#96 Postby Portastorm » Thu Jun 29, 2006 4:56 pm
OK, I'm still struggling with this comparison to Bret. Here is the "synoptic history" about Hurricane Bret in 1999. This is from the National Hurricane Center:
a. Synoptic History
Bret formed as a tropical depression over the Bay of Campeche on 18 August. Both a tropical wave and an upper-level low contributed to the formation of Bret. A tropical wave moved from Africa to the tropical Atlantic Ocean on 5 August. Continuity and soundings from Merida, Mexico place this weak tropical wave in the vicinity of the Yucatan Peninsula on the 18th. The second feature, an upper-level cyclonic circulation, appeared on water vapor imagery over the north central Caribbean moving westward on 15 August. The circulation initiated a thunderstorm complex on the night of the 17th over the Yucatan Peninsula and a weak surface low formed in the same location early on the 18th..
Later on the 18th, the surface low moved over the Bay of Campeche. Early morning visible satellite imagery showed a low level cloud circulation center and, a few hours later, a U.S. Air Force Reserve Unit reconnaissance mission confirmed the existence of a closed circulation. With some deep convection and banding present, the system was upgraded to a tropical depression at 1800 UTC on the 18th over the Bay of Campeche. The best track begins at this time, as shown in Table 1, which is a listing of Bret's best track positions, wind speeds, and central pressures, every six hours. Figure 1 shows a map of this track.
The depression did not strengthen right away due to vertical shear caused by an upper-level trough over the extreme western Gulf of Mexico. But the trough moved away and Bret reached tropical storm strength late on the 19th while beginning to move slowly northward. The vertical shear decreased. Bret rapidly became more organized and then steadily strengthened to a 125-knot category four hurricane on the Saffir/Simpson scale on the morning of the 22nd, while appproaching south Texas coast near Brownsville. Responding to the presence of a weak mid-tropospheric ridge over the northwest Gulf of Mexico and to a mid-tropospheric cyclonic circulation over the Rio Grande valley, Bret turned northwestward and slowed its forward speed down to about 5 knots. The forward speed had earlier been as high as 9 knots.
Bret's center crossed the Texas coast over the central portion of Padre Island, midway between Brownsville and Corpus Christi, at 0000 UTC, 23 August. It had weakened to a category three hurricane with 100 knot winds and a pressure of 951mb by the time of landfall. After moving inland, Bret's movement became more westward with a slow forward speed. Bret continued to weaken as it moved across south Texas and into the high terrain of north central Mexico where it dissipated on the 25th
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