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Preliminary Report
Hurricane Hernan
30 September - 4 October 1996

Richard J. Pasch
National Hurricane Center
17 January 1997


PRELIMINARY REPORTS
Unnamed Tropical Storm
Tropical Depression 2-E
Hurricane Alma
Hurricane Boris
Tropical Storm Cristina
Tropical Depression 6-E
Hurricane Douglas
Tropical Storm Elida
Hurricane Fausto
Tropical Storm Genevieve
Hurricane Hernan
Tropical Depression 12-E


[1996 East Pacific Hurricane Season]

Hernan made landfall on the coast of Mexico, between Manzanillo and Puerto Vallarta, as a category one hurricane on the Saffir/Simpson Hurricane Scale.



a. Synoptic History

A tropical wave that emerged from the coast of western Africa in mid-September moved westward across the Atlantic basin during the latter half of the month. Convection associated with the system temporarily increased near the Lesser Antilles on 22 September, and again on 25-27 September, as the wave moved across the western Caribbean Sea and Central America. Deep convection associated with the wave became a little more consolidated near the Gulf of Tehuantepec on the 28th. By 1800 UTC on the 29th, when the wave axis was near 97W, the cloud pattern was sufficiently well-organized that Dvorak classifications on the system were being given by the Tropical Analysis and Forecast Branch (TAFB). Satellite data indicate that Tropical Depression Eleven-E developed from this disturbance a little over 250 n mi south-southeast of Acapulco around 0600 UTC 30 September, as shown in Table 1, the post-analysis "best track". Gradual development continued, and the cyclone became Tropical Storm Hernan about 12 hours later.

Initially, the cyclone was moving westward, but the motion soon became west-northwestward and then northwestward. Early on October 1, Hernan shifted northward, and then north-northeastward. The storm was still in the developing stage and not yet well-organized; thus, part of this displacement was probably related to a reformation of the center. Later on the 1st, Hernan, then better-organized, turned back toward the north-northwest and, on the 2nd, toward the northwest. By 0600 on the 2nd, when the center was nearing the coast and located about 60 n mi south of Lazaro Cardenas, Hernan strengthened into a hurricane. Reflectivity presentations from the Mexican weather service radar located at Cuyutlan (central coast of the State of Colima), at around 1000 UTC on the 2nd, revealed a well-defined, closed eyewall. The maximum intensity of Hernan, 75 knots, is estimated to have occurred around that time.

From 1200 UTC on the 2nd through 0000 UTC on the 3rd, the hurricane moved parallel, but very near, to the coastline. Early on the 3rd, the forward motion slowed to a crawl and the center moved in a small counter-clockwise loop, just offshore. Hernan then responded to a mid- to upper-tropospheric trough over the southwestern United States and moved northward, making landfall near Barra de Navidad, at 1000 UTC 3 October. Since the center had been moving very near to the mountainous landmass of Mexico for about 24 hours prior to landfall, the hurricane had weakened somewhat before the center finally crossed the coast. Hernan weakened to a tropical storm just after landfall. The cyclone moved mostly northward over land, passing just east of Puerto Vallarta while weakening below storm strength by 0000 UTC on the 4th. Although the center briefly moved back out over the waters north of Puerto Vallarta, the system had become so disorganized that it dissipated around 0000 UTC 5 October.

Figure 1 (25K GIF) depicts the best track of Hernan.


b. Meteorological Statistics

Figures 2 (24K GIF) and 3 (27K GIF) are the curves of minimum central sea-level pressure and maximum one-minute average "surface" (10 meters above ground level) wind speed, respectively, as functions of time. Also plotted are the observations on which the curves are based, consisting of Dvorak-technique estimates (from the TAFB, the Synoptic Analysis Branch, and the U.S. Air Force Global Weather Center) using satellite imagery.

There were three ship reports of tropical storm force winds associated with Hernan. The first, at 0600 UTC 1 October, a vessel with unknown call sign, location 15.2°N 100.2°W, wind 090/35 knots, pressure 1008.3 mb. The second, at 1200 UTC 1 October, call sign KLHZ, location 14.7°N 97.1°W, wind 150/35 knots, pressure 1007.8 mb. The third, at 1800 UTC 1 October, call sign MQWA5, location 15.4°N 100.7°W, wind 160/40 knots, pressure 999.1 mb.

