Tropical Storm Barry (2007)

Last updated
Map key
  Tropical depression (≤38 mph, ≤62 km/h)
  Tropical storm (39–73 mph, 63–118 km/h)
  Category 1 (74–95 mph, 119–153 km/h)
  Category 2 (96–110 mph, 154–177 km/h)
  Category 3 (111–129 mph, 178–208 km/h)
  Category 4 (130–156 mph, 209–251 km/h)
  Category 5 (≥157 mph, ≥252 km/h)
  Unknown
Storm type
Disc Plain black.svg Tropical cyclone
Solid black.svg Subtropical cyclone
ArrowUp.svg Extratropical cyclone, remnant low, tropical disturbance, or monsoon depression

By late on May 29, a weak trough over the Yucatán Peninsula produced a small area of convection over the Yucatán Channel. [1] Convection increased in association with the trough, and the next day a broad envelope of cyclonic turning developed within the system. By May 30, the moisture from the trough extended from Nicaragua through the southeastern Gulf of Mexico, with the greatest area of convection near Cuba. [2] A westward moving tropical wave spawned a broad area of low pressure on May 30, and by May 31, a circulation had developed within the system to the southeast of Cozumel, Mexico. The low moved north-northeastward, [3] and gradually became better organized despite high amounts of vertical wind shear. [4] The deep convection became more concentrated near the center, and it is estimated the system developed into a tropical depression at 12:00  UTC on June 1, just to the northwest of the western tip of Cuba. Operationally, the system was not classified until eleven hours later. [3]

Animated radar image from Tampa of Tropical Storm Barry passing through Florida on June 2 TS Barry 2007 Tampa radar.gif
Animated radar image from Tampa of Tropical Storm Barry passing through Florida on June 2

The depression developed a large area of squalls, and organized enough to warrant a Hurricane Hunters flight into the area. [5] The plane reported flight level winds of 60 mph (97 km/h) and a central pressure of 1000  mbar near the increasingly well-defined low-level circulation. Initially it maintained characteristics of both a tropical and subtropical cyclone, although deep convection continued to organize near the center; based on the observations, the National Hurricane Center initiated advisories on Tropical Storm Barry at 21:00  UTC on June 1, while the storm was centered about 235 miles (378 km) west of Key West, Florida. [6] Embedded within the southwesterly flow ahead of an approaching mid-level trough, it tracked quickly northward, [6] and early on June 2, Barry attained peak winds of 60 mph (97 km/h), with a minimum central pressure of 997 millibars (29.4 inHg). [3]

Shortly after reaching peak intensity, strong wind shear removed most of the deep convection; the cloud pattern consisted of an exposed yet well-defined center surrounded by a curved convective band extending from Cuba along the eastern Gulf of Mexico. [7] The center became elongated and weakened as it accelerated northeastward, and at 14:00 UTC on June 2, Barry made landfall near Tampa, Florida, as a weakening tropical depression. [8] As the system continued inland, it rapidly lost tropical characteristics, and later that day the National Hurricane Center discontinued advisories on Barry, while it was located over northeastern Florida. [9] The extratropical remnants strengthened, as the system continued northeastward, and on June 3, the storm moved ashore along the coast of South Carolina. [10] Spiral bands developed to the north of the system as it moved up the coast, and a large plume of moisture extended well ahead of the low-level circulation. [11] At 00:00 UTC on June 4, Barry's extratropical remnants reached an extratropical peak intensity of 990 millibars (29 inHg). [3] Late on June 4, the extratropical remnant entered New England, [12] and late on June 5, the remnants of Barry were absorbed by a larger extratropical cyclone near the border between the U.S. state of Maine and the Canadian province of Quebec. [3]

Preparations

Tropical Depression Barry shortly after landfall in Florida on June 2 TD Barry.jpg
Tropical Depression Barry shortly after landfall in Florida on June 2

