Skip Navigation Links 
NOAA logo - Click to go to the NOAA homepage National Weather Service   NWS logo - Click to go to the NWS homepage
National Hurricane Center / Tropical Prediction Center
Local forecast by
"City, St" or "ZIP" is the U.S. Government's official Web portal to all Federal, state and local government Web resources and services.

Tropical Cyclone Report

Tropical Storm Matthew

8 - 10 October 2004

Lixion A. Avila
National Hurricane Center
27 October 2004

Matthew made landfall on the Louisiana coast as a tropical storm with 35 kt winds.

a. Synoptic History

The origin of Matthew can be traced to a tropical wave that moved across the west coast of Africa on 19 September. The wave was very difficult to track between Africa and the Lesser Antilles because its close proximity to Tropical Storm Lisa and another large disturbance in the tropical Atlantic. The wave crossed the Lesser Antilles on 29 September and began to interact with a westward moving upper-level low. Cloudiness and showers gradually increased as the wave moved very slowly westward, trailing the upper-level low. The shower activity associated with the wave reached the Bay of Campeche on 5 October and gradually became better organized while moving little. An upper-level ridge became established over the convection and surface pressures began to fall in the area. On 7 October, data from a reconnaissance aircraft indicated a broad area of low pressure had formed just east of Tampico, Mexico, accompanied by light winds. The system continued to become better organized while moving little, and it is estimated that a tropical depression formed at 1200 UTC 8 October about 180 n mi southeast of Brownsville Texas. By 1800 UTC that day the cyclone strengthened into Tropical Storm Matthew. Initially, the cyclone moved toward the east and east-northeast, but then gradually turned to the northeast and north steered by a large mid- to upper-level low over western Texas. It is estimated that Matthew reached its peak intensity of 40 knots and a minimum pressure of 997 mb at 1800 UTC 9 October. Matthew's center made landfall just west of Cocodrie, Louisiana about 1100 UTC 10 October. Maximum estimated winds were then 35 knots. Thereafter, Matthew weakened to a depression and became an extratropical low. It continued moving northward and was absorbed by a frontal system at 1200 UTC 11 October.

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 positions and intensities are listed in Table 1.

b. Meteorological Statistics

Observations in Matthew (Figure 2 and Figure 3) include 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), as well as flight-level observations from flights of the 53rd Weather Reconnaissance Squadron of the U. S. Air Force Reserve Command. Microwave satellite imagery from NOAA polar-orbiting satellites, the NASA Tropical Rainfall Measuring Mission (TRMM), the NASA QuikSCAT, and Defense Meteorological Satellite Program (DMSP) satellites were also useful in tracking Matthew.

Table 2 shows selected surface observations including reports from southern Louisiana of heavy rainfall. The maximum rainfall was reported at Reserve in St. John Parish with 16.23 inches.

c. Casualty and Damage Statistics

One tornado briefly occurred near Golden Meadow, damaging the roof of a trailer. In Terrebonne Parish about 20 homes were flooded by the combination of rains and storm surge. There was a report of a 5.85 ft surge at Frenier as indicated in Table 2. According to local newspapers, Grand Isle suffered extensive beach front erosion. There were no known deaths or injuries.

d. Forecast and Warning Critique

Matthew was a short-lived tropical cyclone and there were only a few forecasts to verify. The few track forecasts produced errors are comparable to the average official track errors for the 10-yr period 1994-2003. The average official intensity errors were smaller than the average official intensity errors over the same period.

A strong pressure gradient prevailed over the northeastern Gulf of Mexico and produced gale force winds in that area during the formation of Matthew. As the circulation of the tropical cyclone headed for the coast, a tropical storm warning was issued from the Alabama-Florida border westward to Intracoastal City, Louisiana at 2100 UTC 9 October. The tropical storm warning replaced the existing gale warning about 15 hours before the poorly-defined center of Matthew crossed the Louisiana coast. The warning was discontinued at 1500 UTC 10 October.

Table 1: Best track for Tropical Storm Matthew, 8-10 October, 2004.
Wind Speed
 08 / 1200 24.0 95.4 1007 30 tropical depression
 08 / 1800 24.1 94.2 1004 35 tropical storm
 09 / 0000 24.6 93.7 1000 40 "
 09 / 0600 25.3 93.2 1002 35 "
 09 / 1200 26.3 92.8 1002 35 "
 09 / 1800 26.8 92.0 997 40 "
 10 / 0000 27.3 91.4 998 40 "
 10 / 0600 28.1 91.2 999 40 "
 10 / 1200 29.4 90.9 1000 30 tropical depression
 10 / 1800 30.4 90.9 1002 25 "
 11 / 0000 32.0 91.0 1003 25 extratropical
 11 / 0600 33.6 91.9 1005 20 "
 11 / 1200     Absorbed by front
 10 / 1100 29.2 91.0 999 35 Landfall near Cocodrie, LA.
 09 / 1800 26.8 92.0 997 40 minimum pressure

Table 2: Selected surface and coastal observations for Tropical Storm Matthew, 8-10 October, 2004.
Maximum Surface Wind Speed
Gust (kts)
(storm total)
New Orleans Lakefront Airport10/1205 1003.7 10/1306 33 41   4.06 
BURLI (CMAN)10/1200 1004.0 10/0940 42 48    
Grand Isle GDIL1 (CMAN)10/1100 1002.8 10/0927  40 3.61   
Lumcon10/1000 1001.7 10/0200  34    
LSU Agricultural Stn. Citrus  10/1506  38   5.47 
Tambour Bay10/1000 999.7       
Cocodrie     3.7   
NWS Mandeville     5.3   
NWS Frenier     5.85   
Slidell KASD       5.16 
Baton Rouge KBTR       7.42 
New Orleans KMSY       7.50 
Galliano       14.28 
Thibodaux       9.43 
LSU Agricultural Stn Sugarcane       13.02 
Houma       8.86 
Paradis       8.68 
Reserve       16.23 
aDate/time is for sustained wind when both sustained and gust are listed.
bExcept as noted, sustained wind averaging periods for C-MAN and land-based ASOS reports are 2 min; buoy averaging periods are 8 min.
cStorm surge is water height above normal astronomical tide level.
dStorm tide is water height above National Geodetic Vertical Datum (1929 mean sea level).

Best track positions for Tropical Storm Matthew

Figure 1: Best track positions for Tropical Storm Matthew, 8-10 October, 2004.

Selected wind observations and best track maximum sustained surface wind speed curve for Matthew

Figure 2: Selected wind observations and best track maximum sustained surface wind speed curve for Matthew, 8-10 October, 2004. Aircraft observations have been adjusted for elevation using 80%, reduction factors for observations from 1500 ft or less.

Selected pressure observations and best track minimum central pressure curve for Tropical Storm Matthew

Figure 3: Selected pressure observations and best track minimum central pressure curve for Tropical Storm Matthew, 8-10 October, 2004.

Tropical Cyclone, Tropical Weather, & TPC Information Topics:
Storm Information, Hurricane Awareness, Historical Information,
Tropical Analysis and Forecasting Branch, About Us, Contact Us

NOAA/ National Weather Service
National Centers for Environmental Prediction
National Hurricane Center
Tropical Prediction Center
11691 SW 17th Street
Miami, Florida, 33165-2149 USA
Privacy Policy
About Us
Career Opportunities
Page last modified: Tuesday, 15-Mar-2005 16:06:17 EST