When the storm came near Canada, a buoy recorded winds of 36 mph (56 km/h). It also recorded a wind gust of 44 mph (70 km/h). The storm lost a large amount of strength before it moved over Newfoundland. Because of this, there was no damage. The Atlantic Storm Prediction Centre sent out gale warnings for the storm.
Every year, the National Hurricane Center checks to make sure they did not miss any storms during the past tropical storm season. They found this storm on December 15, 2006, when they were studying the 2006 season. If the storm was found when it was active, it would have been called "Tropical Storm Beryl". It is guessed that the storm became a tropical cyclone at 39.1º N. This was the farthest north that any Atlantic storm in July became a tropical cyclone. This broke the past record that was set by Tropical Storm Arthur in 2002.
Nantucket, Massachusetts
Nantucket is an island 30 miles (48.3 km) south of Cape Cod, Massachusetts, in the United States.
Cape Hatteras
Cape Hatteras is a cape on the coast of North Carolina. It is the point that protrudes the farthest to the southeast along the northeast-to-southwest line of the Atlantic coast of North America, making it a key point for navigation along the eastern seaboard. So many ships have been lost around it that the area is known as the "Graveyard of the Atlantic". The nearby shoals are known as Diamond Shoals.
The Cape Hatteras Lighthouse is a well known feature on Cape Hatteras. It was built in 1870 and it is the tallest brick lighthouse in the United States.
Tropical Storm Alberto (1988)
Tropical Storm Alberto (also known as Hurricane Alberto) became a tropical storm farther north than any other Atlantic tropical cyclone. It was the first tropical storm of the 1988 Atlantic hurricane season. It started from a region of low pressure off of the coast of South Carolina on August 5.
It quickly moved northeast. It became a tropical storm on August 7. It was about 60 miles (95 km) east of the Massachusetts island of Nantucket.
Tropical Storm Alberto continued to move quickly, and struck the western area of Nova Scotia late on August 7. It lost its status as a tropical storm the next day when it reached north of Newfoundland. Alberto produced light rain and wind across its path. No damage came from it.
Tropical Storm Beryl (2006)
Tropical Storm Beryl was the third tropical storm of the 2006 Atlantic hurricane season. Developing from a tropical disturbance on July 18, it tracked generally northward, and strengthened to attain peak winds of 60 mph (95 km/h) under generally favorable conditions. After turning to the northeast, Beryl weakened over cooler waters. On July 21 it struck the island of Nantucket, and shortly thereafter it became extratropical. The extratropical remnants continued northeastward through Nova Scotia, and on July 22 it merged with an approaching cold front.
Beryl produced rough seas along the northeast United States coastline. In Massachusetts, its impact was limited to light rainfall and gusty winds, with no reported damage. Beryl later produced moderate rainfall and gusty winds across Atlantic Canada, resulting in some localized power outages though little damage. No deaths were reported.
A cold front moved off the East Coast of the United States on July 16 and stalled off the coast of North Carolina. It slowly decayed into a surface low pressure trough, and developed into two disturbances; one was centered 290 miles (490 km) south-southeast of Cape Cod and another was located 200 miles (320 km) south of Cape Hatteras, North Carolina. The first low quickly organized into an unnamed tropical storm, and the other area stayed broad and disorganized. However, by July 18, the system became much better organized with improved banding features, and the area developed into Tropical Depression Two while located 220 miles (355 km) south-southeast of Cape Hatteras.
The depression moved slowly to the north-northwest through a break in the subtropical ridge, and as convective banding features became more visible the system strengthened into Tropical Storm Beryl. Throughout much of its duration, the storm tracked through an environment with light vertical wind shear and well-established upper-level outflow. Shortly after becoming a tropical storm, the low-level circulation of Beryl became exposed with limited deep convection, though deep convection re-developed the following morning. Outflow continued to improve, and with warm sea surface temperatures Beryl slowly strengthened further to reach peak winds of 60 mph (95 km/h) early on July 20 while located about 120 miles (190 km) east of Nags Head, North Carolina.
Beryl maintained peak winds for about 18 hours as it paralleled the Mid-Atlantic and New Jersey coasts, during which an eye-like feature developed in the center of the convection. Late on July 20, it began a slow weakening trend after passing over cooler waters. Steering winds ahead of an approaching mid-level trough caused Beryl to speed up northeastward, and early on July 21 the center of the storm crossed the island of Nantucket. The convection diminished as it moved through progressively colder waters, and shortly after 1200 UTC on July 21 Beryl became an extratropical cyclone a short distance east of Cape Cod. Hours later, it made landfall in southwestern Nova Scotia, and on July 22 the extratropical remnants of Beryl merged with an approaching cold front over Newfoundland.
Forecasters originally predicted Beryl to brush the Carolinas; as such, a tropical storm watch was issued for the eastern coast of North Carolina from Cape Lookout northward to Currituck Beach Lighthouse. When a more northeastward track became apparent, a tropical storm watch was issued about 33 hours before moving ashore from Woods Hole to Plymouth, Massachusetts, including Cape Cod, Nantucket, and Martha's Vineyard. About 22 hours before landfall, the National Hurricane Center replaced the watch with a tropical storm warning for the same area, and also issued a tropical storm watch from Woods Hole, Massachusetts westward to New Haven, Connecticut and for the eastern portion of Long Island from east of Fire Island to Port Jefferson. Expecting for the storm, the Massachusetts Emergency Management Agency was activated as a trial run for the hurricane season. Local Red Cross chapters were opened, as well, with two volunteer teams placed on standby to assist. Across southeastern Massachusetts, police departments maintained extra staff in preparation for any potential problems from the storm. Many fishermen secured their boats, while some business owners boarded up windows to prevent storm damage.
Several days prior to the passage of Beryl through Atlantic Canada, the Canadian Hurricane Centre issued gale warnings for the coastal waters off of Nova Scotia and Newfoundland. In anticipation of heavy rainfall, the agency also issued heavy rainfall warnings for western Nova Scotia, including Halifax.
The storm caused high waves along the East Coast of the United States, with 19 foot seas (5.97 m) in the open ocean. Waves along the southern coast of Nantucket reached 10 feet in height as the storm approached the island, resulting in four people being rescued by lifeguards from rip currents.
High surf was also reported along the southern coast of Massachusetts and Rhode Island. Beryl also produced a storm surge of 0.9 feet on Nantucket. Winds across southeastern Massachusetts were fairly light, with no sustained tropical storm force winds and wind gusts peaking at 44 mph; unofficially gusts reached 51 mph.