No actual measurements of strong winds from land have been received. Local press reports indicate that waves along the coasts of the states of Colima and Jalisco reached 13 feet.


c. Casualty and Damage Statistics

Hernan struck a relatively sparsely-populated area of Mexico. Local press reported at least 100 injuries with 1,000 homes damaged. There was flooding in the coastal town of Melaque, Jalisco. Washouts were reported on Mexico Route 200, the coastal road between Puerto Vallarta and Manzanillo, and on Mexico Route 80, which runs between Melaque and Guadalajara. Telephone service and electricity were disrupted in various locations.


d. Forecast and Warning Critique

Table 2 is a listing of track forecast error statistics for Hernan. Although, the sample size is very small, one can see that the official and model forecasts were generally larger than the NHC's long-term averages for the eastern Pacific. This is typically the case for landfalling storms in that basin. Hernan was correctly forecast to become a hurricane. However, in most cases, the intensity of this tropical cyclone was somewhat underforecast in the NHC advisories.

A tropical storm warning was issued for Mexico from Acapulco to Manzanillo at 1800 UTC 1 October. A hurricane watch was put into effect from Zihuatanejo to Manzanillo at 0300 UTC 2 October. This was changed to a hurricane warning at 0900 UTC 2 October. A tropical storm warning was issued north of Manzanillo to San Blas at 1500 UTC 2 October, and the hurricane warning was extended north of Manzanillo to Cabo Corrientes at 2100 UTC 2 October. Hurricane warnings were extended north of Cabo Corrientes to San Blas and tropical storm warnings were extended north of San Blas to Mazatlan at 0300 UTC 3 October. There was a relatively short lead time, roughly six hours, between the issuance of hurricane warnings and the arrival of the eyewall (not the center) on the coast on 2 October. Hernan's center ultimately crossed the coast (on 3 October) about 13 hours after the issuance of hurricane warnings for the landfall area.


 
Table 1. Best track, Hurricane Hernan, 30 September-4 October, 1996.
Date/Time
(UTC)
Position Pressure
(mb)
Wind Speed
(kt)
Stage
Lat. (°N)Lon. (°W)
30/060012.698.7100430 tropical depression
120012.699.7100330"
180012.9100.7100335 tropical storm
1/000013.4101.5100235"
060014.1101.4100135"
120014.7101.199945"
180015.5101.399550"
2/000016.1101.799255"
060016.9102.398765hurricane
120017.9103.198075"
180018.5103.998170"
3/000018.9104.698565"
060018.7104.998765"
120019.5104.998960tropical storm
180020.1105.099140"
4/000020.7105.199430 tropical depression
060021.1105.699830"
120021.7105.6100225"
180022.0105.5100325"
5/0000     dissipated
 
2/120017.9103.198075 minimum pressure
3/100018.8104.998765 landfall near Barra de Navidad



 
Table 2
Preliminary forecast evaluation of Hurricane Hernan
Heterogeneous sample (Errors in nautical miles for tropical storm and hurricane stages with number of forecasts in parenthesis)
Forecast TechniquePeriod (hours)
1224364872
CLIP 90 (11)156 (9)184 (7)260 (5)429 (1)
GFDI 73 (9)103 (7)117 (6)125 (5)112 (1)
GFDL *112 (4)136 (3)144 (2)162 (2) - (0)
LBAR 79 (11)126 (9)164 (7)233 (5)345 (1)
AVNI 94 (10)126 (8)161 (6)166 (4)174 (1)
BAMD 83 (11)143 (9)216 (7)276 (5)406 (1)
BAMM 75 (11)123 (9)174 (7)220 (5)258 (1)
BAMS 81 (11)143 (9)200 (7)239 (5)329 (1)
P91E 93 (11)151 (9)198 (7)304 (5)536 (1)
NGPI76 (8)108 (7)120 (5)181 (3)- (0)
UKMI80 (9)114 (7)159 (5)260 (3) - (0)
NHC OFFICIAL66 (11)111 (9)143 (7)176 (5) 252 (1)
NHC OFFICIAL
1988-1995 8-year average
39 (2180) 71 (1970) 105 (1752) 139 (1553) 196 (1189)

* GFDL output not available until after forecast issued.



Brian Maher
Jack Beven

Last updated December 28, 1998