{"refrec":{"BRefID":359044,"RR":"<b>Mueller, K.</b> (2004). Differing methods of accounting ocean carbon sequestration efficiency. <i>J. Geophys. Res. 109(C12)</i>. <a href=\"https://dx.doi.org/10.1029/2003jc002252\" target=\"_blank\">https://dx.doi.org/10.1029/2003jc002252</a>","BEntID":356759,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>J. Geophys. Res. 109(C12)</i>. <a href=\"https://dx.doi.org/10.1029/2003jc002252\" target=\"_blank\">https://dx.doi.org/10.1029/2003jc002252</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Mueller, K.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Mueller, K.","Englishabstract":"<span class=\"paraNumber\">[1] </span>Presently, much of CO<sub>2</sub> fossil-fuel emissions are removed from the atmosphere through natural ocean uptake of CO<sub>2</sub>. Many schemes have now been proposed by which the accumulation of anthropogenic CO<sub>2</sub> in the atmosphere could be slowed with intentional further storage of CO<sub>2</sub> in the ocean. Our review of the literature indicates inconsistency in whether ambient ocean carbon uptake is included when accounting for the effectiveness of such schemes. This inconsistency is a consequence of differing choices of atmospheric boundary condition. In the case of one particular form of ocean sequestration, namely direct injection of liquefied CO<sub>2</sub> emissions into the ocean interior, this choice is the determination of whether the atmospheric CO<sub>2</sub> concentration responsively increases due to leakage of injected carbon from the ocean or retains a specified value. We first show how results of simulations using these two different boundary conditions can be related with the convolution of an atmosphere pulse release. We then use a numerical model to present a more complete analysis of the role of these boundary conditions. Finally, we suggest that a responsive atmospheric CO<sub>2</sub> boundary condition is appropriate for predicting future carbon concentrations, but a specified atmospheric CO<sub>2</sub> boundary condition is appropriate for evaluating how much CO<sub>2</sub> storage should be attributed to an ocean storage project.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Differing methods of accounting ocean carbon sequestration efficiency","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-06-06 01:34:53.820706","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"ocean sequestration, ISAM","OtherDescriptors":null,"Notes":null,"AnaPub":2004,"MonPub":null,"DateUpdate":"2022-11-04","DateCreate":"2022-11-04","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000225882700004","VABBcode":null,"OpenAcc":1,"DOI":"10.1029/2003jc002252"},"refs":null,"anarec":{"AnaID":359044,"PubliDate":2004,"Pagination":null,"XtraPublOfAnaID":null,"ISBN":null,"Volume":"109","Issue":"C12","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":90908,"SerRR":"Journal of Geophysical Research. American Geophysical Union: Richmond.  ISSN 0148-0227; e-ISSN 2156-2202","StandardTitleSer":"Journal of Geophysical Research","ISSN":"0148-0227","AbbrevSer":"J. Geophys. 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