Hurricane Danielle (2010)

This is an archive of a former Wikipedia article.

Hurricane Danielle was the first of four Category 4 hurricanes during the 2010 Atlantic hurricane season. The sixth tropical depression, fourth named storm, second hurricane, and first major hurricane of the season, Danielle developed as a typical Cape Verde-type hurricane from a tropical wave on August 21. Quickly intensifying, the new tropical depression became a tropical storm eighteen hours after formation on August 22, and it reached category 2 on August 24. Also on August 24, Hurricane Danielle weakened back to a category 1 hurricane, but it returned to category 2 strength on August 25. Further intensification occurred and Danielle became a Category 4 hurricane with peak winds of Template:Convert/mph on August 27. It then weakened, and finally dissipated on August 30. The hurricane was the first in a rapid succession of eleven named storms, which ended in late September.

Meteorological history

File:Danielle 2010 track.png

Map plotting the storm's track and intensity, according to the Saffir–Simpson scale
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On August 20, a tropical wave that formed two days earlier off Africa's western coast interacted with a large tropical disturbance in the Intertropical Convergence Zone. This disorganized disturbance covered an area from the southwest of Senegal to the south of the Cape Verde Islands while slowly moving west. The National Hurricane Center (NHC) began monitoring the system. As it moved through favorable conditions, the system became more organized and began circulating at a low level. Following a further increase in organization, the system was designated as Tropical Depression Six. As the depression tracked slowly westward, it quickly intensified. The following day, it was upgraded to Tropical Storm Danielle, the fourth tropical storm of the season.

Slow intensification ensued as Danielle headed generally westward and eventually became the second hurricane of the season on August 23. Hurricane Danielle reached an initial peak intensity on August 24 at category 2 with a maximum wind speed of Template:Convert/mph, making it a Category 2 hurricane on the Saffir-Simpson Hurricane Wind Scale. However, later that day, Danielle began to rapidly weaken as it briefly encountered an area of high wind shear and dry air. Danielle weakened to a category 1 hurricane with Template:Convert/mph winds late on August 24, only to suddenly re-intensify overnight. Further intensification was gradual, and Danielle again reached category 2 strength late on August 25, and an eye was present on satellite images. After a few days of gradual strengthening, Danielle began to rapidly intensify on August 27, and became the first major hurricane (Category 3 or higher on the Saffir-simpson hurricane wind scale) of the season with winds of Template:Convert/mph. Continuing the rapid intensification, Hurricane Danielle briefly became a category 4 hurricane on August 27, when it was situated Template:Convert/LoffAonD5Soff southeast of Bermuda, attaining its peak intensity with winds of Template:Convert/mph and a minimum barometric pressure of 94.2 kPa (27.82 inHg).

However, on August 28, Danielle encountered a large middle-level to upper-level weather trough moving off the coast of the eastern United States into the Atlantic Ocean. This pushed Danielle north-northeast. The inner of Danielle's two eye walls eroded as the hurricane weakened, signifying an eyewall replacement cycle. During this time, Hurricane Danielle's outflow exposed the core of the more southerly Hurricane Earl. However, Hurricane Earl (then a tropical storm) retained strong circulation, and the center eventually moved back under the convective canopy. The outflow from Danielle kept Earl a tropical storm before Danielle accelerated north and northeastward. As Danielle moved into a region with cooler sea surface temperatures and higher wind shear, it began to weaken at a steady pace and slowly began its extratropical transition. Danielle weakened to a category 1 hurricane on August 29, and became a tropical storm on the afternoon of August 30. Accelerating northeastward, Danielle completed the extratropical transition later that day. During the next few days, the extratropical remnants of Hurricane Danielle moved across the northern Atlantic Ocean, and were forecast to move into the area of Greenland and Iceland over the next five days. However, on September 3, Danielle's remnants dissipated after 72 hours in the cold waters of the northern Atlantic Ocean.

Preparations and impact

On August 27, a tropical storm watch was issued on Bermuda before being canceled during the afternoon of August 28 because Danielle turned sharply east. However, it still triggered an advisory concerning high surf and large waves on Bermuda.

Hurricane Danielle and Hurricane Earl caused strong ocean swells and rip currents on the coasts of New Jersey, Delaware, and Maryland. which swept people out to sea. In Florida, around 250 people from Ocean City were swept out to sea, and at least one person was drowned by the riptides. At least 70 more people had to be rescued off the remaining coast of eastern central Florida. On August 31, despite being more than Template:Convert/LoffAoffDbSoff from Newfoundland, Tropical Storm Danielle still caused Template:Convert/LoffAoffDbSoff waves on its shores.

Researchers exploring the sunken remnants of the RMS Titanic were forced to leave the area when Danielle approached on August 29.

External links

• The NHC's archive on Danielle
• NHC Graphics Archive on Danielle