A snowdrift is a deposit of snow sculpted by wind into a mound during a snowstorm. Snowdrifts resemble sand dunes and are formed in a similar manner, namely, by wind moving light snow and depositing it when the wind has stopped against a stationary object. Snow crests and slopes off toward the surface on the windward side of a large object. On the leeward side, areas near the object are a bit lower than surrounding areas, but are flatter; the impact of snowdrifts on transportation can be more significant than the snowfall itself, such as in the USA during the Great Blizzard of 1978. Snowdrifts are many times found at or on roads, as the crest of the roadbed or the furrows along the road create the disruption to the wind needed to shed its carried snow. Snow fences may be employed on the windward side of the road to intentionally create a drift before the snow-laden wind reaches the road. Blizzard Lake-effect snow Snow Snow removal Snowdrift Exhibit at Evansville Museum
The River Thames, known alternatively in parts as the Isis, is a river that flows through southern England including London. At 215 miles, it is the longest river in England and the second longest in the United Kingdom, after the River Severn, it flows through Oxford, Henley-on-Thames and Windsor. The lower reaches of the river are called the Tideway, derived from its long tidal reach up to Teddington Lock, it rises at Thames Head in Gloucestershire, flows into the North Sea via the Thames Estuary. The Thames drains the whole of Greater London, its tidal section, reaching up to Teddington Lock, includes most of its London stretch and has a rise and fall of 23 feet. Running through some of the driest parts of mainland Britain and abstracted for drinking water, the Thames' discharge is low considering its length and breadth: the Severn has a discharge twice as large on average despite having a smaller drainage basin. In Scotland, the Tay achieves more than double the Thames' average discharge from a drainage basin, 60% smaller.
Along its course are 45 navigation locks with accompanying weirs. Its catchment area covers a small part of western England; the river contains over 80 islands. With its waters varying from freshwater to seawater, the Thames supports a variety of wildlife and has a number of adjoining Sites of Special Scientific Interest, with the largest being in the remaining parts of the North Kent Marshes and covering 5,449 hectares; the Thames, from Middle English Temese, is derived from the Brittonic Celtic name for the river, recorded in Latin as Tamesis and yielding modern Welsh Tafwys "Thames". The name may have meant "dark" and can be compared to other cognates such as Russian темно, Lithuanian tamsi "dark", Latvian tumsa "darkness", Sanskrit tamas and Welsh tywyll "darkness" and Middle Irish teimen "dark grey"; the same origin is shared by countless other river names, spread across Britain, such as the River Tamar at the border of Devon and Cornwall, several rivers named Tame in the Midlands and North Yorkshire, the Tavy on Dartmoor, the Team of the North East, the Teifi and Teme of Wales, the Teviot in the Scottish Borders, as well as one of the Thames' tributaries called the Thame.
Kenneth H. Jackson has proposed that the name of the Thames is not Indo-European, while Peter Kitson suggested that it is Indo-European but originated before the Celts and has a name indicating "muddiness" from a root *tā-,'melt'. Indirect evidence for the antiquity of the name'Thames' is provided by a Roman potsherd found at Oxford, bearing the inscription Tamesubugus fecit, it is believed. Tamese was referred to as a place, not a river in the Ravenna Cosmography; the river's name has always been pronounced with a simple t /t/. A similar spelling from 1210, "Tamisiam", is found in the Magna Carta; the Thames through Oxford is sometimes called the Isis. And in Victorian times and cartographers insisted that the entire river was named the Isis from its source down to Dorchester on Thames and that only from this point, where the river meets the Thame and becomes the "Thame-isis" should it be so called. Ordnance Survey maps still label the Thames as "River Isis" down to Dorchester. However, since the early 20th century this distinction has been lost in common usage outside of Oxford, some historians suggest the name Isis is nothing more than a truncation of Tamesis, the Latin name for the Thames.
Sculptures titled Tamesis and Isis by Anne Seymour Damer can be found on the bridge at Henley-on-Thames, Oxfordshire. Richard Coates suggests that while the river was as a whole called the Thames, part of it, where it was too wide to ford, was called *lowonida; this gave the name to a settlement on its banks, which became known as Londinium, from the Indo-European roots *pleu- "flow" and *-nedi "river" meaning something like the flowing river or the wide flowing unfordable river. For merchant seamen, the Thames has long been just the "London River". Londoners refer to it as "the river" in expressions such as "south of the river"; the river gives its name to three informal areas: the Thames Valley, a region of England around the river between Oxford and West London. Thames Valley Police is a formal body. In non-administrative use, the river's name is used in those of Thames Valley University, Thames Water, Thames Television, publishing company Thames & Hudson and South Thames College. An example of its use in the names of historic entities is the Thames Ironworks and Shipbuilding Company.
