Meteorological history of Hurricane Katrina
was an extremely destructive Category 5 hurricane that affected the majority of the Gulf Coast. Its damaging trek began on August 23, 2005, when it originated as Tropical Depression Twelve near the Bahamas. The next day, the tropical depression strengthened to a tropical storm, and was named Katrina; it proceeded to make landfall on the southern tip of the U.S. state of Florida as a minimal hurricane.
In passing across Florida, Katrina did not attain any more strength but did manage to maintain hurricane status. After passing over Florida, the warm waters of the Gulf of Mexico allowed it to rapidly intensify to the sixth-strongest Atlantic hurricane in recorded history. Afterward, Katrina made landfall as a Category 3 storm near Buras-Triumph, Louisiana, and once more near the Mississippi/Louisiana border. Katrina progressed northward through the central United States and finally dissipated near the Great Lakes on August 31, when it was absorbed by a cold front.
Formation
On August 19, a tropical wave merged with the remnants of Tropical Depression Ten, the surface low of which had dissipated earlier due to the effects of a nearby upper tropospheric trough. On August 23, 2005, at 5:00 p.m. EDT, this system developed into Tropical Depression Twelve over the southeastern Bahamas. While the normal standards for numbering tropical depressions in the Atlantic indicate that the old name/number is retained when a depression dissipates and regenerates, satellite data indicated that a second tropical wave combined with Tropical Depression Ten north of Puerto Rico to form a new, much more advanced system, which was then designated as Tropical Depression Twelve. Simultaneously, the trough in the upper storm weakened, causing the wind shear in the area to relax, thereby allowing the new tropical depression to develop. In a later re-analysis, it was determined that the low-level circulation of Ten had completely detached and dissipated, with only the remnant mid-level circulation moving on and merging with the aforementioned second tropical wave. As a result, the criteria for keeping the same name and identity were not met.First landfall
As the atmospheric conditions surrounding Tropical Depression Twelve were favorable for tropical development, the system began to intensify and was upgraded to Tropical Storm Katrina on the morning of August 24. A burst of convection allowed Katrina to become the fifth hurricane of the 2005 season on August 25, only two hours before it made landfall around 6:30 p.m. EST between Hallandale Beach and Aventura, Florida. Katrina struck the peninsula with winds, and had a well-defined eye on NEXRAD weather radar, which remained intact throughout its passage over Florida. Parts of the Florida Keys experienced tropical storm winds throughout August 26, with the Dry Tortugas briefly experiencing hurricane-force winds.Gulf of Mexico
The initial National Hurricane Center forecasts predicted that Katrina would begin turning northward after landfall, eventually to hit the Florida Panhandle approximately three to four days later. Katrina, however, continued a westerly and west-southwesterly track, which eventually shifted the forecast track westward to New Orleans..
Immediately after the storm entered the Gulf of Mexico, the low wind shear, good upper-level outflow, and the warm sea surface temperatures of the Gulf Loop Current caused Katrina to intensify rapidly. On August 27, the storm was upgraded to Category 3 intensity, becoming the third major hurricane of the season. An eyewall replacement cycle disrupted the intensification of maximum winds for about 18 hours, but almost doubled the radius of the storm. A second period of rapid intensification started by 7:00 p.m. CDT on August 27, and by 12:40 a.m. CDT on August 28, Katrina was upgraded to a Category 4 hurricane with maximum sustained winds of. It became a Category 5 storm by 7:00 a.m. CDT, twelve hours after the beginning of the second round of rapid intensification, and reached its peak intensity at 1:00 p.m. CDT with maximum sustained winds of, gusts of and a central pressure of 902 millibars. The minimum pressure made Katrina, at the time, the fourth-most intense Atlantic hurricane on record. As the hurricane approached New Orleans, the Weather Forecast Office in Slidell, Louisiana issued two strongly worded warnings of the storm's danger.
