Meteorological history | |
---|---|
Formed | August 4,2002 |
Dissipated | August 9,2002 |
Tropical storm | |
1-minute sustained (SSHWS/NWS) | |
Highest winds | 40 mph (65 km/h) |
Lowest pressure | 1007 mbar (hPa);29.74 inHg |
Overall effects | |
Fatalities | 1 direct |
Damage | $200,000 (2002 USD) |
Areas affected | Florida,Alabama,Mississippi,Louisiana,Texas |
IBTrACS | |
Part of the 2002 Atlantic hurricane season |
Tropical Storm Bertha was a minimal tropical storm that made landfall twice along the Gulf Coast of the United States in August 2002. The second tropical storm of the 2002 Atlantic hurricane season,Bertha developed in the northern Gulf of Mexico out of a trough of low pressure that extended into the Atlantic on August 4. It quickly organized and reached tropical storm strength before making landfall on southeastern Louisiana. Bertha turned to the southwest over the state,and re-entered the Gulf of Mexico on August 7. It remained disorganized due to proximity to land,and after making landfall on south Texas,Bertha dissipated on August 9.
Bertha was one of only three tropical cyclones to make landfall on both Louisiana and Texas;the others being Allison in 2001 and Fern in 1971. [1] Heavy surf killed one person in Florida. The storm dropped moderate amounts of rainfall along its path,peaking at over 10 inches (250 mm) in eastern Louisiana and southern Mississippi. Damage was light,totaling to only $200,000 (2002 USD).
A non-tropical trough at the surface extended from the northern Gulf of Mexico across Florida into the western Atlantic Ocean. On August 3, the western portion developed into a low pressure area. The eastern portion slowly organized and ultimately developed into Tropical Storm Cristobal. The low pressure area in the Gulf of Mexico steadily organized, [2] and late on August 4 the circulation was organized enough for the National Hurricane Center to classify it as Tropical Depression Two while located 40 miles (64 km) east of Port Eads, Louisiana. Northeasterly wind shear initially prevented organization of the cloud pattern, [3] though the depression was able to strengthen to become Tropical Storm Bertha about five hours after it formed. [2]
Outflow became much better organized as Bertha became a tropical storm, and well-defined banding features persisted to the north of the storm. Though convection waned, forecasters predicted the friction between land and the warm atmosphere to redevelop more deep convection, potentially resulting in further strengthening. [4] However, the storm failed to intensify, and Bertha made landfall near Boothville, Louisiana as a minimal tropical storm early on August 5. It slowly weakened over the swampy portions of southeastern Louisiana, and degenerated to a tropical depression later on the 5th after crossing Lake Pontchartrain. [2] Initially it was expected that a ridge of high pressure to its north would keep Bertha moving to the west and result in it slowly dissipating. [5] However, it turned to the southwest, and reached the Gulf of Mexico again on August 7. [2] The circulation persisted over land, and Tropical Depression Bertha quickly redeveloped convection. Though the environment was not unfavorable, its proximity to land prevented re-strengthening to tropical storm status. [6] Though the system showed periods of increased organization as it moved southwestward, Bertha remained a weak tropical depression until making landfall on south Texas to the east of Kingsville on August 9. Bertha weakened quickly over land, and dissipated over southern Texas ten hours after making landfall. [2]
The National Hurricane Center issued a tropical storm warning from Pascagoula, Mississippi to the mouth of the Mississippi River as Bertha became a tropical storm. The warning occurred 90 minutes before the storm made landfall. All warnings were discontinued when Bertha weakened to a tropical depression over Louisiana. No watches or warnings were required for Texas, due to the improbability of it re-intensifying. [2]
The National Weather Service advised boats along the Gulf coast to remain at port. The service also issued a coastal flood watch from Alabama through the Florida Panhandle. [7] A flood watch was issued for portions of eastern Louisiana and southwestern Mississippi. [8]
The area of low pressure preceding the development of Bertha produced rough surf and rip currents along the Florida coastline. In Perdido Key State Recreation Area, [2] two children were swimming in an unguarded area when they were swept away by the currents. Their grandfather attempted to rescue them, but drowned in the rough waters. Another family rescued the two children. [9] The large circulation of Bertha produced light rainfall across Florida, [10] with Pensacola and Destin reporting 2.75 inches. [11] Extreme southern portions of Alabama received over 3 inches (76 mm) of rain from the storm, while western Dauphin Island reported over 5 inches (130 mm). [10]
Upon making landfall, Waveland, Mississippi recorded a peak storm surge of 4.12 feet (1.26 m). Sustained winds there peaked at 31 mph (50 km/h), and a peak gust of 41 mph (66 km/h). Tropical Storm Bertha produced moderate to heavy precipitation across southern Mississippi, including a total of 10.25 inches (260 mm) in Pascagoula. [2] In Moss Point, the rainfall resulted in flooding which entered 15 to 20 houses and several cars. The rainfall also flooded roadways and streets. Damage in Mississippi totaled to at least $50,000 (2002 USD, $60,000 2008 USD). [12]
