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Spanish Plume
The Spanish Plume (Penacho Ibérico in Spanish and Spaanse Pluim in Dutch) is a weather pattern in which a plume of warm air moves from the Iberian plateau or the Sahara to northwestern Europe, causing thunderstorms. This meteorological pattern can lead to extreme high temperatures and intense rainfall during the summer months, with potential for flash flooding, damaging hail, and tornado formation. Some of these intense thunderstorms are formed from thermal lows, which are also known as heat lows. Thermal lows can be semipermanent features around some parts of Europe, particularly in the summer season. These thermal lows can be developed or created around Spain, Portugal, France etc., during the summer season because of the intense heat. Thermal low pressure can be located around the world, particularly in the summer or in tropical regions. Notable occurrences * 1788, 13 July, a hailstorm sweeps across France and the Dutch Republic with hailstones 'as big as quart bottles' that ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wokingham
Wokingham is a market town in Berkshire, England, west of London, southeast of Reading, north of Camberley and west of Bracknell. History Wokingham means 'Wocca's people's home'. Wocca was apparently a Saxon chieftain who may also have owned lands at Wokefield in Berkshire and Woking in Surrey. In Victorian times, the name became corrupted to ''Oakingham'', and consequently the acorn with oak leaves is the town's heraldic charge, granted in the 19th century. Geologically, Wokingham sits at the northern end of the Bagshot Formation, overlying London clay, suggesting a prehistorical origin as a marine estuary. The courts of Windsor Forest were held at Wokingham and the town had the right to hold a market from 1219. The Bishop of Salisbury was largely responsible for the growth of the town during this period. He set out roads and plots making them available for rent. There are records showing that in 1258 he bought the rights to hold three town fairs every year. E ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wimbledon, London
Wimbledon () is a district and town of Southwest London, England, southwest of the centre of London at Charing Cross; it is the main commercial centre of the London Borough of Merton. Wimbledon had a population of 68,187 in 2011 which includes the electoral wards of Abbey, Dundonald, Hillside, Trinity, Village, Raynes Park and Wimbledon Park. It is home to the Wimbledon Championships and New Wimbledon Theatre, and contains Wimbledon Common, one of the largest areas of common land in London. The residential and retail area is split into two sections known as the "village" and the "town", with the High Street being the rebuilding of the original medieval village, and the "town" having first developed gradually after the building of the railway station in 1838. Wimbledon has been inhabited since at least the Iron Age when the hill fort on Wimbledon Common is thought to have been constructed. In 1086 when the Domesday Book was compiled, Wimbledon was part of the manor of Mortlake. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Earlsfield
Earlsfield is an area within the London Borough of Wandsworth, London, England. It is a typical London suburb and comprises mostly residential Victorian terraced houses with a high street of shops, bars, and restaurants between Garratt Lane, Allfarthing Lane, and Burntwood Lane. The population of Earlsfield at the 2001 Census was 12,903, increasing to 15,448 at the 2011 Census. Earlsfield railway station provides access to central London (three stops to London Waterloo (Clapham Junction, Vauxhall, Waterloo) in 12 minutes) and other areas in South London (Victoria - changing at Clapham Junction, Wimbledon one stop). The station's redevelopment was completed in April 2013. History In medieval times, the area now known as Earlsfield was the northern part of the manor and hamlet of Garrat (also spelt Garratt, Garrett or Garret) in the parish of Wandsworth and notorious in the 18th century for the Garrat mock elections. By then the area was already industrialised with numerous m ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
South West Main Line
The South West Main Line (SWML) is a 143-mile (230 km) major railway line between Waterloo station in central London and Weymouth on the south coast of England. A predominantly passenger line, it serves many commuter areas including south western suburbs of London and the conurbations based on Southampton and Bournemouth. It runs through the counties of Surrey, Hampshire and Dorset. It forms the core of the network built by the London and South Western Railway, today mostly operated by South Western Railway. Network Rail refers to it as the South West Main Line. Operating speeds on much of the line are relatively high, with large stretches cleared for up to running. The London end of the line has as many as eight tracks plus the two Windsor Lines built separately, but this narrows to four by and continues this way until Worting Junction west of , from which point most of the line is double track. A couple of miles from the Waterloo terminus, the line runs briefly alongside ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bow Echo
