@article{fdi:010091478,
  title = {{R}esponse of {CO}2 fluxes to the ocean-atmosphere interaction processes in the {F}ernando de {N}oronha island},
  author = {{A}lves, {L}.{H}.{B}. and {F}lores {M}ontes, {M}. and {L}ef{\`e}vre, {N}athalie and {L}uiz do {V}ale {S}ilva, {T}. and {L}opes, {F}. and {V}eleda, {D}.},
  editor = {},
  language = {{ENG}},
  abstract = {{T}his study investigates thermodynamic conditions and air-sea {CO}2fluxes in the {F}ernando de {N}oronha {I}sland region.  {T}he  analyses  were  based  on  coupled  ocean-atmosphere  modeling  results  for  three  periods  of oceanographic cruises, {C}amadas {F}inas {I}, {C}amadas {F}inas {II}, and {C}amadas {F}inas {IV}, in 2010, 2012, and 2014. {T}he ocean-atmosphere modeling results correspond well with data from three oceanographic cruises around the  island.  {T}he  modeled  wind  correlated  well  with  the  wind  speed  and  direction  values  at  10m,  with  a statistical significance of 95%. {T}he presence of the island modifies the sea surface temperature and surface currents.  {O}n  the  island's  west  side,  ocean  currents  are  weakened  due  to  the  physical  barrier,  and  the  sea surface temperature increases, indicating an island effect. {T}he island effect is also observed when analyzing vertical  sections.  {W}eather  conditions  in  2010  show  that  the  air  temperature  was  higher  than  in  2012  and 2014.  {T}he  atmosphere  also  exhibits  an  island  effect,  with  the  wind  skirting  the  island's  upper  terrain  and weakening on  the  leeward  side.  {T}he  oceanic  part  shows  the  warming  of  the  upper  waters  and  the convergence  of  currents  on  the  island's  west  side.  {M}odeled  ocean  temperatures  underestimate  (~ -0.3  °{C}) observations,  except  to  the  west  of  the  island  (~  +0.3  °{C}),  where  model  temperatures  are  higher than measurements.  {C}alculation  of  the  {FCO}2  bias  (f{CO}2is  the  {CO}2fugacity  with  unit  atm,  and  {FCO}2is  the  {CO}2flux) shows that the model underestimates the measurements by about 20 mmol m-2d-1. {T}he ocean was a source of {CO}2 during the three oceanographic cruise periods.},
  keywords = {{BRESIL} ; {ATLANTIQUE} ; {FERNANDO} {DE} {NORONHA} {ARCHIPEL}},
  booktitle = {},
  journal = {{T}ropical {O}ceanography},
  volume = {50},
  numero = {2},
  pages = {1--33},
  ISSN = {1679-3005},
  year = {2023},
  URL = {https://www.documentation.ird.fr/hor/fdi:010091478},
}