Coinciding with its classification as a tropical storm, the National Hurricane Center issued a tropical storm warning for the west coast of Florida from Bonita Beach through Keaton Beach, with a tropical storm watch declared from Keaton Beach northward to Saint Marks. [13] An inland tropical storm warning was also issued for non-coastal and non-tidal areas of Charlotte, Citrus, DeSoto, Hardee, Hernando, Highlands, Lee, Levy, Manatee, Pasco, Pinellas, Polk, Sarasota, and Sumter counties. The passage of the storm resulted in an increased threat for rip currents, with officials recommending that swimmers stay out of the water until the storm leaves the area. [14] A tornado watch was also posted for the southern portion of the state, though was dropped after the storm weakened. [15]

After becoming an extratropical cyclone, local National Weather Service offices issued flood watches for portions of South Carolina, much of eastern North Carolina, southeastern Virginia, and southeastern Maryland. [10] Later, flood and flash flood watches were issued for southeast Pennsylvania, northern Delaware, northern New Jersey, east-central New York, and southern New England. [11] Wind and lake wind advisories were posted in parts of Georgia. [16]

Impact

Rainfall Summary for Tropical Storm Barry Barry 2007 rainfall.gif
Rainfall Summary for Tropical Storm Barry

Caribbean

In El Salvador, the precursor trough produced about 2.76 inches (70 mm) of rainfall in about ten hours. [17]

The precursor system dropped heavy rainfall across western Cuba, peaking at 12.0 inches (300 mm) in Sancti Spíritus Province. [3] Several other locations recorded over 4 inches (100 mm) of precipitation, which caused flooding along rivers and low-lying areas. The city of Guane was isolated after flooding cut off communications. In total, more than 2,000 people were evacuated due to the threat for flooding. Additionally, the precursor disturbance spawned four tornadoes in Pinar del Río Province; the tornadoes injured three people and damaged fifty-five houses, of which four collapsed. [18]

United States

Florida

Barry dropped moderate to heavy rainfall across Florida, peaking at 6.99 inches (178 mm) at Palm Beach International Airport; several other locations reported over 3 inches (76 mm). [10] The rainfall alleviated persistent drought conditions [15] and assisted in combating severe wildfires across the state. [19] In Brevard County, the rainfall closed a portion of Eau Gallie Boulevard after a large sinkhole developed. Several other roads across the area were flooded, [20] and on Interstate 95 near Lake Worth, a sinkhole closed two lanes of traffic. [21] Wet roads caused several traffic accidents across the state; in both Brevard and Volusia counties, a motorist was killed from an accident. On Interstate 4, a tractor trailer led to disruptions near Orlando after it crashed into a guardrail. [22]

Tropical Storm Barry
Barry 2007-06-01 1650Z.jpg
Tropical Storm Barry shortly after being classified on June 1
Rainfall maxima by state [23]
LocationPeak
inchmm
West Palm Beach, Florida 6.99178
Mount Vernon, Georgia 8.00203
Near Hardeeville, South Carolina 6.12156
Fuquay-Varina, North Carolina 3.7394.7
Pennington Gap, Virginia 3.7595.3
Frostburg, Maryland 1.7043.2
Dover, Delaware 1.5439.1
Philadelphia, Pennsylvania 1.6642.2
Absecon, New Jersey 4.50114
Central Park, New York 3.9199.3
Berlin, Connecticut 2.9073.7
Taunton, Massachusetts 3.1981.0
Burrillville, Rhode Island 3.1078.7
Newmarket, New Hampshire 2.7569.9
Saco, Maine 2.6467.1

The storm produced heavy surf along the western coastline, as well as a storm tide of 4.78 feet (1.46 m) at Clearwater Beach. The wave action caused minor beach erosion, with 50–60 feet (15–18 m) of sand washed away at Bradenton Beach. The increased ocean action caused minor flooding along several roads in the Tampa Bay area, [24] which trapped some automobile travelers. [25] At Indian Shores, a woman died after sustaining injuries from the rough surf. [24]

High winds across the state included a report of 47 mph (76 km/h) near the state's southeastern coastline. [26] The winds downed some trees and resulted in power outages, [27] and one person in Carrolwood was injured after a tree fell onto a house. [24] The storm spawned several tornadoes in the southern portion of the state, some of which damaged fences and power lines. One possible tornado in Goulds left about 2,000 people without power after it knocked down a power line. [15] Another tornado near Miami damaged a few homes and trees. [28]