The administrative powers of the Thames Conservancy have been taken on with modifications by the Environment Agency and, in respect of the Tideway part of the river, such powers are split between the agency and the Port of London Authority. The marks of human activity, in some cases dating back to Pre-Roman Britain, are visible at various points along the river; these include a variety of structure
Electric power transmission
Electric power transmission is the bulk movement of electrical energy from a generating site, such as a power plant, to an electrical substation. The interconnected lines which facilitate this movement are known as a transmission network; this is distinct from the local wiring between high-voltage substations and customers, referred to as electric power distribution. The combined transmission and distribution network is known as the "power grid" in North America, or just "the grid". In the United Kingdom, Myanmar and New Zealand, the network is known as the "National Grid". A wide area synchronous grid known as an "interconnection" in North America, directly connects a large number of generators delivering AC power with the same relative frequency to a large number of consumers. For example, there are four major interconnections in North America. In Europe one large grid connects most of continental Europe. Transmission and distribution lines were owned by the same company, but starting in the 1990s, many countries have liberalized the regulation of the electricity market in ways that have led to the separation of the electricity transmission business from the distribution business.
Most transmission lines are high-voltage three-phase alternating current, although single phase AC is sometimes used in railway electrification systems. High-voltage direct-current technology is used for greater efficiency over long distances. HVDC technology is used in submarine power cables, in the interchange of power between grids that are not mutually synchronized. HVDC links are used to stabilize large power distribution networks where sudden new loads, or blackouts, in one part of a network can result in synchronization problems and cascading failures. Electricity is transmitted at high voltages to reduce the energy loss which occurs in long-distance transmission. Power is transmitted through overhead power lines. Underground power transmission has a higher installation cost and greater operational limitations, but reduced maintenance costs. Underground transmission is sometimes used in environmentally sensitive locations. A lack of electrical energy storage facilities in transmission systems leads to a key limitation.
Electrical energy must be generated at the same rate. A sophisticated control system is required to ensure that the power generation closely matches the demand. If the demand for power exceeds supply, the imbalance can cause generation plant and transmission equipment to automatically disconnect or shut down to prevent damage. In the worst case, this may lead to a cascading series of a major regional blackout. Examples include the US Northeast blackouts of 1965, 1977, 2003, major blackouts in other US regions in 1996 and 2011. Electric transmission networks are interconnected into regional and continent wide networks to reduce the risk of such a failure by providing multiple redundant, alternative routes for power to flow should such shut downs occur. Transmission companies determine the maximum reliable capacity of each line to ensure that spare capacity is available in the event of a failure in another part of the network. High-voltage overhead conductors are not covered by insulation; the conductor material is nearly always an aluminum alloy, made into several strands and reinforced with steel strands.
Copper was sometimes used for overhead transmission, but aluminum is lighter, yields only marginally reduced performance and costs much less. Overhead conductors are a commodity supplied by several companies worldwide. Improved conductor material and shapes are used to allow increased capacity and modernize transmission circuits. Conductor sizes range from 12 mm2 with varying resistance and current-carrying capacity. For normal AC lines thicker wires would lead to a small increase in capacity due to the skin effect; because of this current limitation, multiple parallel cables are used when higher capacity is needed. Bundle conductors are used at high voltages to reduce energy loss caused by corona discharge. Today, transmission-level voltages are considered to be 110 kV and above. Lower voltages, such as 66 kV and 33 kV, are considered subtransmission voltages, but are used on long lines with light loads. Voltages less than 33 kV are used for distribution. Voltages above 765 kV are considered extra high voltage and require different designs compared to equipment used at lower voltages.