The storm dropped heavy rainfall in Louisiana, which peaked at 10.25 inches (260 mm) in Norwood. Storm tides were generally 1 to 2 feet (0.30 to 0.61 m) above normal, while the mouth of the Bayou Dupre recorded a storm tide of 3.79 feet (1.16 m). [2] The rainfall led to flash flooding in places, and also a few overflowed rivers in St. Tammany Parish. [13] The flooding covered several roadways and bridges, and entered a few businesses and houses in East Feliciana Parish. [14] Damage in Louisiana totaled to $150,000 (2002 USD, $180,000 2008 USD). [15]
In Texas, Bertha produced a storm tide of 3 feet (0.91 m) at Baffin Bay. [16] Only light rainfall occurred in the state, with a few isolated areas receiving over 1 inch (25 mm) of precipitation. [10]
Tropical Storm Allison was a tropical storm that devastated southeast Texas in June of the 2001 Atlantic hurricane season. An arguable example of the "brown ocean effect", Allison lasted unusually long for a June storm, remaining tropical or subtropical for 16 days, most of which was when the storm was over land dumping torrential rainfall. The storm developed from a tropical wave in the northern Gulf of Mexico on June 4, 2001, and struck the upper Texas coast shortly thereafter. It drifted northward through the state, turned back to the south, and re-entered the Gulf of Mexico. The storm continued to the east-northeast, made landfall on Louisiana, then moved across the southeast United States and Mid-Atlantic. Allison was the first storm since Tropical Storm Frances in 1998 to strike the northern Texas coastline.
The 2002 Atlantic hurricane season was a near-average Atlantic hurricane season. It officially started on June 1, 2002, and ended on November 30, dates which conventionally limit the period of each year when most tropical cyclones develop in the Atlantic Ocean. The season produced fourteen tropical cyclones, of which twelve developed into named storms; four became hurricanes, and two attained major hurricane status. While the season's first cyclone did not develop until July 14, activity quickly picked up: eight storms developed in the month of September. It ended early however, with no tropical storms forming after October 6—a rare occurrence caused partly by El Niño conditions. The most intense hurricane of the season was Hurricane Isidore with a minimum central pressure of 934 mbar, although Hurricane Lili attained higher winds and peaked at Category 4 whereas Isidore only reached Category 3. However, Lili had a minimum central pressure of 938 mbar.
Hurricane Danny was the only hurricane to make landfall in the United States during the 1997 Atlantic hurricane season, and the second hurricane and fourth tropical storm of the season. The system became the earliest-formed fifth tropical or subtropical storm of the Atlantic season in history when it attained tropical storm strength on July 17, and held that record until the 2005 Atlantic hurricane season when Tropical Storm Emily broke that record by several days. Like the previous four tropical or subtropical cyclones of the season, Danny had a non-tropical origin, after a trough spawned convection that entered the warm waters of the Gulf of Mexico. Danny was guided northeast through the Gulf of Mexico by two high pressure areas, a rare occurrence in the middle of July. After making landfall on the Gulf Coast, Danny tracked across the southeastern United States and ultimately affected parts of New England with rain and wind.
Tropical Storm Matthew was a weak tropical storm in the 2004 Atlantic hurricane season that made landfall on Louisiana. It was the thirteenth tropical storm of the season and the ninth to affect the United States. It formed over the western Gulf of Mexico on October 8 and struck south-central Louisiana two days later. The combination of the storm and an upper cyclone over the southern Plains brought heavy rains to much of the Gulf Coast, with the highest amounts reported over 15 inches (380 mm) in northern Louisiana. Damage was minimal, totaling $305,000 (2004 USD), and no casualties were reported.
Tropical Storm Fay was the sixth named storm of the 2002 Atlantic hurricane season; it was a moderate tropical storm which caused flooding in parts of Texas and Northern Mexico. It formed from a trough of low pressure that moved south into the Gulf of Mexico, and became stationary. A low pressure center developed along this trough, and on September 5, a Hurricane Hunter aircraft reported that the system had gained sufficient organization to be classified a tropical depression, 95 miles (153 km) southeast of Galveston. The depression drifted south-southwest while strengthening, reaching its peak strength of 60 miles per hour (97 km/h) on the morning of September 6. The system then made an abrupt turn to the west-northwest, and remained steady in strength and course until landfall the next day, near Matagorda. The system weakened rapidly after landfall degenerating into a remnant low on September 8, but the storm's circulation survived for another three days.
Tropical Storm Hanna was a moderately strong tropical storm that affected the Gulf Coast and Southeastern regions of the United States. The ninth tropical cyclone and eighth named storm of the 2002 Atlantic hurricane season, Hanna formed through the complex interaction of a surface trough, a tropical wave, and an upper-level low pressure system, a disturbance in the upper atmosphere. Designated a tropical depression at 0000 UTC on September 12, the storm remained disorganized throughout its duration, though it attained tropical storm status and a peak intensity of 1,001 mbar (29.6 inHg), with winds of 60 miles per hour (100 km/h). Hanna crossed extreme southeastern Louisiana, and made a second landfall along the Alabama–Mississippi border.
