{"refrec":{"BRefID":335780,"RR":"<b>Aumont, O.; Bopp, L.</b> (2006). Globalizing results from ocean in situ iron fertilization studies. <i>Global Biogeochem. Cycles 20(2)</i>: GB2017. <a href=\"https://dx.doi.org/10.1029/2005gb002591\" target=\"_blank\">https://dx.doi.org/10.1029/2005gb002591</a>","BEntID":332402,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Global Biogeochem. Cycles 20(2)</i>: GB2017. <a href=\"https://dx.doi.org/10.1029/2005gb002591\" target=\"_blank\">https://dx.doi.org/10.1029/2005gb002591</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Aumont, O.; Bopp, L.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Aumont, O.; Bopp, L.","Englishabstract":"<span class=\"paraNumber\">[1] </span>Despite the growing number of in situ iron fertilization experiments, the efficiency of such fertilization to sequester atmospheric CO<sub>2</sub> remains largely unknown. For the first time, a global ocean biogeochemical model has been evaluated against those experiments and then used to estimate the effect of a long‐term and large‐scale iron addition on atmospheric CO<sub>2</sub>. The model reproduces the observed timing and amplitude in chlorophyll, the shift in ecosystem composition, and the pCO<sub>2</sub> drawdown; it also proves to be of utility in interpreting the observations. 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