Tropical Depression Fourteen developed from a tropical wave that crossed the west coast of Africa on 6 September. The wave was associated with a broad surface circulation almost immediately, and by 8 September the system possessed enough organized convection to be considered a tropical depression about 250 n mi southeast of the southernmost Cape Verde Islands. The cyclone moved slowly to the west-southwest initially, but an upper-level low dropped down to the west of the depression and caused it to accelerate to the north-northwest on 9 September. Under southerly shear, the convection became separated from the circulation center and the circulation began to elongate. The depression dissipated on 10 September over the western Cape Verde Islands.
| Date/Time (UTC) | Position | Pressure (mb) | Wind Speed (kt) | Stage | |
|---|---|---|---|---|---|
| Lat. (°N) | Lon. (°W) |
||||
| 08 / 0600 | 11.6 | 21.7 | 1009 | 25 | tropical depression |
| 08 / 1200 | 11.4 | 22.2 | 1009 | 25 | " |
| 08 / 1800 | 11.2 | 22.6 | 1009 | 25 | " |
| 09 / 0000 | 11.2 | 23.0 | 1008 | 25 | " |
| 09 / 0600 | 11.6 | 23.6 | 1007 | 25 | " |
| 09 / 1200 | 12.4 | 24.4 | 1007 | 30 | " |
| 09 / 1800 | 13.6 | 24.9 | 1007 | 30 | " |
| 10 / 0000 | 14.6 | 25.0 | 1008 | 25 | " |
| 10 / 0600 | 15.3 | 25.1 | 1009 | 25 | " |
| 10 / 1200 | 15.9 | 25.2 | 1010 | 25 | " |
| 10 / 1800 | dissipated | ||||
| 09 / 0600 - 09 / 1800 | 1007 | minimum pressure | |||
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Page last modified: Monday, 07-Feb-2005 16:38:05 UTC