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- W2048711936 startingPage "5091" @default.
- W2048711936 abstract "The numerical dynamic model of the advective province of the ocean described in part 1 of this paper was applied to the Gulf of Mexico using three layers. Real data and artificial conditions were used as initial conditions. Realistic forecasts were made covering 4-week periods (672 hours). None showed indication of computational instability. Results show that important variations occur in the Gulf over short time periods. Cyclonic circulations in the northwest and in the Yucatan Current are dynamically required. The major anticyclone in the western Gulf of Mexico is probably a result of external influences." @default.
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- W2048711936 date "1968-08-15" @default.
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- W2048711936 title "Experiments in oceanic forecasting for the advective region by numerical modeling: 2. Gulf of Mexico" @default.
- W2048711936 cites W1982856045 @default.
- W2048711936 doi "https://doi.org/10.1029/jb073i016p05091" @default.
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