October 2000 Atlantic Canada Storm Complex
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October 2000 Atlantic Canada Storm Complex
The October 2000 Atlantic Canada storm complex was reported as the worst storm in Prince Edward Island in 30 years. Environment Canada considered as one of the ten most significant weather events in Canada in the year. It moved southeastward from Atlantic Canada in late October 2000, producing high snowfall totals in Maine. It absorbed an unnamed subtropical cyclone, and remained nearly stationary in the Gulf of Maine for over a week. Some locations in Atlantic Canada reported record durations of continuous cloud cover. Daily amounts of rainfall produced flooding in Nova Scotia, while a high storm surge associated with the storm washed out roads in New Brunswick and Prince Edward Island. The storm produced wind gusts that peaked at 104 mph (168 km/h) in Newfoundland, and across the region there were scattered power outages. Meteorological history The coastal storm moved southward over southeastern Canada on October 28. Around the same time, a subtropical ...
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Extratropical Cyclone
Extratropical cyclones, sometimes called mid-latitude cyclones or wave cyclones, are low-pressure areas which, along with the anticyclones of high-pressure areas, drive the weather over much of the Earth. Extratropical cyclones are capable of producing anything from cloudiness and mild showers to severe gales, thunderstorms, blizzards, and tornadoes. These types of cyclones are defined as large scale (synoptic) low pressure weather systems that occur in the middle latitudes of the Earth. In contrast with tropical cyclones, extratropical cyclones produce rapid changes in temperature and dew point along broad lines, called weather fronts, about the center of the cyclone. Terminology The term " cyclone" applies to numerous types of low pressure areas, one of which is the extratropical cyclone. The descriptor ''extratropical'' signifies that this type of cyclone generally occurs outside the tropics and in the middle latitudes of Earth between 30° and 60° latitude. They are term ...
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National Hurricane Center
The National Hurricane Center (NHC) is the division of the United States' NOAA/National Weather Service responsible for tracking and predicting tropical weather systems between the Prime Meridian and the 140th meridian west poleward to the 30th parallel north in the northeast Pacific Ocean and the 31st parallel north in the northern Atlantic Ocean. The agency, which is co-located with the Miami branch of the National Weather Service, is situated on the campus of Florida International University in Westchester, Florida. The NHC's Tropical Analysis and Forecast Branch (TAFB) routinely issues marine forecasts, in the form of graphics and high seas forecasts year round, with the Ocean Prediction Center having backup responsibility for this unit. The Technology and Science Branch (TSB) provides technical support for the center, which includes new infusions of technology from abroad. The Chief, Aerial Reconnaissance Coordination, All Hurricanes (CARCAH) unit tasks planes, for r ...
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November 2001 Atlantic Canada Storm Complex
The November 2001 Atlantic Canada storm complex was a powerful coastal storm that included the remnants of North Atlantic hurricanes Michelle and Noel. The low intensified as it moved westward into Atlantic Canada on November 6, reaching a minimum pressure of 946 mbars. The storm turned to the northeast and emerged into the Atlantic Ocean on November 8. It produced strong winds throughout Atlantic Canada, including gusts of up to at the Confederation Bridge in Prince Edward Island. High waves caused damage along the coastlines, while high winds left up to 100,000 without power. Overall damage was minor, and no casualties were reported. Meteorological history On November 6, an extratropical storm located south of Newfoundland absorbed the remnants of Hurricane Noel. The extratropical storm previously absorbed Hurricane Michelle, and was moving quickly northeastward. The storm complex moved over Newfoundland, intensifying and producing strong winds throughout Atlan ...
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Stephenville, Newfoundland And Labrador
Stephenville (Canada 2021 Census population 6540) is a town in Newfoundland and Labrador, Canada, on the west coast of the island of Newfoundland. The town functions as a local service centre for the southwestern part of the island, serving a direct population of 35,000 people from surrounding areas and over 100,000 people along the entire southwestern coast of the island. The primary employer in the town was a paper mill, which closed in 2005. Stephenville has a modern 40-bed hospital (built in 2003), schools, stores, movie theater, banks, and an International Airport ( Stephenville International Airport, CYJT), year round ice free sea port (Port Harmon), and government institutions. The provincial community college system, College of the North Atlantic, is headquartered in Stephenville and maintains a campus there for students from the southwestern region of the island. The Newfoundland and Labrador Public Library system is also headquartered in Stephenville. A provincial mi ...
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Corner Brook
Corner Brook ( 2021 population: 19,333 CA 29,762) is a city located on the west coast of the island of Newfoundland in the province of Newfoundland and Labrador, Canada. Corner Brook is the fifth largest settlement in Newfoundland and Labrador. Located on the Bay of Islands at the mouth of the Humber River, the city is the second-largest population centre in the province behind St. John's, and smallest of three cities behind St. John's and Mount Pearl. As such, Corner Brook functions as a service centre for western and northern Newfoundland. It is located on the same latitude as Gaspé, Quebec, a city of similar size and landscape on the other side of the Gulf of St. Lawrence. Corner Brook is the most northern city in Atlantic Canada. It is the administrative headquarters of the Qalipu Mi'kmaq First Nations band government. The Mi'kmaq name for the nearby Humber River is "Maqtukwek". History The area was surveyed by Captain James Cook in 1767. The Captain James Cook Hist ...
