Gilma was a category 1 hurricane (on the Saffir-Simpson Hurricane Scale)
that took a climatological west-northwesterly track over the open waters of
the eastern North Pacific.
a. Synoptic History
The precursor disturbance for Hurricane Gilma was a tropical wave that moved
off the coast of Africa on 20-21 July. The wave quickly lost convection
which it did not regain until it entered the eastern Caribbean on the
28th. The wave moved into the eastern Pacific on 2 August.
Early on the 4th a cloud system center became briefly trackable
about 300 n mi south of Zihuatanejo, Mexico. This center dissipated but a
second one consolidated rapidly late in the day and a tropical depression
formed on the 5th at 0000 UTC, about 250 n mi south of Manzanillo.
The "best track" chart of the tropical cyclone's path is given in
Figure 1,
with the wind and pressure histories shown in
Figure 2 and Figure 3, respectively.
The best track is listed in Table 1.
The depression remained very poorly organized for the next 36 hours and did
not have a very well-defined circulation center while it moved to the
west-northwest, a heading from which the cyclone never deviated very much.
By 1200 UTC on the 5th, the cloud pattern had become better
organized and the cyclone became a tropical storm about 350 n mi south of
Cabo San Lucas. Gilma gradually intensified over the next couple of days and
became a hurricane at 0600 UTC on the 8th about 500 n mi
west-southwest of Cabo San Lucas. Gilma's peak intensity of 70 kt was
reached at 1200 UTC on the 8th as water temperatures under the
cyclone's center fell below about 26C. A smooth decline in intensity ensued
over the next 60 hours, with the system weakening to a tropical depression
at 0000 UTC on the 10th. No significant convection was noted
after about 1800 UTC on the 10th, and the tropical cyclone had
dissipated by 0000 UTC on the 11th about 750 n mi west of
Cabo San Lucas.
Meteorological Statistics
Observations in Gilma (Figure 2 and
Figure 3) were limited to satellite-based Dvorak
technique intensity estimates from the Tropical Analysis and Forecast Branch
(TAFB), the Satellite Analysis Branch (SAB) and the U. S. Air Force Weather
Agency (AFWA). Of note is the relatively large discrepancy between intensity
estimates from the various agencies on the 7th and 8th,
which introduces more than the usual uncertainty regarding the peak intensity
attained by the cyclone.
There were no ship reports of winds of tropical storm force associated with
Gilma.
Casualty and Damage Statistics
There were no reports of damage or casualties associated with Gilma.
Forecast and Warning Critique
There were relatively few verifying forecasts for Gilma (twelve at 12 hours
and only two at 72 hours). Average official track errors for Gilma were 27,
49, 61, 82, and 93 n mi for the 12, 24, 36, 48, and 72 h forecasts,
respectively. These errors are lower than the average official track errors
for the 10-yr period 1990-1999 (37, 69, 101, 132, and 189 n mi,
respectively). Intensity errors were close to or less than the long term
averages.
There were no watches or warnings associated with Gilma.
Table 1.
Best track for Hurricane Gilma, 5-11 August 2000.
Date/Time (UTC) | Position |
Pressure (mb) |
Wind Speed (kt) | Stage |
Lat. (°N) | Lon. (°W) |
05 / 0000 | 15.0 | 105.2 | 1005 | 30 | tropical depression |
05 / 0600 | 15.2 | 106.1 | 1005 | 30 | " |
05 / 1200 | 15.5 | 106.9 | 1005 | 30 | " |
05 / 1800 | 15.8 | 107.8 | 1005 | 30 | " |
06 / 0000 | 16.2 | 108.8 | 1005 | 30 | " |
06 / 0600 | 16.6 | 109.9 | 1005 | 30 | " |
06 / 1200 | 17.0 | 111.0 | 1003 | 35 | tropical storm |
06 / 1800 | 17.4 | 112.0 | 1000 | 45 | " |
07 / 0000 | 17.9 | 113.0 | 995 | 50 | " |
07 / 0600 | 18.2 | 114.1 | 993 | 55 | " |
07 / 1200 | 18.4 | 114.9 | 991 | 60 | " |
07 / 1800 | 18.5 | 115.8 | 991 | 60 | " |
08 / 0000 | 18.7 | 116.7 | 990 | 60 | " |
08 / 0600 | 18.9 | 117.5 | 987 | 65 | hurricane |
08 / 1200 | 19.0 | 118.3 | 984 | 70 | " |
08 / 1800 | 19.3 | 119.1 | 986 | 65 | " |
09 / 0000 | 19.8 | 119.7 | 989 | 60 | tropical storm |
09 / 0600 | 20.2 | 120.2 | 992 | 55 | " |
09 / 1200 | 20.7 | 120.6 | 996 | 45 | " |
09 / 1800 | 21.2 | 121.1 | 999 | 35 | " |
10 / 0000 | 21.7 | 121.6 | 1002 | 30 | tropical depression |
10 / 0600 | 22.0 | 122.2 | 1004 | 30 | " |
10 / 1200 | 22.1 | 122.7 | 1005 | 25 | " |
10 / 1800 | 22.2 | 123.2 | 1006 | 25 | " |
11 / 0000 | 22.3 | 123.6 | 1007 | 25 | " |
11 / 0600 | | dissipated |
|
08 / 1200 | 19.0 | 118.3 | 984 | 70 | minimum pressure |
Figure 1.
Best track positions for Hurricane Gilma, 5-11 August 2000.
Figure 2.
Best track maximum sustained surface wind speed curve for Hurricane Gilma,
5-11 August 2000, and the observations on which the best track curve is
based.
Figure 3.
Best track minimum central pressure curve for Hurricane Gilma, 5-11 August
2000, and the observations on which the best track curve is based.