Since overhead transmission wires depend on air for insulation, the design of these lines requires minimum clearances to be observed to maintain safety. Adverse weather conditions, such as high wind and low temperatures, can lead to power outages. Wind speeds as low as 23 knots can permit conductors to encroach operating clearances, resulting in a flashover and loss of supply. Oscillatory motion of the physical line can be termed gallop or flutter depending on the frequency and amplitude of oscillation. Electric power can be transmitted by underground power cables instead of overhead power lines. Underground cables take up less right-of-way than overhead lines, have lower visibility, are less affected by bad weather. However, costs of insulated cable and excavation are much higher
Dunkirk, is a commune in Nord, a French department in northern France. It is the most northern city of France, it has the third-largest French harbour. The population of the commune at the 2016 census was 91,412; the name of Dunkirk derives from West Flemish dun'dune' or'dun' and kerke'church', which together means'church in the dunes'. Until the middle of the 20th century, the city was situated in the French Flemish area. Today Dunkirk is the world's northernmost Francophone city. A fishing village arose late in the tenth century, in the flooded coastal area of the English Channel south of the Western Scheldt, when the area was held by the Counts of Flanders, vassals of the French Crown. About 960AD, Count Baldwin III had a town wall erected in order to protect the settlement against Viking raids; the surrounding wetlands were cultivated by the monks of nearby Bergues Abbey. The name Dunkirka was first mentioned in a tithe privilege of 27 May 1067, issued by Count Baldwin V of Flanders. Count Philip I brought further large tracts of marshland under cultivation, laid out the first plans to build a Canal from Dunkirk to Bergues and vested the Dunkirkers with market rights.
In the late 13th century, when the Dampierre count Guy of Flanders entered into the Franco-Flemish War with his suzerain King Philippe IV of France, the citizens of Dunkirk sided with the French against their count, who at first was defeated at the 1297 Battle of Furnes, but reached de facto autonomy upon the victorious Battle of the Golden Spurs five years and exacted vengeance. Guy's son, Count Robert III granted further city rights to Dunkirk. Count Louis remained a loyal liensman of the French king upon the outbreak of the Hundred Years' War with England in 1337, prohibited the maritime trade, which led to another revolt by the Dunkirk citizens. After the count had been killed in the 1346 Battle of Crécy, his son and successor Count Louis II of Flanders signed a truce with the English. However, in the course of the Western Schism from 1378, English supporters of Pope Urban VI disembarked at Dunkirk, captured the city and flooded the surrounding estates, they left great devastations in and around the town.
Upon the extinction of the Counts of Flanders with the death of Louis II in 1384, Flanders was acquired by the Burgundian, Duke Philip the Bold. The fortifications were again enlarged, including the construction of a belfry daymark; as a strategic point, Dunkirk has always been exposed to political covetousness, by Duke Robert I of Bar in 1395, by Louis de Luxembourg in 1435 and by the Austrian archduke Maximilian I of Habsburg, who in 1477 married Mary of Burgundy, sole heiress of late Duke Charles the Bold. As Maximilian was the son of Emperor Frederick III, all Flanders was seized by King Louis XI of France. However, the archduke defeated the French troops in 1479 at the Battle of Guinegate; when Mary died in 1482, Maximilian retained Flanders according to the terms of the 1482 Treaty of Arras. Dunkirk, along with the rest of Flanders, was incorporated into the Habsburg Netherlands and upon the 1581 secession of the Seven United Netherlands, remained part of the Southern Netherlands, which were held by Habsburg Spain as Imperial fiefs.
The area remained much disputed between the Kingdom of Spain, the United Netherlands, the Kingdom of England and the Kingdom of France. At the beginning of the Eighty Years' War, Dunkirk was in the hands of the Dutch rebels, from 1577. Spanish forces under Duke Alexander Farnese of Parma re-established Spanish rule in 1583 and it became a base for the notorious Dunkirkers; the Dunkirkers lost their home port when the city was conquered by the French in 1646 but Spanish forces recaptured the city in 1652. In 1658, as a result of the long war between France and Spain, it was captured after a siege by Franco-English forces following the battle of the Dunes; the city along with Fort-Mardyck was awarded to England in the peace the following year as agreed in the Franco-English alliance against Spain. The English governors were Sir Edward Harley and Lord Rutherford, it came under French rule when King Charles II of England sold it to France for £320,000 on 17 October 1662. The French government developed the town as a fortified port.
