Hurricane Bertha (2008) classified as a tropical depression by 06:00 UTC on July 3, located about 255 miles (410 km) south-southeast of Cabo Verde. The NHC noted that global modelling suggested the possibility of tropical development over a week prior, a "remarkable achievement" at the time. The storm's cloud pattern continued to coalesce, and it was upgraded to Tropical Storm Bertha six hours later. On the southern periphery of a mid-level ridge over the open Atlantic, Bertha moved swiftly west-northwest to northwest for several days. Despite being embedded within an environment of low vertical wind shear, the storm passed over ocean temperatures near
Hurricane Bertha (1990) Operationally, forecasters at the National Hurricane Center speculated whether Bertha was transitioning into a subtropical cyclone, due to its deep convection being located, at times, over 200 miles (321.8 km) from the center. However, the convection progressively returned to the center and by late on July 30, Bertha re-intensified into a hurricane as the convection covered the center, about 415 miles (667.8 km) east of where it first formed. Early on July 31, the hurricane briefly attained peak winds of 80 mph (130 km/h) before weakening and accelerated northeastward as the ridge of high pressure was slowly eroded. Bertha maintained