Tropical Storm Jerry was a tropical storm that caused severe flooding throughout the southeast United States in August of the 1995 Atlantic hurricane season. Jerry, the tenth tropical storm of the season, formed from a tropical wave that moved off the African coast in early August, which organized into a tropical depression and tropical storm between the Bahamas and Florida later in the month, before striking Florida in the latter part of the month. Its remnant circulation persisted until five days after landfall. The rainfall it produced, amounting to over 12 inches (300 mm) in several locations across Florida, Georgia, and South Carolina, was responsible for $40 million (2005 USD) in damage and 6 deaths. At the time, Jerry was the earliest tenth storm to form in a season on record, until Jose in the 2005 season overtook it. Tropical Storm Jerry was also the first tropical cyclone to make landfall in South Florida since Hurricane Andrew in 1992.
Tropical Storm Bill was a tropical storm that affected the Gulf Coast of the United States in the summer of 2003. The second storm of the 2003 Atlantic hurricane season, Bill developed from a tropical wave on June 29 to the north of the Yucatán Peninsula. It slowly organized as it moved northward, and reached a peak of 60 miles per hour (97 km/h) shortly before making landfall in south-central Louisiana. Bill quickly weakened over land, and as it accelerated to the northeast, moisture from the storm, combined with cold air from an approaching cold front, produced an outbreak of 34 tornadoes. Bill became extratropical on July 2, and was absorbed by the cold front later that day.
Hurricane Fern was the sixth named storm and fourth hurricane of the 1971 Atlantic hurricane season. It formed from a tropical wave which interacted with a large trough of low pressure to form Fern, as well as Hurricane Ginger, Tropical Storm Heidi, and a system later designated as Tropical Depression Sixteen, which moved into South Carolina. Fern crossed southeastern Louisiana as a tropical depression on September 4 before swinging back out over the Gulf of Mexico. Fern reached hurricane status on September 8, reaching a peak intensity of 90 mph (140 km/h) before making landfall near Freeport, Texas, two days later.
The 1987 Gulf Coast tropical storm caused flooding along the Gulf Coast of the United States. The second tropical cyclone and first tropical storm of the 1987 Atlantic hurricane season, it originated from a tropical wave in the Gulf of Mexico, southeast of Texas, on August 9. Initially a tropical depression, the cyclone moved north-northwestward and slightly intensified into a tropical storm later that day. By August 10, it made landfall between Galveston and Beaumont. The system weakened after moving inland and turned towards the east and later southeast. Briefly reemerging over the Gulf on August 15, the depression moved onshore a second time in Florida, before dissipating over eastern Georgia on August 17.
Tropical Storm Dean was a short-lived storm that formed in late July 1995 and lasted into early August. It was the fourth named storm of the 1995 Atlantic hurricane season. It spent most of its life as a tropical depression, and briefly gained tropical storm status before its landfall on the Texas coast on July 30. After landfall, it dissipated over central Texas on August 2. The impacts from Dean were minimal, mainly due to heavy rain in Oklahoma and Texas that caused localized coastal and inland flooding. Two F0 Tornadoes touched down in Texas as a result of Dean's landfall. Also, Twenty families had to be evacuated in Chambers County, due to flooding in the area. One fatality was recorded as a result of flooding in Oklahoma. Several highways were flooded out in Oklahoma, which impeded travel in the state. In addition approximately $500,000 worth of damage was recorded in the aftermath of Dean.
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Hurricane Babe was the second named storm and the first to impact the United States during the inactive 1977 Atlantic hurricane season. Forming out of a tropical wave on September 3, Babe began as a subtropical cyclone in the eastern Gulf of Mexico. The storm gradually intensified as it tracked westward. On September 5, the storm turned north and acquired tropical characteristics. Later that day, Babe intensified into a hurricane and attained its peak strength with winds of 75 mph (120 km/h) and a barometric pressure of 995 mbar. Several hours later, the hurricane made landfall in Louisiana and quickly weakened. By September 6, Babe had weakened to a tropical depression and later dissipated early on September 9 over North Carolina.
Tropical Storm Bonnie was a small and rather weak tropical storm that brought squally weather to the northern Caribbean Sea and Gulf Coast of the United States in July 2010. The third tropical cyclone and second named storm of the 2010 Atlantic hurricane season, Bonnie developed from a tropical wave over the Bahamas on July 22. It strengthened to a tropical storm while crossing the islands, and made landfall on the southeastern coast of Florida the following day. Inland, Bonnie weakened to a tropical depression before entering the Gulf of Mexico, where its surface circulation dissipated on July 24. The remnants of the storm moved ashore between Louisiana and Mississippi early on July 25, prompting severe thunderstorm and tornado warnings in the area.
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