The town's existing defences were adapted to create ten bastions. The port was expanded in the 1670s by the construction of a basin that could hold up to thirty warships with a double lock system to maintain water levels at low tide; the basin was linked to the sea by a channel. This work was completed by 1678; the jetties were defended a few years by the construction of five forts, Château d'Espérance, Château Vert, Grand Risban, Château Gaillard, Fort de Revers. An additional fort was built in 1701 called Fort Blanc; the jetties, their forts, the port facilities were demolished in 1713 under the terms of the Treaty of Utrecht. During
An anticyclone is a weather phenomenon defined by the United States National Weather Service's glossary as "a large-scale circulation of winds around a central region of high atmospheric pressure, clockwise in the Northern Hemisphere, counterclockwise in the Southern Hemisphere". Effects of surface-based anticyclones include clearing skies as well as drier air. Fog can form overnight within a region of higher pressure. Mid-tropospheric systems, such as the subtropical ridge, deflect tropical cyclones around their periphery and cause a temperature inversion inhibiting free convection near their center, building up surface-based haze under their base. Anticyclones aloft can form within warm core lows such as tropical cyclones, due to descending cool air from the backside of upper troughs such as polar highs, or from large scale sinking such as the subtropical ridge; the evolution of an anticyclone depends on a few variables such as its size, moist-convection, Coriolis force etc. Sir Francis Galton first discovered anticyclones in the 1860s.
Preferred areas within a synoptic flow pattern in higher levels of the hydrosphere are beneath the western side of troughs, or dips in the Rossby wave pattern. High-pressure systems are alternatively referred to as anticyclones, their circulation is sometimes referred to as cum sole. Subtropical high pressure zones form under the descending portion of the Hadley cell circulation. Upper-level high-pressure areas lie over tropical cyclones due to their warm core nature. Surface anticyclones form due to downward motion through the troposphere, the atmospheric layer where weather occurs. Preferred areas within a synoptic flow pattern in higher levels of the troposphere are beneath the western side of troughs. On weather maps, these areas show converging winds known as confluence, or converging height lines near or above the level of non-divergence, near the 500 hPa pressure surface about midway up the troposphere; because they weaken with height, these high-pressure systems are cold. Heating of the earth near the equator forces upward motion and convection along the monsoon trough or intertropical convergence zone.
The divergence over the near-equatorial trough leads to air rising and moving away from the equator aloft. As air moves towards the mid-latitudes, it cools and sinks leading to subsidence near the 30° parallel of both hemispheres; this circulation known as the Hadley cell forms the subtropical ridge. Many of the world's deserts are caused by these climatological high-pressure areas; because these anticyclones strengthen with height, they are known as warm core ridges. The development of anticyclones aloft occurs in warm core cyclones such as tropical cyclones when latent heat caused by the formation of clouds is released aloft increasing the air temperature. In the absence of rotation, the wind tends to blow from areas of high pressure to areas of low pressure; the stronger the pressure difference between a high-pressure system and a low-pressure system, the stronger the wind. The coriolis force caused by Earth's rotation gives winds within high-pressure systems their clockwise circulation in the northern hemisphere and anticlockwise circulation in the southern hemisphere.
Friction with land slows down the wind flowing out of high-pressure systems and causes wind to flow more outward from the center. High-pressure systems are associated with light winds at the surface and subsidence of air from higher portions of the troposphere. Subsidence will warm an air mass by adiabatic heating. Thus, high pressure brings clear skies; because no clouds are present to reflect sunlight during the day, there is more incoming solar radiation and temperatures rise near the surface. At night, the absence of clouds means that outgoing longwave radiation is not blocked, giving cooler diurnal low temperatures in all seasons; when surface winds become light, the subsidence produced directly under a high-pressure system can lead to a buildup of particulates in urban areas under the high pressure, leading to widespread haze. If the surface level relative humidity rises towards 100 percent overnight, fog can form; the movement of continental arctic air masses to lower latitudes produces strong but vertically shallow high-pressure systems.
The surface level, sharp temperature inversion can lead to areas of persistent stratocumulus or stratus cloud, colloquially known as anticyclonic gloom. The type of weather brought about by an anticyclone depends on its origin. For example, extensions of the Azores high pressure may bring about anticyclonic gloom during the winter because they pick up moisture as they move over the warmer oceans. High pressures that build to the north and move southwards bring clear weather because they are cooled at the base which helps prevent clouds from forming. Once arctic air moves over an unfrozen ocean, the air mass modifies over the warmer water and takes on the character of a maritime air mass, which reduces the strength of the high-pressure system; when cold air moves over warm oceans, polar lows can develop. However and moist air masses which move poleward from tropical sources are slower to modify than arctic air masses; the circulation around mid-level ridges, the air subsidence at their center, act to steer tropical cyclones ar
Sutherland is a historic county, registration county and lieutenancy area in the Highlands of Scotland. Its county town is Dornoch. Sutherland borders Caithness to the east, Ross-shire to the south and the Atlantic to the north and west. Like its southern neighbour Ross-shire, Sutherland has some of the most dramatic scenery in the whole of Europe on its western fringe where the mountains meet the sea; these include high sea cliffs, old mountains composed of Precambrian and Cambrian rocks. The name Sutherland dates from the era of Norwegian Viking rule and settlement over much of the Highlands and Islands, under the rule of the jarl of Orkney. Although it contains some of the northernmost land in the island of Great Britain, it was called Suðrland from the standpoint of Orkney and Caithness. In Gaelic, the area is referred to according to its traditional areas: Dùthaich MhicAoidh in the northeast, Asainte in the west, Cataibh in the east. Cataibh is sometimes used to refer to the area as a whole.
