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Gale Of January 1976
The Gale of January 1976, widely known as the "Capella" storm in Germany and the Ruisbroek flood in Belgium, was one in a series of extratropical cyclones and storm surges, which occurred over January 1976. The gale of 2–5 January 1976 resulted in severe wind damage across western and central Europe and coastal flooding around the southern North Sea coasts. At the time, this was the most severe storm of the century over the British Isles. Total fatalities reached 82 across Europe, although a figure of 100 is given by the World Meteorological Organization. Of these 24 were reported in Britain and 4 in Ireland. Overall losses of US$1.3 billion were incurred, with insured losses standing at US$500 million (1976). Meteorological history December 1975 saw a deep low persisting over the northern Barents Sea with a high north of the Azores and west of Biscay, which enhanced a strong westerly flow over northern Europe. This anomalously strong westerly flow over the No ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
European Windstorm
European windstorms are powerful extratropical cyclones which form as cyclonic windstorms associated with areas of low atmospheric pressure. They can occur throughout the year, but are most frequent between October and March, with peak intensity in the winter months. Deep areas of low pressure are common over the North Atlantic, and occasionally start as nor'easters off the New England coast. They frequently track across the North Atlantic Ocean towards the north of Scotland and into the Norwegian Sea, which generally minimizes the impact to inland areas; however, if the track is further south, it may cause adverse weather conditions across Central Europe, Northern Europe and especially Western Europe. The countries most commonly affected include the United Kingdom, Ireland, the Netherlands, Norway, Germany, the Faroe Islands and Iceland. The strong wind phenomena intrinsic to European windstorms, that give rise to "damage footprints" at the surface, can be placed into three cat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Malin Head
Malin Head ( ga, Cionn Mhálanna) is the most northerly point of mainland Ireland, located in the townland of Ardmalin on the Inishowen peninsula in County Donegal. The head's northernmost point is called Dunalderagh at latitude 55.38ºN. It is about 16 km (10 mi) north of the village of Malin. The island of Inishtrahull is further north, about 10 km (6 mi) northeast of the headland. Malin Head gives its name to the Malin sea area. There is a weather station on the head, which is one of 22 such stations whose reports are broadcast as part of the BBC Shipping Forecast. A tower built in 1805 is on Altnadarrow, also known locally as the Tower Hill. Ptolemy's ''Geography'' (2nd century AD) described a point called Βορειον (''Boreion'', "the northern") which probably referred to Malin Head. Locality To the northeast Inistrahull Island can be seen. The first lighthouse on the island was put into operation in 1813, and the light flashes every 30 seco ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ulster
Ulster (; ga, Ulaidh or ''Cúige Uladh'' ; sco, label= Ulster Scots, Ulstèr or ''Ulster'') is one of the four traditional Irish provinces. It is made up of nine counties: six of these constitute Northern Ireland (a part of the United Kingdom); the remaining three are in the Republic of Ireland. It is the second-largest (after Munster) and second-most populous (after Leinster) of Ireland's four traditional provinces, with Belfast being its biggest city. Unlike the other provinces, Ulster has a high percentage of Protestants, making up almost half of its population. English is the main language and Ulster English the main dialect. A minority also speak Irish, and there are Gaeltachtaí (Irish-speaking regions) in southern County Londonderry, the Gaeltacht Quarter, Belfast, and in County Donegal; collectively, these three regions are home to a quarter of the total Gaeltacht population of Ireland. Ulster-Scots is also spoken. Lough Neagh, in the east, is the largest lake i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shannon Airport
Shannon Airport ( ga, Aerfort na Sionainne) is an international airport located in County Clare in the Republic of Ireland. It is adjacent to the Shannon Estuary and lies halfway between Ennis and Limerick. The airport is the third busiest airport in the Republic of Ireland, and the fifth busiest on the island. The airport has a history of pioneering in global aviation with the first transatlantic proving flight in 1945, the world's first duty-free airport opening in 1947, and Europe's first United States border preclearance facility opening in 1986. It was a busy refuelling stop for many international carriers in the 1960s, making it a gateway between Europe and the Americas. At , Shannon has the longest runway in Ireland, which allowed it to be a designated alternative landing site for the Space Shuttle. History Establishment In the late 1930s, transatlantic air traffic was dominated by flying boats, and a flying boat terminal was located at Foynes on the south side ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
ESB Group
The Electricity Supply Board (ESB; ga, Bord Soláthair an Leictreachais) is a state owned (95%; the rest are owned by employees) electricity company operating in the Republic of Ireland. While historically a monopoly, the ESB now operates as a commercial semi-state concern in a "liberalised" and competitive market. It is a statutory corporation whose members are appointed by the Government of Ireland. Business areas The ESB is composed of several distinct, separate and legally demarcated companies. By business area, the principal companies are: ''ESB Networks Limited'' manages construction and maintenance of the electricity transmission system. (The transmission system operator is an independent state company, EirGrid). ''ESB Generation and Wholesale Markets (ESB GWM)'' operates a portfolio of power stations across the country, along with holdings in wind and other renewables. ''Electric Ireland'' is a regulated supply company, one of fourteen companies (as of 10 October 2 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