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Coastal Erosion
Coastal erosion is the loss or displacement of land, or the long-term removal of sediment and rocks along the coastline due to the action of waves, currents, tides, wind-driven water, waterborne ice, or other impacts of storms. The landward retreat of the shoreline can be measured and described over a temporal scale of tides, seasons, and other short-term cyclic processes. Coastal erosion may be caused by hydraulic action, abrasion, impact and corrosion by wind and water, and other forces, natural or unnatural. On non-rocky coasts, coastal erosion results in rock formations in areas where the coastline contains rock layers or fracture zones with varying resistance to erosion. Softer areas become eroded much faster than harder ones, which typically result in landforms such as tunnels, bridges, columns, and pillars. Over time the coast generally evens out. The softer areas fill up with sediment eroded from hard areas, and rock formations are eroded away. Also erosion commonly ...
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Escuminac, New Brunswick
Escuminac (2011 population: 212) is a rural community in Northumberland County, New Brunswick, Canada. The local service district of Escuminac takes its name from the community. Located on the south shore of Miramichi Bay, the community is several kilometres west of Point Escuminac, the southeastern limit of the bay. Canada's largest inshore fishing vessel harbour is home to the local fishing fleet. Industries include two fish processing & freezing plants and a boat building facility. One of Canada's important herring spawning grounds is located beside Point Escuminac. According to Joseph-Étienne Guinard, a missionary and Cree language specialist with some experience with the Mi'kmaq, the word means "here are small fruits". This perfectly describes the area as berries proliferate en masse in this low-lying flat area, and the first colonist were amazed at the amount of Ericaceae. Peat bogs and rare peat cliffs are situated in the vicinity of Point Escuminac, approximatel ...
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Miramichi Bay
Miramichi Bay is an estuary located on the west coast of the Gulf of St. Lawrence in New Brunswick, at the mouth of the Miramichi River. Miramichi Bay is separated into the "inner bay" and the "outer bay", with the division being a line of uninhabited barrier islands which are continually reshaped by ocean storms. The largest of these islands is the uninhabited Portage Island, which was broken in two during a violent storm in the 1950s. The islands provide some protection to the inner bay from ocean storms in the Gulf of St. Lawrence. Miramichi Bay was named by Jacques Cartier in 1534. The Inner Miramichi Bay, and the lower portions of its tributary rivers (including the Miramichi River), are parts of a drowned river valley system. Since deglaciation, sea level rise in Miramichi Bay has flooded the mouths of these rivers with saltwater. The flooded, meandering, ancient Miramichi river channel forms a navigable route through the Inner Bay for ocean-going ships entering the p ...
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Cabot Trail
The Cabot Trail is a scenic highway on Cape Breton Island in Nova Scotia, Canada. It is a loop around the northern tip of the island, passing along and through the Cape Breton Highlands and the Cape Breton Highlands National Park. It is named after the explorer John Cabot who landed in Atlantic Canada in 1497, although modern historians agree his landfall likely took place in Newfoundland (island), Newfoundland and not Cape Breton Island. Premier Angus L. MacDonald wanted to re-brand Nova Scotia for tourism purposes as primarily Scottish and, as part of this effort, created both the names Cape Breton Highlands and Cabot Trail.Ian MacKay and Robin Bates. ''In the Province of History''. Montreal: McGill-Queen's Press. 2010. Construction of the initial route was completed in 1932. The western and eastern sections follow the rugged coastline, with views of the ocean. The southwestern section passes through the Margaree River valley before passing along Bras d'Or Lake. The route is ...
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Canadian Dollar
The Canadian dollar ( symbol: $; code: CAD; french: dollar canadien) is the currency of Canada. It is abbreviated with the dollar sign $, there is no standard disambiguating form, but the abbreviation Can$ is often suggested by notable style guides for distinction from other dollar-denominated currencies. It is divided into 100 cents (¢). Owing to the image of a common loon on its reverse, the dollar coin, and sometimes the unit of currency itself, are sometimes referred to as the ''loonie'' by English-speaking Canadians and foreign exchange traders and analysts. Accounting for approximately 2% of all global reserves, the Canadian dollar is the fifth-most held reserve currency in the world, behind the U.S. dollar, the euro, the yen and sterling. The Canadian dollar is popular with central banks because of Canada's relative economic soundness, the Canadian government's strong sovereign position, and the stability of the country's legal and political systems. Histo ...
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Gulf Of St
A gulf is a large inlet from the ocean into the landmass, typically with a narrower opening than a bay, but that is not observable in all geographic areas so named. The term gulf was traditionally used for large highly-indented navigable bodies of salt water that are enclosed by the coastline. Many gulfs are major shipping areas, such as the Persian Gulf, Gulf of Mexico, Gulf of Finland, and Gulf of Aden The Gulf of Aden ( ar, خليج عدن, so, Gacanka Cadmeed 𐒅𐒖𐒐𐒕𐒌 𐒋𐒖𐒆𐒗𐒒) is a deepwater gulf of the Indian Ocean between Yemen to the north, the Arabian Sea to the east, Djibouti to the west, and the Guardafui Channe .... See also * References External links * {{Authority control Bodies of water Coastal and oceanic landforms Coastal geography Oceanographical terminology ...
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Storm Surge
A storm surge, storm flood, tidal surge, or storm tide is a coastal flood or tsunami-like phenomenon of rising water commonly associated with low-pressure weather systems, such as cyclones. It is measured as the rise in water level above the normal tidal level, and does not include waves. The main meteorological factor contributing to a storm surge is high-speed wind pushing water towards the coast over a long fetch. Other factors affecting storm surge severity include the shallowness and orientation of the water body in the storm path, the timing of tides, and the atmospheric pressure drop due to the storm. There is a suggestion that climate change may be increasing the hazard of storm surges. Some theorize that as extreme weather becomes more intense and sea level rises due to climate change, storm surge is expected to cause more risk to coastal populations. Communities and governments can adapt by building hard infrastructure, like surge barriers, soft infrastructure, ...
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