Hurricane Karl (2004)
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Hurricane Karl (2004)
Hurricane Karl was a large and powerful Cape Verde hurricane during the 2004 Atlantic hurricane season. It was the eleventh named storm, eighth hurricane, and the sixth and final major hurricane of the 2004 season. Karl formed on September 16, originating from a strong tropical wave that emerged off the coast of Africa. It rapidly intensified, becoming a major hurricane on two occasions. Karl peaked as a strong Category 4 hurricane on the Saffir-Simpson hurricane scale on September 21 with 145 mph (230 km/h) winds. It weakened as it moved northward, becoming extratropical on September 24 in the north Atlantic before it was absorbed by another system on September 28. The extratropical storm affected the Faroe Islands, but no damage was reported there, nor were there any fatalities. Meteorological history Karl originated in a strong tropical wave that moved off the coast of Africa on September 13. The wave gradually became better organized, and it was declared Tropic ...
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Faroe Islands
The Faroe Islands ( ), or simply the Faroes ( fo, Føroyar ; da, Færøerne ), are a North Atlantic island group and an autonomous territory of the Kingdom of Denmark. They are located north-northwest of Scotland, and about halfway between Norway ( away) and Iceland ( away). The islands form part of the Kingdom of Denmark, along with mainland Denmark and Greenland. The islands have a total area of about with a population of 54,000 as of June 2022. The terrain is rugged, and the subpolar oceanic climate (Cfc) is windy, wet, cloudy, and cool. Temperatures for such a northerly climate are moderated by the Gulf Stream, averaging above freezing throughout the year, and hovering around in summer and 5 °C (41 °F) in winter. The northerly latitude also results in perpetual civil twilight during summer nights and very short winter days. Between 1035 and 1814, the Faroe Islands were part of the Kingdom of Norway, which was in a personal union with Denmark from 1 ...
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Eye (cyclone)
The eye is a region of mostly calm weather at the center of tropical cyclones. The eye of a storm is a roughly circular area, typically in diameter. It is surrounded by the ''eyewall'', a ring of towering thunderstorms where the most severe weather and highest winds occur. The cyclone's lowest barometric pressure occurs in the eye and can be as much as 15 percent lower than the pressure outside the storm. In strong tropical cyclones, the eye is characterized by light winds and clear skies, surrounded on all sides by a towering, symmetric eyewall. In weaker tropical cyclones, the eye is less well defined and can be covered by the central dense overcast, an area of high, thick clouds that show up brightly on satellite imagery. Weaker or disorganized storms may also feature an eyewall that does not completely encircle the eye or have an eye that features heavy rain. In all storms, however, the eye is the location of the storm's minimum barometric pressure—where the atmospheric pr ...
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Hurricanes In Europe
The effects of tropical cyclones in Europe and their extratropical remnants include strong winds, heavy rainfall, and in rare instances, tornadoes or snowfall. Only two modern cyclones officially are being regarded as directly impacting mainland Europe while still fully tropical or subtropical: Hurricane Vince in 2005, which struck southwestern Spain as a tropical depression; and Subtropical Storm Alpha in 2020, which made landfall in northern Portugal at peak intensity. It is possible that Hurricane Debbie in 1961, may have been tropical still, when it made landfall in northwestern Ireland, but this is disputed. It is believed that a hurricane struck Europe in 1842. Atlantic hurricanes generally do not form east of the 30th meridian west, and those that do typically continue to the west. Storms can move around the Bermuda high and turn to the northeast and affect Europe. Several extratropical cyclones have struck Europe, and they were called colloquially "hurricanes". Some of the ...
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Category 4 Atlantic Hurricanes
Category, plural categories, may refer to: Philosophy and general uses * Categorization, categories in cognitive science, information science and generally *Category of being * ''Categories'' (Aristotle) *Category (Kant) *Categories (Peirce) *Category (Vaisheshika) *Stoic categories *Category mistake Mathematics * Category (mathematics), a structure consisting of objects and arrows * Category (topology), in the context of Baire spaces * Lusternik–Schnirelmann category, sometimes called ''LS-category'' or simply ''category'' * Categorical data, in statistics Linguistics * Lexical category, a part of speech such as ''noun'', ''preposition'', etc. *Syntactic category, a similar concept which can also include phrasal categories *Grammatical category, a grammatical feature such as ''tense'', ''gender'', etc. Other * Category (chess tournament) * Objective-C categories, a computer programming concept * Pregnancy category * Prisoner security categories in the United Kingdom * ...
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Hurricane Lorenzo (2019)
Hurricane Lorenzo, also known as Storm Lorenzo for Ireland and the United Kingdom while extratropical, was the easternmost Category 5 Atlantic hurricane on record. Lorenzo was the twelfth named storm, fifth hurricane, third major hurricane and second Category5 hurricane of the 2019 Atlantic hurricane season. The storm formed from a tropical wave that moved off the west coast of Africa on 22 September, growing larger in size over the course of its development. It strengthened into a hurricane on 25 September, and rapidly intensified into a Category 4 hurricane the following day before weakening due to an eyewall replacement cycle. After completing the cycle, Lorenzo rapidly restrengthened, peaking at Category 5 intensity on 29 September with 1-minute sustained winds of 160 mph. Steady weakening followed as the storm moved through unfavorable atmospheric conditions. Accelerating northeastward, Lorenzo skirted the western Azores on 2 October, and transitioned ...
