@article{fdi:010006286,
  title = {{E}quatorial adjusment in the {E}astern {A}tlantic},
  author = {{M}oore, {D}. and {H}isard, {P}hilippe and {M}c{C}reary, {J}. and {M}erle, {J}acques and {O}'{B}rien, {J}. and {P}icaut, {J}o{\¨e}l and {V}erstraete, {J}ean-{M}arc and {W}unsch, {C}.},
  editor = {},
  language = {{ENG}},
  abstract = {{O}bservations suggest that the annual upwelling event in the {G}ulf of {G}uinea is not associated with changes in the local winds. {A} possible explanation is that a strong upwelling signal, generated by increased westward wind stress in the {W}estern {A}tlantic as an equatorially trapped {K}elvin wave. {T}his explanation is analogous to current theories of {E}l {N}ino in the {P}acific {O}cean. ({R}{\'e}sum{\'e} d'auteur)},
  keywords = {{TEMPERATURE} {DE} {SURFACE} ; {UPWELLING} ; {VENT} ; {TOPOGRAPHIE} {DYNAMIQUE} ; {ATLANTIQUE} {TROPICAL} ; {GOLFE} {DE} {GUINEE}},
  booktitle = {},
  journal = {{G}eophysical {R}esearch {L}etters},
  volume = {5},
  numero = {8},
  pages = {637--640},
  ISSN = {0094-8276},
  year = {1978},
  URL = {https://www.documentation.ird.fr/hor/fdi:010006286},
}