Elsewhere

Minor street flooding from Barry in Florida Tropical Storm Barry.jpg
Minor street flooding from Barry in Florida

Rainfall in Georgia peaked at 8 inches (200 mm) in Mount Vernon. [11] The precipitation assisted firefighters in combating wildfires in the southern portion of the state, which gave thousands of workers a brief respite after they had fought the fires daily for over a month. [29] The rainfall caused some minor flooding, and in Savannah a few minor traffic accidents occurred. [30] Gusty winds blew down trees and power lines, and along the coast, rough surf was reported. [31] Heavy rainfall from the storm spread across much of the East Coast of the United States. State totals peaked at 6.12 inches (155 mm) near Hardeeville, South Carolina, [11] 3.73 inches (95 mm) in Fuquay-Varina, North Carolina, and 3.75 inches (95 mm) near Pennington Gap, Virginia. [23] High winds also occurred in South Carolina. [31]

The extratropical remnants of Barry produced gusty winds along the Atlantic coastline which peaked at 60 mph (97 km/h) near Charleston, South Carolina. [10] Around 200 houses in Craven County, North Carolina, were without power after winds downed a power line. [32] In North Carolina, adverse conditions from the storm delayed an elimination baseball game between the East Carolina University and Western Carolina University teams. [33] In southeastern Virginia, the remnants of Barry caused over 60 traffic accidents, which resulted in 10 injuries. [34] Rough seas off of Cape Fear left a sailboat containing three people requiring rescue from the Coast Guard. [35] Rainfall extended into the Mid-Atlantic states through New England, with 4.50 inches (114 mm) reported at Absecon, New Jersey, 3.91 inches (99 mm) recorded near Central Park, New York, and 3.19 inches (81 mm) at Taunton, Massachusetts. [23] The remnants of Tropical Storm Barry contributed to heavy rainfall and flooding in the Finger Lakes region of New York State. Roads and several driveways were washed out. [36] Flash flooding was also reported in southeast New York, and high wind gusts caused sporadic tree damage. [37] In New Jersey, northeast onshore flow associated with the remnants of Barry produced high tides and minor coastal flooding. [38]