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Hurricane Katia (2011)
Hurricane Katia was a fairly intense Cape Verde hurricane that had substantial impact across Europe as a post-tropical cyclone. The eleventh named storm, second hurricane, and second major hurricane of the active 2011 Atlantic hurricane season, Katia originated as a tropical depression from a tropical wave over the eastern Atlantic on August 29. It intensified into a tropical storm the following day and further developed into a hurricane by September 1, although unfavorable atmospheric conditions hindered strengthening thereafter. As the storm began to recurve over the western Atlantic, a more hospitable regime allowed Katia to become a major hurricane by September 5 and peak as a Category 4 hurricane with winds of that afternoon. Internal core processes, increased wind shear, an impinging cold front, and increasingly cool ocean temperatures all prompted the cyclone to weaken almost immediately after peak, and Katia ultimately transitioned into an extratro ...
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Hurricane Maria (2005)
Hurricane Maria was an Atlantic hurricane which formed in September 2005 during the annual hurricane season. Maria was the thirteenth named storm, sixth hurricane, and fourth major hurricane of the record-breaking season. Maria formed in the central Atlantic on September 1 and tracked to the northwest, strengthening as it moved over warm waters. The storm reached its peak intensity on September 5 east of Bermuda and gradually weakened before becoming extratropical on September 10. Maria did not affect any land as a tropical cyclone, but Maria brought tropical storm-force winds to Iceland as an extratropical cyclone and produced heavy rain and three fatalities in Norway. Meteorological history A powerful tropical wave moved off the coast of Africa on August 27. As it moved west into the Atlantic, it became more organized and the system developed into Tropical Depression Fourteen about midway between Cape Verde and the Lesser Antilles on September 1. Shear from an upper-lev ...
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Hurricane Kate (2003)
Hurricane Kate was a long-lived and erratic tropical cyclone that caused minor impacts across the Atlantic Ocean from late September to early October 2003. The sixteenth tropical cyclone, eleventh tropical storm, seventh hurricane, and third major hurricane of the 2003 Atlantic hurricane season, Kate developed from a tropical wave in the central tropical Atlantic on September 25. Its unusual track included four major changes in direction. The storm moved northwestward until a weakness in the subtropical ridge forced it eastward. Kate strengthened to a hurricane, turned sharply westward while moving around a mid-level low, and intensified to a major hurricane on October 4. Kate turned sharply northward around the periphery of an anticyclone, weakened, and became extratropical after passing to the east of Newfoundland. The extratropical storm persisted for three days until losing its identity near Scandinavia. The storm had minimal effects on land, limited to moderately strong wind ...
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List Of Category 4 Atlantic Hurricanes
Category 4 hurricanes are tropical cyclones that reach Category 4 intensity on the Saffir–Simpson scale. Category 4 hurricanes that later attained Category 5 strength are not included in this list. The Atlantic basin includes the open waters of the Atlantic Ocean The Atlantic Ocean is the second-largest of the world's five oceans, with an area of about . It covers approximately 20% of Earth's surface and about 29% of its water surface area. It is known to separate the " Old World" of Africa, Europe ..., the Caribbean Sea and the Gulf of Mexico. Category 4 is the second-highest hurricane classification category on the Saffir–Simpson Hurricane Scale, and storms that are of this intensity maintain maximum sustained winds of 113–136 knot (unit), knots (130–156 mph, 209–251 km/h). Based on the Atlantic hurricane database, 144 hurricanes have attained Category 4 hurricane status since 1851, the start of m ...
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North Sea
The North Sea lies between Great Britain, Norway, Denmark, Germany, the Netherlands and Belgium. An epeiric sea on the European continental shelf, it connects to the Atlantic Ocean through the English Channel in the south and the Norwegian Sea in the north. It is more than long and wide, covering . It hosts key north European shipping lanes and is a major fishery. The coast is a popular destination for recreation and tourism in bordering countries, and a rich source of energy resources, including wind and wave power. The North Sea has featured prominently in geopolitical and military affairs, particularly in Northern Europe, from the Middle Ages to the modern era. It was also important globally through the power northern Europeans projected worldwide during much of the Middle Ages and into the modern era. The North Sea was the centre of the Vikings' rise. The Hanseatic League, the Dutch Republic, and the British each sought to gain command of the North Sea and access t ...
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North Atlantic Ocean
The Atlantic Ocean is the second-largest of the world's five oceans, with an area of about . It covers approximately 20% of Earth's surface and about 29% of its water surface area. It is known to separate the "Old World" of Africa, Europe and Asia from the "New World" of the Americas in the European perception of the World. The Atlantic Ocean occupies an elongated, S-shaped basin extending longitudinally between Europe and Africa to the east, and North and South America to the west. As one component of the interconnected World Ocean, it is connected in the north to the Arctic Ocean, to the Pacific Ocean in the southwest, the Indian Ocean in the southeast, and the Southern Ocean in the south (other definitions describe the Atlantic as extending southward to Antarctica). The Atlantic Ocean is divided in two parts, by the Equatorial Counter Current, with the North(ern) Atlantic Ocean and the South(ern) Atlantic Ocean split at about 8°N. Scientific explorations of the Atlant ...
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Baroclinic
In fluid dynamics, the baroclinity (often called baroclinicity) of a stratified fluid is a measure of how misaligned the gradient of pressure is from the gradient of density in a fluid. In meteorology a baroclinic flow is one in which the density depends on both temperature and pressure (the fully general case). A simpler case, barotropic flow, allows for density dependence only on pressure, so that the curl of the pressure-gradient force vanishes. Baroclinity is proportional to: :\nabla p \times \nabla \rho which is proportional to the sine of the angle between surfaces of constant pressure and surfaces of constant density. Thus, in a ''barotropic'' fluid (which is defined by zero baroclinity), these surfaces are parallel. In Earth's atmosphere, barotropic flow is a better approximation in the tropics, where density surfaces and pressure surfaces are both nearly level, whereas in higher latitudes the flow is more baroclinic. These midlatitude belts of high atmospheric bar ...
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