Hurricane Karl (2004)

Hurricane Karl was a powerful Cape Verde-type hurricane during the 2004 Atlantic hurricane season. It was the eleventh named storm, eighth hurricane and fifth major hurricane of the 2004 season. Karl formed on September 16, originating from a strong tropical wave that emerged off of Africa. It rapidly intensified, becoming a major hurricane on two occasions. Karl peaked as a strong Category 4 hurricane on the Saffir-Simpson hurricane scale on September 21 with 145 mph (230 km/h) winds. It weakened as it moved northward, becoming extratropical on September 24 in the north Atlantic and becoming absorbed by another system on September 28. The extratropical storm affected the Faroe Islands, but no damage was reported there and no lives were lost.

Meteorological history

Karl originated in a strong tropical wave that moved off the coast of Africa on September 13. The wave gradually became better organized, and it was declared Tropical Depression Twelve about 670 miles (1,080 km) west-southwest of the Cape Verde islands on the morning of September 16, as it headed westward in the open tropical Atlantic following the periphery of the subtropical ridge. That afternoon, the depression continued to rapidly organize and was upgraded to Tropical Storm Karl. Due to healthy outflow around an upper-level anticyclone over Karl and a favorable environment with the warmest sea surface temperatures of the year, rapid deepening began on the evening of September 17, with the storm developing a small eye and being upgraded to Hurricane Karl. With SST's around 83°F (28°C) and minimal wind shear to disrupt circulation, the cyclone continued to rapidly intensify on the morning of September 18. The intensity leveled off somewhat that afternoon as a strong Category 2 hurricane with winds of 110 mph (175 km/h).

Late in the evening of September 18, Karl attained Category 3 status, becoming the fifth major hurricane of 2004. On September 19, Karl continued to strengthen, maintaining a well-defined eye, and strengthening late that day into a Category 4 hurricane with winds of 135 mph (215 km/h) and a minimum pressure of 948 mbar. Early on September 20, the storm weakened slightly as a result of an eyewall replacement cycle, falling back to a high-end Category 3 storm. At this time Karl began to turn sharply northward into a weakness in the subtropical ridge.

After intensification stopped on September 20 due to the eyewall cycle and slightly increased wind shear, Karl quickly restrengthened that evening over very warm water, and early on September 21 reached its peak intensity as a powerful Category 4 hurricane with 145 mph (230 km/h) winds and a minimum central pressure of 938 mbar. That morning, as Karl was moving northward, another eyewall replacement cycle began to take place and vertical shear increased, again weakening the storm temporarily. The trend continued into the evening, and the storm weakened to a Category 2 hurricane by early on September 22. The weakening trend slowed down and eventually leveled off that afternoon with Karl remaining a Category 2 hurricane as the storm turned towards the north-northeast. Late that evening, Karl began to restrengthen once again as wind shear diminished. The intensification continued into the morning of September 23, as Karl became a major hurricane a second time, reaching a final peak of 125 mph (205 km/h) winds. Cooler waters and increased shear soon prevailed, however, and the storm quickly weakened, dropping to a Category 1 hurricane by late that evening as the low-level circulation became detached from the mid-level circulation due to the strong southwesterly vertical wind shear.

Early on September 24, Karl continued its north-northeast track over the open north-central Atlantic and continued to gradually weaken. It started to come in contact with the baroclinic zone and began to lose tropical characteristics, while still a Category 1 hurricane. Karl became extratropical shortly afterward over the northern Atlantic at about 47°N, with its winds dropping below hurricane strength shortly thereafter. The extratropical storm made landfall on the Faroe Islands with hurricane-force wind gusts. As an extratropical low, the cyclone moved northeastward and eastward across the North Atlantic Ocean and the North Sea, eventually reaching Norway before it was absorbed into another extratropical low late on September 28.

Impact

Karl made landfall in the Faroe Islands as an extratropical storm with sustained winds near 70 mph (110 km/h) and with wind gusts up to 89 mph (144 km/h). No damages or deaths were reported, and no ships came directly into contact with Karl; the strongest winds reported were from the ship Rotterdam, which reported 52 mph (83 km/h) sustained winds in the north Atlantic while Karl was a Category 1 storm in extratropical transition. Because the storm caused only mminimal damage, the name Karl was not retired, and is on the list of names for the 2010 Atlantic hurricane season.

See also

• List of tropical cyclones
• List of Atlantic hurricane seasons
• 2004 Atlantic hurricane season

References

External links

• NHC's Tropical Cyclone Report on Hurricane Karl