See also

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References

  1. Waddington (2007-05-29). "May 29 Tropical Weather Discussion". National Hurricane Center. Retrieved 2007-06-01.[ permanent dead link ]
  2. John Cangialosi (2007). "May 30 Tropical Weather Discussion". National Hurricane Center. Retrieved 2007-06-01.[ permanent dead link ]
  3. 1 2 3 4 5 6 Lixion Avila (2007). "Tropical Storm Barry Tropical Cyclone Report" (PDF). National Hurricane Center. Retrieved 2007-06-22.
  4. John Cangialosi (2007-05-31). "May 31 Tropical Weather Discussion 17z". National Hurricane Center. Retrieved 2007-06-01.[ permanent dead link ]
  5. Lixion Avila (2007-06-01). "June 1 Tropical Weather Outlook 15z". National Hurricane Center. Retrieved 2007-06-01.[ permanent dead link ]
  6. 1 2 Lixion Avila (2007-06-01). "Tropical Storm Barry Discussion One". National Hurricane Center. Retrieved 2007-06-01.
  7. Lixion Avila (2007-06-02). "Tropical Storm Barry Discussion Two". National Hurricane Center. Retrieved 2007-06-02.
  8. Lixion Avila and Xavier William Proenza (2007-06-02). "Tropical Storm Barry Discussion Four". National Hurricane Center. Retrieved 2007-06-02.
  9. Lixion Avila (2007). "Tropical Storm Barry Discussion Five". National Hurricane Center. Retrieved 2007-06-01.
  10. 1 2 3 4 Rubin-Oster (2007). "Public Advisory Number 7 for Remnants of Barry". Hydrometeorological Prediction Center. Retrieved 2007-06-03.
  11. 1 2 3 4 Kong (2007-06-03). "Public Advisory Number 9 for Remnants of Barry". Hydrometeorological Prediction Center. Retrieved 2007-06-03.
  12. Fracasso (2007-06-03). "Public Advisory Number 13 for Remnants of Barry". Hydrometeorological Prediction Center. Retrieved 2007-06-03.
  13. Avila (2007). "Tropical Storm Barry Public Advisory One-A". National Hurricane Center. Retrieved 2007-09-25.
  14. Ruskin, FL National Weather Service (2007). "Tropical Storm Local Statement". Archived from the original on 2013-10-05. Retrieved 2007-06-01.
  15. 1 2 3 Martin Merzer (2007). "Barry weakens but drenches South Florida". Miami Herald. Retrieved 2007-06-02.[ dead link ]
  16. "Tropical Storm Barry Event Report for Georgia". National Climatic Data Center. 2007. Retrieved 2008-11-19.
  17. Mike Tichacek (2007). "May 31 Tropical Weather Discussion". National Hurricane Center. Retrieved 2007-06-01.[ permanent dead link ]
  18. EFE (2007). "La tormenta tropical "Barry" baña con sus lluvias a Cuba" (in Spanish). Cuba Debate. Archived from the original on 2013-02-10. Retrieved 2007-06-02.
  19. First Coast News (2007). "Tropical Storm Barry Helps Out Wildfires" . Retrieved 2007-06-03.[ permanent dead link ]
  20. Susanne Cervenka (2007). "Barry brings precious gift of rain". Florida Today. Archived from the original on 2007-06-06. Retrieved 2007-06-03.
  21. Kimberly Miller (2007). "Welcome rains carve sinkholes in I-95". Palm Beach Post. Archived from the original on 2012-05-29. Retrieved 2007-06-03.
  22. WFTV-9 (2007). "Barry Downgraded After Soaking Central Florida". Archived from the original on 2007-06-06. Retrieved 2007-06-03.{{cite web}}: CS1 maint: numeric names: authors list (link)
  23. 1 2 3 Fracasso (2007). "Public Advisory Number 14 for Remnants of Barry". Hydrometeorological Prediction Center. Retrieved 2007-06-03.
  24. 1 2 3 McMichael (2007). "Tropical Storm Barry Post Tropical Cyclone Report". Ruskin, Florida National Weather Service. Archived from the original on 2018-09-15. Retrieved 2007-06-11.
  25. Fox13 (2007). "Barry leaves his calling card" . Retrieved 2007-06-03.{{cite web}}: CS1 maint: numeric names: authors list (link)[ dead link ]
  26. "Tropical Storm Barry brings rain to Florida". Associated Press. 2007. Archived from the original on September 30, 2007. Retrieved 2007-06-02.
  27. Tiffany Pakkala (2007). "Barry dumps 5 inches of rain on area". The St. Augustine Record. Archived from the original on 2013-11-03. Retrieved 2007-06-03.
  28. KFSN-TV (2007). "Tropical Storm Barry Brings Much Needed Rain To Florida". Archived from the original on 2012-10-04. Retrieved 2007-06-03.
  29. "First significant rain in weeks gives fire crews much-needed break". Associated Press. 2007. Archived from the original on September 26, 2007. Retrieved 2007-06-03.
  30. Savannah Morning News (2007). "Barry brings relief with 5 inches of rain" . Retrieved 2007-06-03.[ dead link ]
  31. 1 2 "Tropical Storm Barry Event Report for Georgia (2)". National Climatic Data Center. 2007.
  32. Charlie Hall (2007). "Barry causes few problems in region". New Bern Sun Journal. Archived from the original on 2011-07-27. Retrieved 2007-06-04.
  33. Bonesville.net (2007). "Chapel Hill Regional slips in the rain" . Retrieved 2007-06-03.
  34. Stone, Steve; Coutee, Amy (2007). "Tropical storm's leftovers force cancellations across region". Virginia Pilot. Archived from the original on 2012-10-02. Retrieved 2007-06-04.
  35. Daily Press (2007). "Boaters off Cape Fear rescued". Archived from the original on 2013-06-30. Retrieved 2007-06-03.
  36. "Tropical Storm Barry Event Report for New York". National Climatic Data Center. 2007.
  37. "Tropical Storm Barry Event Report for New York (2)". National Climatic Data Center. 2007.
  38. "Tropical Storm Barry Event Report for New Jersey". National Climatic Data Center. 2007.