The northwest corner of Sutherland, traditionally known as the Province of Strathnaver, was not incorporated into Sutherland until 1601. This was the home of the powerful and warlike Clan Mackay, as such was named in Gaelic, Dùthaich'Ic Aoidh, the Homeland of Mackay. Today this part of Sutherland is known as Mackay Country, unlike other areas of Scotland where the names traditionally associated with the area have become diluted, there is still a preponderance of Mackays in the Dùthaich. Much of the population is based in coastal towns, such as Helmsdale and Lochinver, which until recently made much of their living from the rich fishing of the waters around the British Isles. Much of Sutherland is poor relative to the rest of Scotland, with few job opportunities beyond government funded employment and seasonal tourism. Further education is provided by North Highland College, part of the University of the Highlands and Islands; the Ross House Campus in Dornoch was the first establishment in the United Kingdom to provide a degree in golf management.
The Burghfield House Campus in Dornoch, is the home for the Centre for History teaching undergraduate and postgraduate history degrees to students around the UHI network and worldwide. The inland landscape is rugged and sparsely populated. Despite being Scotland's fifth-largest county in terms of area, it has a smaller population than a medium-size Lowland Scottish town, it stretches from the Atlantic across to the North Sea. The sea-coasts boast high cliffs and deep fjords in the east and north, ragged inlets on the west and sandy beaches in the north; the remote far northwest point of Sutherland, Cape Wrath, is the most northwesterly point in Scotland. The county has many fine beaches, a remote example being Sandwood Bay, which can only be reached by foot along a rough track; the number of visiting tourists is minimal. Sutherland has many rugged mountains such as the most northerly Munro; the western part comprises Torridonian sandstone underlain by Lewisian gneiss. The spectacular scenery has been created by denudation to form isolated sandstone peaks such as Foinaven, Arkle, Cùl Mór and Suilven.
Such mountains are attractive for hill scrambling, despite their remote location. Together with similar peaks to the south in Wester Ross, such as Stac Pollaidh, they have a unique structure with great scope for exploration. On the other hand, care is needed when bad weather occurs owing to their isolation and the risks of injury. Owing to its isolation from the rest of the country, Sutherland was reputedly the last haunt of the native wolf, the last survivor being shot in the 18th century. However, other wildlife has survived, including the golden eagle, sea eagle and pine marten amongst other species which are rare in the rest of the country. There are pockets of remnants of the original Caledonian Forest; the importance of the county's scenery is recognised by the fact that 4 of Scotland's 40 national scenic areas are located here. The purpose of the NSA designation is to identify areas of exceptional scenery and to ensure its protection from inappropriate development; the areas protected by the designation are considered to represent the type of scenic beauty "popularly associated with Scotland and for which it is renowned".
The four NSAs within Sutherland are: The Assynt-Coigach NSA has many distinctively shaped mountains, including Quinag, Suilven, Cùl Mòr, Stac Pollaidh and Ben More Assynt, that rise steeply from the surrounding "cnoc and lochan" scenery. These can appear higher than their actual height would indicate due to their steep sides and the contrast with the moorland from which they rise. Assynt lies within Sutherland, whilst Coigach lies within Cromarty; the Dornoch Firth NSA straddles the boundary between Sutherland and Ross and Cromarty, covers a variety of landscapes surrounding the narrow and sinuous firth. The Kyle of Tongue NSA covers the mountains of Ben Hope and Ben Loyal, as well as woodlands and crofting settlements on the shoreline of the kyle itself; the North West Sutherland NSA covers the mountains of Foinaven and Ben Stack as well as the coastal scenery surrounding Loch Laxford and Handa Island. The A9 road main east coast road is challenging north of Helmsdale at the notorious Berriedale Braes, there are few inland roads.