A bow echo is the characteristic radar return from a mesoscale convective system that is shaped like an archer's bow. These systems can produce severe straight-line winds and occasionally tornadoes, causing major damage. They can also become derechos or form Line echo wave pattern (LEWP). Research The term "bow echo" was first used by Theodore Fujita in his May 1978 paper "Manual of Downburst Identification for Project NIMROD." In 2004, research was done to better anticipate the formation of bow echoes, specifically the formation of bow echoes from weakly organized squall lines and supercells. Researchers determined that bow echoes were most likely to occur in weakly organized cells. A Midwest Bow Echo Workshop was held in 2007, at which meteorologists gathered to share their research to better understand bow echoes. Formation A bow echo is associated with squall lines or lines of convective thunderstorms. These echoes can range in size from 20 to 200 km, and have a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rhine
), Surselva, Graubünden, Switzerland , source1_coordinates= , source1_elevation = , source2 = Rein Posteriur/Hinterrhein , source2_location = Paradies Glacier, Graubünden, Switzerland , source2_coordinates= , source2_elevation = , source_confluence = Reichenau , source_confluence_location = Tamins, Graubünden, Switzerland , source_confluence_coordinates= , source_confluence_elevation = , mouth = North Sea , mouth_location = Netherlands , mouth_coordinates = , mouth_elevation = , progression = , river_system = , basin_size = , tributaries_left = , tributaries_right = , custom_label = , custom_data = , extra = The Rhine ; french: Rhin ; nl, Rijn ; wa, Rén ; li, Rien; rm, label= Sursilvan, Rein, rm, label= Sutsilvan and Surmiran, Ragn, rm, label=Rumantsch Grischun, Vallader and Puter, Rain; it, Reno ; gsw, Rhi(n), inclu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pforzheim
Pforzheim () is a city of over 125,000 inhabitants in the federal state of Baden-Württemberg, in the southwest of Germany. It is known for its jewelry and watch-making industry, and as such has gained the nickname "Goldstadt" ("Golden City"). With an area of , it is situated between the cities of Stuttgart and Karlsruhe at the confluence of three rivers (Enz, Nagold and Würm). It marks the frontier between Baden and Württemberg, being located on Baden territory. From 1535-65, it was the home to the Margraves of Baden-Pforzheim. The City of Pforzheim does not belong to any administrative district (''Kreis''), although it hosts the administrative offices of the Enz district that surrounds the town. During World War II, Pforzheim was bombed by the Allies a number of times. The largest raid, and one of the most devastating area bombardments of World War II, was carried out by the Royal Air Force (RAF) on the evening of 23 February 1945. Nearly one third of the town's populati ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chew Stoke
Chew Stoke is a small village and civil parish in the affluent Chew Valley, in Somerset, England, about south of Bristol and 10 miles north of Wells. It is at the northern edge of the Mendip Hills, a region designated by the United Kingdom as an Area of Outstanding Natural Beauty, and is within the Bristol/ Bath green belt. The parish includes the hamlet of Breach Hill, which is approximately southwest of Chew Stoke itself. Chew Stoke has a long history, as shown by the number and range of its heritage-listed buildings. The village is at the northern end of Chew Valley Lake, which was created in the 1950s, close to a dam, pumping station, sailing club, and fishing lodge. A tributary of the River Chew, which rises in Strode, runs through the village. The population of 991 is served by one shop, one working public house, a primary school and a bowling club. Together with Chew Magna, it forms the ward of Chew Valley North in the unitary authority of Bath and North East Somerset ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chew Stoke Flood Of 1968
Chew Stoke Flood was a heavy rain event and severe flash flood which occurred on 10 July 1968, affecting Somerset and Southwest England in particular the Chew Valley and some areas of Bristol, notably Bedminster. The River Chew suffered a major flood in 1968 with serious damage to towns and villages along its route, including sweeping away the bridge at Pensford. On 10 July 1968, torrential rainfall, with falling in 18 hours on Chew Stoke, double the area's average rainfall for the whole of July, led to widespread flooding in the Chew Valley, and water reached the first floor of many buildings. The damage in Chew Stoke was not as severe as in some of the surrounding villages, such as Pensford where it swept away the bridge over the A37 and damaged the railway viaduct so badly that it never reopened. It also flooded 88 properties in Chew Magna with many being inundated with of water. Fears that the Chew Valley Lake dam would be breached caused considerable anxiety. On the sou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rain Dust
Rain dust or snow dust, traditionally known as muddy rain, red rain, or coloured rain, is a variety of rain (or any other form of precipitation) which contains enough desert dust for the dust to be visible without using a microscope. History The rain dust phenomenon was studied by Italian scientist Giuseppe Maria Giovene (1753–1837), who managed to correctly explain the phenomenon as early as 1803. On 7 March 1803, rain dust fell over Southern Italy's region Apulia. At that time, people believed that the rain was caused by the explosions of Italy's volcanoes Mount Vesuvius or Etna, or that it was due to the transport of matter coming from the sea floor and raised by vapor. Giuseppe Maria Giovene related the phenomenon to the wind which occurred prior to the rain event, and he came to the conclusion that the sand had come from Africa and that it had been pushed by the wind coming from south-east. Geography Rain dust is common in the Western and Southern Mediterranean, where ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