1961 Atlantic Hurricane Season
The 1961 Atlantic hurricane season was a hyperactive Atlantic hurricane season, with an accumulated cyclone energy (ACE) total of 189. The season, however, was an average one in terms of named storms. The season featured eight hurricanes and a well above average number of five major hurricanes. It was previously thought that the season had a record-tying seven major hurricanes, before the Atlantic hurricane reanalysis project downgraded two storms in 2019. Two Category 5 hurricanes were seen in 1961, making it one of only seven Atlantic hurricane seasons to feature multiple Category 5 hurricanes in one season. The season started on June 15, and ended on November 15. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. The first system, an operationally unclassified tropical depression, formed offshore east Central Florida on June 10, but dissipated a few days later. Next, Hurricane Anna developed in the eastern Ca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Athlone
Athlone (; ) is a town on the border of County Roscommon and County Westmeath, Ireland. It is located on the River Shannon near the southern shore of Lough Ree. It is the second most populous town in the Midlands Region with a population of 21,349 in the 2016 census. Most of the town lies on the east bank of the river, within the townland of the same name; however, by the terms of the Local Government Act of 1898, six townlands on the west bank of the Shannon, formerly in County Roscommon, were incorporated into the town, and consequently, into the county of Westmeath. Around 100 km west of Dublin, Athlone is near the geographical centre of Ireland, which is north-northwest of the town, in the area of Carnagh East in County Roscommon. History Athlone Castle, situated on the western bank of the River Shannon, is the geographical and historical centre of Athlone. Throughout its early history, the ford of Athlone was strategically important, as south of Athlone the Sha ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Portumna
Portumna ( - meaning 'the landing place of the oak') is a market town in the south-east of County Galway, Ireland, on the border with and linked by a bridge to County Tipperary. The town is located to the west of the point where the River Shannon enters Lough Derg. This historic crossing point over the River Shannon between counties Tipperary and Galway has a long history of bridges and ferry crossings. On the south-western edge of the town lie Portumna Castle and Portumna forest park. History Portumna Bridge Portumna is served with a five-span road bridge over the Shannon. This was designed by C. E. Stanier of London, and completed in 1911, with a central section resting on Hayes's Island which divides the river into two channels. The steel structure of the main bridge and pivoting swing bridge over the navigation channel are of technical and engineering interest, and it is the largest early-twentieth century swing bridge in Europe.. The opening section was replaced in Octobe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Shannon
The River Shannon ( ga, Abhainn na Sionainne, ', '), at in length, is the longest river in the British Isles. It drains the Shannon River Basin, which has an area of , – approximately one fifth of the area of the island of Ireland. The Shannon divides the west of Ireland (principally the province of Connacht) from the east and south (Leinster and most of Munster). (County Clare, being west of the Shannon but part of the province of Munster, is the major exception.) The river represents a major physical barrier between east and west, with fewer than thirty-five crossing points between Limerick city in the south and the village of Dowra in the north. The river takes its name after ''Sionna'', a Celtic goddess. Known as an important waterway since antiquity, the Shannon first appeared in maps by the Graeco-Egyptian geographer Ptolemy ( 100 – 170 AD). The river flows generally southwards from the Shannon Pot in County Cavan before turning west and emptying into the A ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Met Éireann
Met Éireann (; meaning " Met of Ireland") is the state meteorological service of Ireland, part of the Department of Housing, Local Government and Heritage. History The history of modern meteorology in Ireland dates back to 8 October 1860, when the first weather observations were transmitted from Valentia Observatory on Valentia Island in County Kerry to the British Meteorological Office. A network of weather stations was established around the coasts of the United Kingdom of Great Britain and Ireland. The service expanded rapidly in the post-war years, with its headquarters relocating to O'Connell Street, opposite The Gresham Hotel in Dublin. The service began supplying forecasts to Radio Éireann from 1948, to daily newspapers from 1952, to television from shortly after the first Raidió Teilifís Éireann (RTÉ) television broadcasts in 1962, and recorded telephone forecasts in the 1960s. Ireland joined the World Meteorological Organisation in the 1950s, and was a founde ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Occluded Front
In meteorology, an occluded front is a type of weather front formed during cyclogenesis. The classical and usual view of an occluded front is that it initiates when a cold front overtakes a warm front near a cyclone, such that the warm air is separated (occluded) from the cyclone center at the surface. The point where the warm front becomes the occluded front is the ''triple point''; a new area of low-pressure that develops at this point is called a ''triple-point low''. A more modern view of the formation process suggests that occluded fronts form directly without the influence of other fronts during the wrap-up of the baroclinic zone during cyclogenesis, and then lengthen due to flow deformation and rotation around the cyclone as the cyclone forms. Features and variants Occluded fronts usually form around mature low pressure areas. There are two types of front occlusions, warm and cold, depending on the temperature contrast: * In a cold occlusion, the cold air mass that over ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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