As this wave interacted with a high-pressure system, it gradually organized, becoming a tropical depression near the Bahamas on August 23. Initial forecasts showed the storm tracking harmlessly toward Florida, but subtle shifts in the high-pressure ridge caused the developing system to curve westward, setting the stage for a direct hit on the Gulf.
Hurricane Katrina Path Sea Surface Temperatures and Its Role in the Storm's Devastating Journey
The surge overtopped the levees of New Orleans, submerging roughly 80% of the city in water that often exceeded rooftops. Fueled by sea surface temperatures exceeding 80°F (27°C), the depression exploded into a hurricane and then a major Category 5 storm.
The Devastating Storm Surge While the wind was destructive, the water was the true agent of destruction along the hurricane’s path. It tracked north-northeast through Mississippi and Alabama, causing widespread wind damage and flooding before degenerating into a tropical depression over Tennessee.
Hurricane Katrina Path Sea Surface Temperatures and Storm Intensity
The path served as a stark visual aid, illustrating the vulnerability of the Crescent City and the surrounding wetlands to a major tropical event. The Louisiana Landfall At approximately 6:10 AM local time on August 29, the core of the hurricane made landfall near Buras-Triumph, Louisiana.
More About Hurricane katrina's path
Looking at Hurricane katrina's path from another angle can help expand the discussion and give readers a second clear paragraph under the same section.
More perspective on Hurricane katrina's path can make the topic easier to follow by connecting earlier points with a few simple takeaways.