The Far North Line north-south single-track railway line was extended through Sutherland by the Highland Railway between 1868 and 1871. It enters Sutherland near Invershin and runs along the east coast as far as possible, but an inland diversion was necessary from Helmsdale along the Strath of Kildonan; the line
South West England
South West England is one of nine official regions of England. It is the largest in area, covering 9,200 square miles, consists of the counties of Gloucestershire, Wiltshire, Dorset and Cornwall, as well as the Isles of Scilly. Five million people live in South West England; the region includes much of the ancient kingdom of Wessex. The largest city is Bristol. Other major urban centres include Plymouth, Gloucester, Exeter, Bath and the South East Dorset conurbation which includes Bournemouth and Christchurch. There are eight cities: Salisbury, Wells, Gloucester, Exeter and Truro, it includes two entire national parks and Exmoor. The northern part of Gloucestershire, near Chipping Campden, is as close to the Scottish border as it is to the tip of Cornwall; the region has by far the longest coastline of any English region. The region is at the first level of NUTS for Eurostat purposes. Key data and facts about the region are produced by the South West Observatory. Following the abolition of the South West Regional Assembly and Government Office, local government co-ordination across the region is now undertaken by South West Councils.
The region is known for its rich folklore, including the legend of King Arthur and Glastonbury Tor, as well as its traditions and customs. Cornwall has its own language and some regard it as a Celtic nation; the South West is known for Cheddar cheese. It is home to the Eden Project, Aardman Animations, the Glastonbury Festival, the Bristol International Balloon Fiesta, trip hop music and Cornwall's surfing beaches; the region has been home to some of Britain's most renowned writers, including Daphne du Maurier and Agatha Christie, both of whom set many of their works here, the South West is the location of Thomas Hardy's Wessex, the setting for many of his best-known novels. Most of the region is located on the South West Peninsula, between the English Channel and Bristol Channel, it has the longest coastline of all the English regions, totalling over 700 miles. Much of the coast is now protected from further substantial development because of its environmental importance, which contributes to the region's attractiveness to tourists and residents.
Geologically the region is divided into the igneous and metamorphic west and sedimentary east, the dividing line to the west of the River Exe. Cornwall and West Devon's landscape is of rocky coastline and high moorland, notably at Bodmin Moor and Dartmoor; these are due to the slate that underlie the area. The highest point of the region is High Willhays, at 2,038 feet, on Dartmoor. In North Devon the slates of the west and limestones of the east meet at Exmoor National Park; the variety of rocks of similar ages seen here have led to the county's name being lent to that of the Devonian period. The east of the region is characterised by limestone downland; the vales, with good irrigation, are home to the region's dairy agriculture. The Blackmore Vale was Thomas Hardy's "Vale of the Little Dairies"; the Southern England Chalk Formation extends into the region, creating a series of high, sparsely populated and archaeologically rich downs, most famously Salisbury Plain, but Cranborne Chase, the Dorset Downs and the Purbeck Hills.
These downs are the principal area of arable agriculture in the region. Limestone is found in the region, at the Cotswolds, Quantock Hills and Mendip Hills, where they support sheep farming. All of the principal rock types can be seen on the Jurassic Coast of Dorset and East Devon, where they document the entire Mesozoic era from west to east; the climate of South West England is classed as oceanic according to the Köppen climate classification. The oceanic climate experiences cool winters with warmer summers and precipitation all year round, with more experienced in winter. Annual rainfall is up to 2,000 millimetres on higher ground. Summer maxima averages range from 18 °C to 22 °C and winter minimum averages range from 1 °C to 4 °C across the south-west, it is the second windiest area of the United Kingdom, the majority of winds coming from the south-west and north-east. Government organisations predict the region to rise in temperature and become the hottest region in the United Kingdom. Inland areas of low altitude experience the least amount of precipitation.
They experience the highest summer maxima temperatures. Snowfalls are less so in comparison to higher ground, it experiences the lowest wind speeds and sunshine total in between that of the moors. The climate of inland areas is more noticeable the further north-east into the region. In comparison to inland areas, the coast experiences high minimum temperatures in winter, it experiences lower maximum temperatures during the summer. Rainfall is the lowest at the coast and snowfall is rarer than the rest of the region. Coastal areas are the windiest parts of the peninsula and they receive the most sunshine; the general coastal climate is more typical the further south-west into the region. Areas of moorland inland such as: Bodmin Moor and Exmoor experience lower temperatures and more precipitation than the rest of the south west (approxima