By the afternoon of August 28, the storm was large enough that some areas of the Gulf Coast were already experiencing tropical storm-force winds. The center of Katrina was about 180 statute miles from the mouth of the Mississippi River, but tropical storm-force winds extended from the center of the storm, and hurricane-force winds extended about 105 miles away. Overnight on August 29, and into the morning of the next day, Katrina quickly weakened as it began to enter another eyewall replacement cycle. The inner eyewall deteriorated before an outer eyewall had fully formed, playing an important role in the weakening. In 18 hours, the hurricane's maximum sustained winds decreased from to. However, storm surge remained high at landfall because large waves greater than in height were generated beforehand, when Katrina was at Categories 4 and 5 on the Saffir–Simpson hurricane scale. The waves then combined with the storm surge of the large Category 3 hurricane.
Second and third landfalls
Katrina made its second landfall at 6:10 a.m. CDT on August 29 as a Category 3 hurricane with sustained winds of near Buras-Triumph, Louisiana. Because Katrina had just weakened from Category 4 and due to the shape of the coastline, sustained Category 4 winds likely existed on land while the eye was over water. At landfall, hurricane-force winds extended from the center, the storm's pressure was, and its forward speed was. As it made its way up the eastern Louisiana coastline, most communities in Plaquemines, St. Bernard Parish, and Slidell in St. Tammany Parish were severely damaged by storm surge and the strong winds of the eyewall, which also grazed eastern New Orleans, causing in excess of $1 billion worth of damage to the city.Original estimates indicated that Katrina had made this landfall as a Category 4 hurricane, with winds; however, as indicated above, the storm weakened just before landfall to Category 3 intensity. The reasons for this weakening are not completely known yet; while the eye-wall replacement cycle played a part, slightly increasing shear, dropping sea-surface temperatures, dry air on the western semicircle of the storm, and interaction with the continental landmass also may have played a role in weakening the cyclone. This follows the trend of previous strong cyclones in the Gulf of Mexico: most cyclones with minimum central pressures of or less have weakened over the 12 hours before making landfall in the Gulf Coast of the United States.
A few hours later, after weakening slightly, Katrina made its third landfall near the Louisiana–Mississippi border with sustained winds and pressure, still at Category 3 intensity. Its minimum pressure at its second landfall was, making Katrina the fourth-strongest hurricane on record to make landfall on the United States, behind Hurricane Michael's 919-millibar reading, Hurricane Camille's reading in 1969, and the 1935 Labor Day Hurricane's record.
Because the storm was so large, highly destructive eye-wall winds and the strong northeastern quadrant of the storm pushed record storm surges onshore, smashing the entire Mississippi Gulf Coast, including towns in Mississippi such as Waveland, Bay St. Louis, Pass Christian, Long Beach, Gulfport, Biloxi, Ocean Springs, Gautier and Pascagoula, and, in Alabama, Bayou La Batre. The surges peaked at in Bay St. Louis, Mississippi, and at as far away as Mobile, Alabama, which saw its highest storm surge since 1917. Storm surge was particularly high due to the hydrology of the region, the hurricane's extreme size, and the fact that it weakened only shortly before landfall. As Katrina moved inland diagonally over Mississippi, high winds cut a swath of damage that affected almost the entire state.
Demise
Katrina maintained hurricane strength well into Mississippi, but weakened thereafter, losing hurricane strength more than inland, near Meridian, Mississippi. It was downgraded to a tropical depression near Clarksville, Tennessee and broke in half. One half continued to race northward, affecting the Central United States along its path, and was last distinguishable in the eastern Great Lakes region on August 31. On August 31, Katrina merged with a frontal boundary and became a powerful extratropical low, causing of rain in 12 hours, as well as gale-force wind gusts from in southeastern Quebec and northern New Brunswick. In the region of Saguenay and Côte-Nord, rain caused breakdowns and failure in roads. The Côte-Nord region was isolated from the rest of Quebec for at least 1 week. The other half of Katrina broke off in the eastern part of the Appalachians, primarily leading to a significant tornado outbreak in the area from central Georgia to central Pennsylvania, killing two people and causing millions of dollars in additional damage.At 11:00 p.m. EDT on August 31, the center of the remnant low of what was Katrina had been completely absorbed by a frontal boundary in southeastern Canada, with no discernible circulation.