|
La pression au centre de l'ouragan Earl était faible, de l'ordre de 960 millibars lorsque, se déplaçant à 65 nœuds, (alors qu'il était de catégorie 1) il s'est abattu sur les zones côtières à environ 35 km au sud-ouest de Liverpool, Nouvelle-Écosse à 1030 HAA, le 4 septembre.
|
|
Earl formed off the Cape Verde Islands on August 27th, 2010. As it moved west-northwest brushing the northeastern Caribbean Islands it attained Category 4 intensity. On Sept. 3rd and 4th, as Earl moved northeast past the US seaboard, its intensity dropped to Category 1, while the wind field expanded significantly. The central pressure of Earl remained in the low 960 millibar range as it made landfall as a 65 knot (kt), Category 1 hurricane about 35 km southwest of Liverpool, Nova Scotia at 10:30 am ADT, September 4th.
|