@inproceedings{fdi:30231,
  title = {{A} new ocean {GCM} for tropical ocean and {ENSO} studies},
  author = {{G}ent, {P}.{R}.},
  editor = {},
  language = {{ENG}},
  abstract = {{A} new reduced gravity, primitive equation model of the upper equatorial ocean has been developped by {G}ent and {C}ane (1989). {I}t has been configured to simulate the annual cycle in the tropical {P}acific ocean. {I}t is forced by the monthly winds from {R}asmusson and {C}arpenter (1982) and a new heat flux formulation from {S}eager et al. (1988). {T}he coefficients of vertical eddy viscosity and conductivity depend upon the {R}idcharson number of the flow. {W}ith this mixing a deep warm pool form in the western {P}acific, increasing the west-east gradient of the thermocline and equatorial undercurrent. {T}he model has been diagnosed as to what factors maintain this deep warm pool. ({R}{\'e}sum{\'e} d'auteur)},
  keywords = {{CIRCULATION} {OCEANIQUE} ; {FLUX} {THERMIQUE} ; {MODELISATION} ; {PACIFIQUE} {TROPICAL} {OUEST}},
  numero = {},
  pages = {445--450},
  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:30231},
}