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1995 PRELIMINARY
REPORTS |
a. Synoptic HistorySatellite pictures and rawinsonde data show that a tropical
wave emerged from western Africa on 22 September. Three days later, as
the wave neared 30°W longitude, bands of deep convection associated with
the system began to acquire some cyclonic shape and the NHC's Tropical
Analysis and Forecast Branch (TAFB) meteorologist gave the first location
estimate at 0600 UTC 26 September, remarking "potential surface low looking
like it's getting more organized". Twenty-four hours later, TAFB and the
Synoptic Analysis Branch (SAB) gave the initial Dvorak classifications.
By 1800 UTC on the 26th, the cloud structure was strongly indicative of
a low-level circulation and the post-analysis "best track" of Tropical
Depression Sixteen begins at this time over the eastern tropical Atlantic. A mid- to upper-tropospheric trough lay in the path of the
developing tropical cyclone. Southwesterly shearing due to the upper-level
winds ahead of this trough started to affect the depression as early as
27 September. However, these winds were not strong enough to totally offset
the development trend and the depression strengthened into Tropical Storm
Noel around 1200 UTC on the 27th. As the cyclone strengthened into a storm, its motion turned
from west-northwestward to northwestward, due the influence of the above
trough and an accompanying mid- to upper-level low near 28°N 44°W. A northwestward
movement continued until about 1800 UTC on the 28th, when Noel began to
take a more northerly heading. Even though upper-level outflow was being
impeded to the northwest, satellite intensity estimates indicate that
Noel strengthened to a hurricane near 1800 UTC 28 September. Development
was halted after that juncture by increasing upper-level southwesterly
flow. Moving northward to northeastward, Noel maintained minimal hurricane
strength until 30 September, when the center became exposed to the southwest
of the cluster of convection associated with the cyclone. Gradual weakening
took place, and the forward speed slowed to a crawl on 30 September and
1 October. On 2 October, with its maximum winds reduced to 52
mph, Noel moved generally northward at a faster speed. On the 3rd,
the steering of Noel was influenced by a mid- to upper-level cyclone centered
just to the west, and the storm moved north-northwestward for a while. Shearing diminished as Noel came into the area of lighter upper-level
winds near the center of the mid- to upper-level cyclone, and this allowed
the storm to re-strengthen on the 3rd and 4th. By 0000 UTC 5 October,
Noel was again a 75-mph hurricane. The system
maintained this intensity for about 24 hours while moving slowly northeastward
to eastward. The final weakening commenced at 0000 UTC on the 6th, when
Noel's winds dropped to just below hurricane strength. A midlatitude trough
approached the area, causing Noel to move more rapidly, toward the east-northeast
and northeast. Gradually weakening and losing its tropical character as
it approached the Azores, the cyclone was absorbed into a cold front near
0000 UTC 8 October. b. Meteorological Statistics
|
Date/Time (UTC) |
Position | Pressure (mb) |
Wind Speed (mph) |
Stage | |
---|---|---|---|---|---|
Lat. (°N) | Lon. (°W) | ||||
28/1800 | 15.2 | 42.6 | 987 | 75 | Category 1 Hurricane |