| HOME | ARCHIVES | FORECASTS | IMAGERY | ABOUT TPC | RECONNAISSANCE |



Tropical Cyclone Report
Tropical Storm Olivia
2 - 10 October 2000

Stacy R. Stewart
National Hurricane Center
6 November 2000

Olivia was a tropical storm that formed off the southwest coast of mainland Mexico, and generally tracked west-northwestward and remained over open water. After dissipating as a tropical cyclone, the remnant low-level circulation tracked across central Baja California, northwest Mexico and the desert southwest United States.

a. Synoptic history

Tropical Storm Olivia originated from a tropical wave that emerged from the coast of Africa on 16 September. The wave tracked westward across the tropical North Atlantic with disorganized convection, until 25 September when the wave reached the central Caribbean Sea. While the structure of the wave improved while tracking across the western Caribbean Sea and Central America, the convection remained weak and disorganized. Even after emerging over the eastern North Pacific on 28 September, little thunderstorm activity was associated with the wave until a burst of deep convection developed late on 30 September near the region of maximum vorticity.

The lack of deep convection over the eastern Pacific may have been the result of (1) much of the low-level inflow being drawn into major Hurricane Keith located in the western Caribbean Sea east of Belize and (2) the upper-level outflow from Keith creating northeasterly shear on the pre-Olivia wave. However, by 2345 UTC 30 September, the separation between the wave and Hurricane Keith increased enough to allow sufficient convective banding to develop, and the Tropical Analysis and Forecast Branch (TAFB) began satellite classifications on the system. At 0000 UTC 2 October, the TAFB designated the system as a tropical disturbance with low-level cyclonic winds of 20 to 25 kt, and shortly thereafter the NHC upgraded the disturbance to Tropical Depression Seventeen-E at 1200 UTC. By 0600 UTC 3 October, satellite classifications from both TAFB and the NOAA/NESDIS Satellite Analysis Branch (SAB) indicated the depression had strengthened into Tropical Storm Olivia about 220 n mi south of Manzanillo, Mexico.

Olivia tracked west-northwestward and eventually northwestward away from the west coast of Mexico and reached a peak intensity of 55 kt late on 3 October. Tropical Storm Olivia maintained that intensity for another 36 hours before gradual weakening ensued, apparently due to an increase in the northeasterly shear again created by Hurricane Keith as the latter system moved westward across the Yucatan Peninsula of Mexico and into the Bay of Campeche and extreme southwest Gulf of Mexico. Once Keith moved inland over northeast Mexico and weakened, the northeasterly shear previously caused by Keith's outflow decreased enough to allow Olivia to strengthen back to 55 kt early on 8 October. However, by that time, Olivia had tracked far enough westward over cooler sea-surface temperatures to begin the final weakening phase and eventual demise of the tropical cyclone. Olivia decreased back to tropical depression strength at 0600 UTC 9 October and dissipated over water at 0600 UTC 10 October about 520 n mi west-southwest of the southern tip of the Baja California Peninsula of Mexico.

The remnant low-level circulation of Olivia tracked steadily north and then northeastward, and persisted as a swirl of low clouds until early 11 October when a brief burst of moderate convection developed northeast of the low-level center. However, the new convection was unable to persist near the low-level center due to increasing southwesterly shear ahead of an approaching mid-to upper-level trough from the west. The remnant circulation did eventually make landfall along the west coast of Baja California about midway between Punta Eugenia and Cabo San Lazaro, and tracked across the Gulf of California and into northwest mainland Mexico and the southwest United States. While not classified as a tropical cyclone at landfall, the remnant of Olivia did bring much needed rainfall to the normally arid regions of Baja California, northwest Mexico, and the Desert Southwest U.S. Although not spectacular by most standards, rainfall totals exceeded 3 inches across those areas and produced localized flash flooding.

b. Meteorological statistics

The "best track" of Olivia is given in Table 1 and Figure 1. Figure 2 and Figure 3 show the best track maximum sustained (1 min average) surface (10 m elevation) wind speed and minimum central pressure, as well as the associated observations. These include Dvorak satellite technique position and intensity estimates from the TAFB, the SAB, and the Air Force Weather Agency (AFWA).

c. Casualty and Damage Statistics

Olivia developed well offshore the west coast of mainland Mexico and remained well to the south of Baja California. There were no reports of tropical storm force winds. Olivia had no direct effect on any land areas and no reports of damage or casualties were received by the National Hurricane Center.

d. Forecast and Warning Critique

NHC official average track forecast errors for Olivia were 33, 51, 70, 93, and 133 n mi at 12 (23 cases), 24 (21 cases), 36 (19 cases), 48 (17 cases) and 72 h (13 cases), respectively. These errors are considerably smaller than the 1990-1999 average of 37, 69, 101, 132, and 189 n mi. A few of the objective aids had slightly lower forecast errors than the official forecast at 12, 24, and 36 h, whereas the official forecast errors were considerably better than most of the objective aids at 48 and 72 h, especially at 72 h where the GFDL, NOGAPS, and UKMET models had errors of 180, 170, and 175 n mi, respectively.

NHC intensity forecast errors were near the 1990-1999 average at 12 and 24 h and worse than the average at 36, 48, and 72 h. There was a negative bias (underforecast) during the first 36 hours as Olivia was strengthening and a positive bias (winds overforecast) in all of the forecasts afterwards, but especially in the 36, 48, and 72 h forecasts. The overforecasts of intensity were apparently due to the underestimation of the effects of vertical shear caused by Hurricane Keith's outflow, even though Keith remained located well to the northeast of Olivia over the western Caribbean Sea and southwest Gulf of Mexico.

There were no tropical cyclone watches or warnings associated with Olivia.



 
Table 1. Best track, Tropical Storm Olivia, 2-10 October 2000.
Date/Time
(UTC)
Position Pressure
(mb)
Wind Speed
(kt)
Stage
Lat. (°N)Lon. (°W)
02 / 120015.3103.11006 25tropical depression
02 / 180015.3103.61005 30 "
03 / 000015.3103.71005 35 tropical storm
03 / 060015.3103.8100335"
03 / 120015.3103.91002 40"
03 / 180015.4104.5 994 55"
04 / 000015.5104.8 994 55"
04 / 060015.7105.2 994 55"
04 / 120015.8105.5 994 55"
04 / 180015.9105.9 994 55"
05 / 000016.0106.5 994 55"
05 / 060016.0107.0 994 55"
05 / 120015.9107.6994 50"
05 / 180015.8108.0100050"
06 / 000015.7108.4100045"
06 / 060015.6108.7100235"
06 / 120015.5109.1100145"
06 / 180015.6109.5100345"
07 / 000015.9110.0100245"
07 / 060016.1110.6100045"
07 / 120016.5111.399745"
07 / 180016.9111.999445"
08 / 000017.4112.599750"
08 / 060017.8113.3100055"
08 / 120018.1114.0100050"
08 / 180018.5114.9100040"
09 / 000018.9115.7100435"
09 / 060019.4116.6100630tropical depression
09 / 120019.9117.4100630"
09 / 180020.3117.8100630"
10 / 000020.7118.3100725"
10 / 060021.0118.7100820"
 
03 / 180015.4104.5 99455minimum pressure

Figure 1. Best track for Tropical Storm Olivia, 2-10 October 2000.

Figure 2. Best track maximum sustained 1-minute 10 meter wind speed curve for Tropical Storm Olivia, 2-10 October 2000.

Figure 3. Best track minimum central pressure curve for Tropical Storm Olivia, 2-10 October 2000.



nhcwebmaster

Last updated January 31, 2001