc":1,"DOI":"10.1038/s41467-022-31983-0"},"refs":null,"anarec":{"AnaID":354196,"PubliDate":2022,"Pagination":"4300","XtraPublOfAnaID":null,"ISBN":null,"Volume":"13","Issue":"1","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":198717,"SerRR":"Nature Communications. 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