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2000 PRELIMINARY
REPORTS |
Ernesto was a minimal tropical storm that moved across the tropical Atlantic Ocean for a few days without affecting land. a. Synoptic HistoryErnesto formed from a tropical wave that moved from Africa to the eastern tropical Atlantic Ocean on 28 August. Moving west-northwestward, the wave showed signs of a weak low-level circulation on satellite imagery as early as the 29th, while located a few hundred nautical miles south of the Cape Verde Islands. By 1 September, when the wave was midway between Africa and the Lesser Antilles, there was sufficient convection and evidence of a low-level circulation to identify the system as the eighth tropical depression of the season. The system moved toward the west-northwest at 14 to 17 mph from the 1st to the 3rd, under the influence of a westward building subtropical ridge to its north. It became a 40-mph tropical storm, even though rather strong southerly vertical wind shear was evident. This shear was the result of an upper low to the northwest of the storm. This upper low retreated westward as the storm advanced and continued to produce strong shear that prevented further strengthening and caused Ernesto to lose its low-level circulation on the 3rd while centered about 250 nautical miles northeast of the northern Leeward Islands. The remnant clouds moved northward and merged with a frontal cloud system in the north Atlantic over the next several days.
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Date/Time (UTC) |
Position | Pressure (mb) |
Wind Speed (mph) |
Stage | |
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Lat. (°N) | Lon. (°W) | ||||
03/0000 | 18.2 | 53.6 | 1008 | 40 | Tropical Storm |