@inproceedings{fdi:30232,
  title = {{T}he steady state response of indonesian sea to a steady wind field},
  author = {{H}adi, {W}. and {N}uraini, {W}.},
  editor = {},
  language = {{ENG}},
  abstract = {{A} barotropic fluid model based on the vertically integrated equations of motion was used for studying the steady-state response of {I}ndonesian sea to a steady wind field. {U}sing climatological wind field in {I}ndonesia, the model results yield reasonable direction of water transport due to wind. {I}t was also found that direction of water transport vary according to the direction of the wind. ({R}{\'e}sum{\'e} d'auteur)},
  keywords = {{VENT} ; {CIRCULATION} {OCEANIQUE} ; {MODELE} ; {MASSE} {D}'{EAU} ; {MER} {D}'{INDONESIE}},
  numero = {},
  pages = {451--463},
  booktitle = {{W}estern {P}acific international meeting and workshop on {T}oga {C}oare : proceedings},
  year = {1989},
  URL = {https://www.documentation.ird.fr/hor/fdi:30232},
}