@article{fdi:010078685,
  title = {{G}lobalizing results from ocean in situ iron fertilization studies},
  author = {{A}umont, {O}livier and {B}opp, {L}.},
  editor = {},
  language = {{ENG}},
  abstract = {{D}espite the growing number of in situ iron fertilization experiments, the efficiency of such fertilization to sequester atmospheric {CO}2 remains largely unknown. {F}or 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}2. {T}he model reproduces the observed timing and amplitude in chlorophyll, the shift in ecosystem composition, and the p{CO}(2) drawdown; it also proves to be of utility in interpreting the observations. {H}owever, a full ocean fertilization during 100 years results in a 33 mu atm decrease in atmospheric {CO}2, that is 2 to 3 times smaller than found previously.},
  keywords = {{MONDE}},
  booktitle = {},
  journal = {{G}lobal {B}iogeochemical {C}ycles},
  volume = {20},
  numero = {2},
  pages = {art. no. {GB}2017 -- {NIL}_32--{NIL}_46},
  ISSN = {0886-6236},
  year = {2006},
  DOI = {10.1029/2005{GB}002591},
  URL = {https://www.documentation.ird.fr/hor/fdi:010078685},
}