Tropical Cyclone Report
Tropical Storm Blas
11 - 15 July 2004
Richard J. Pasch
National Hurricane Center 8 September 2004
Blas was a large tropical storm whose
center remained at sea. Its outer bands produced gusty winds over
extreme southern Baja California.
a. Synoptic History
A tropical wave emerged from western Africa
on 1 July. This wave was accompanied by a large swirl of low clouds
over the far eastern tropical Atlantic, but the system generated
little deep convection as it traversed the tropical Atlantic and
Caribbean Sea. The wave crossed Central America on 8 July, and over
the next several days deep convection increased and slowly became
organized to the south of Mexico. The pace of development increased
around 0600 UTC 12 July, when the first Dvorak classification was
made for the system. By 1200 UTC that day, the organization and
amount of deep convection was sufficient to designate the system as
a tropical depression. Banding features became more pronounced
during the day, and it is estimated that the tropical cyclone
strengthened into Tropical Storm Blas by around 1800 UTC that
day.
The "best track" chart of the tropical
cyclone's path is given in Figure 1. On 12-13 July, Blas moved
northwestward at a relatively fast forward speed of 15-18 kt, on
the southwest side of a mid-level anticyclone centered over the
southwestern United States. The storm reached its estimated peak
intensity of 55 kt around 1200 UTC 13 July, at which time it
exhibited a large convective overcast with very cold cloud tops.
Thereafter, deep convection decreased and Blas gradually weakened
due to cooler sea-surface temperatures. The weakening storm turned
toward the west-northwest on 14 July. Although the circulation
remained large and well-defined, cool waters continued to take
their toll on Blas and the cyclone weakened to a tropical
depression by 1800 UTC 14 July. Blas degenerated to a large remnant
low around 0600 UTC 15 July which moved generally
west-northwestward for a couple of days while continuing to slowly
spin down. As its forward speed slowed to a drift, the remnant low
turned northward, then northeastward on 18 July. Early on 19 July,
the low turned eastward and dissipated well to the west of central
Baja California.
b. Meteorological Statistics
The best track positions and intensities
for Blas are listed in Table 1, and the wind and pressure histories
are shown in Figure 2 and Figure 3,
respectively. Observations in 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 a few estimates based on QuikSCAT data
(indicated as "Surface" observations in Figure 2). Because Blas had a
broad circulation and lacked a tight inner core structure, the
estimated minimum central pressures in the best track were set
slightly lower than those given by the standard Dvorak
wind-pressure relationship.
Blas was a larger than normal-sized
tropical cyclone. Based on QuikSCAT data and a few ship
observations, tropical storm force winds extended about 200 n mi to
the northeast and northwest of the center by 0000 UTC 13 July. Even
though Blas's center remained well offshore of Baja California,
strong gusty winds of the storm's outer circulation affected the
extreme southern Baja California peninsula. On 13 July, an
automated station just north of Cabo San Lucas at an elevation of
225 m above sea level reported a maximum sustained wind of 41 kt at
1630 UTC and a peak gust of 57 kt at 1750 UTC. A ship with call
sign ELYS4 at 22.2ºN 113.6ºW reported winds of 090/33 kt
and a pressure of 1006.0 mb at 0600 UTC 14 July
c. Casualty and Damage Statistics
There were no reports of damage or
casualties associated with Blas.
d. Forecast and Warning Critique
Blas was a tropical cyclone for only 60
hours so there are too few forecasts to produce meaningful
verification statistics. Although the direction of motion was
generally well predicted, the early track forecasts had a slow
bias. This resulted in some overprediction of the intensity, since
the storm reached cooler waters sooner than expected.
Table 1: Best track for Tropical Storm
Blas, 11-15 July 2004.
Date/Time (UTC) | Position | Pressure (mb) | Wind Speed (kt) | Stage |
Lat. (°N) | Lon. (°W) |
12 / 1200 | 14.6 | 105.5 | 1006 | 30 | tropical
depression |
12 / 1800 | 15.5 | 106.8 | 1002 | 35 | tropical storm |
13 / 0000 | 16.4 | 108.0 | 997 | 45 | " |
13 / 0600 | 17.3 | 109.3 | 994 | 50 | " |
13 / 1200 | 18.4 | 110.8 | 991 | 55 | " |
13 / 1800 | 19.6 | 112.2 | 994 | 50 | " |
14 / 0000 | 20.7 | 113.7 | 997 | 45 | " |
14 / 0600 | 21.5 | 115.1 | 999 | 40 | " |
14 / 1200 | 22.1 | 116.6 | 1002 | 35 | " |
14 / 1800 | 22.5 | 117.9 | 1004 | 30 | tropical
depression |
15 / 0000 | 22.9 | 119.2 | 1005 | 30 | " |
15 / 0600 | 23.2 | 120.4 | 1006 | 30 | remnant low |
15 / 1200 | 23.4 | 121.4 | 1007 | 25 | " |
15 / 1800 | 23.6 | 122.3 | 1008 | 25 | " |
16 / 0000 | 23.8 | 123.3 | 1008 | 25 | " |
16 / 0600 | 24.0 | 124.5 | 1008 | 25 | " |
16 / 1200 | 24.1 | 125.5 | 1008 | 20 | " |
16 / 1800 | 24.2 | 126.3 | 1008 | 20 | " |
17 / 0000 | 24.4 | 127.0 | 1009 | 20 | " |
17 / 0600 | 24.8 | 127.5 | 1009 | 20 | " |
17 / 1200 | 25.2 | 127.8 | 1009 | 20 | " |
17 / 1800 | 25.6 | 128.1 | 1010 | 15 | " |
18 / 0000 | 26.0 | 128.3 | 1010 | 15 | " |
18 / 0600 | 26.4 | 128.4 | 1011 | 15 | " |
18 / 1200 | 26.7 | 128.2 | 1012 | 15 | " |
18 / 1800 | 26.9 | 127.9 | 1013 | 15 | " |
19 / 0000 | 26.9 | 127.6 | 1014 | 15 | " |
19 / 0600 | 26.9 | 127.3 | 1015 | 15 | " |
19 / 1200 | | | | | dissipated |
13 / 1200 | 18.4 | 110.8 | 991 | 55 | minimum pressure |
Figure 1:
Best track positions for
Tropical Storm Blas, 11-15 July 2004.
Figure 2:
Selected wind observations and best
track maximum sustained surface wind speed curve for Tropical Storm
Blas, 11-15 July 2004.
Figure 3:
Selected pressure observations
and best track minimum central pressure curve for Tropical Storm
Blas, 11-15 July 2004.
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