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HURRICANE ETA

HURRICANE ETA

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given in Fig. 1, with the wind and pressure histori es shown in Figs. 2 and 3, respectively. The best track positions and intensities are listed in Table 11. A ridge of high pressure to the north caused the cyclone to move westward over the west-central and western Caribbean Sea for a couple of days, and the depression strengthened into a

  High, Hurricane, Wind

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