Climate of England

Climate of England: England has a temperate climate, with plentiful rainfall all year round, although the seasons are quite variable in temperature. However, temperatures rarely fall below −5 °C (23 °F) or rise above 30 °C (86 °F). The prevailing wind is from the south-west, bringing mild and wet weather to England regularly from the Atlantic Ocean. It is driest in the east and warmest in the south, which is closest to the European mainland. Snowfall can occur in winter and early spring, although it is not that common away from high ground. England has warmer maximum and minimum temperatures throughout the year than the other countries of the UK, though Wales has milder minimums from November to February, and Northern Ireland has warmer maximums from December to February. England is also sunnier throughout the year, but unlike Wales, Northern Ireland and Scotland, the sunniest month is July, totalling 192.8 hours.

The highest temperature recorded in England is 38.5 °C (101.3 °F) on 10 August 2003 at Brogdale, near Faversham, in Kent. The lowest temperature recorded in England is −26.1 °C (−15.0 °F) on 10 January 1982 at Edgmond, near Shropshire. The climate of south-west England is rather distinct and somewhat milder than the rest of England, forming its own separate climate. Crops, flowers and plants can be grown much earlier in the South West than in the rest of England or the UK.

England has a temperate maritime climate meaning that it is mild with temperatures not much lower than 0 °C (32 °F) in winter and not much higher than 32 °C (90 °F) in summer. The weather is damp relatively frequently and is subject to change. The coldest months are January and February, the latter particularly on the English coast, while July is normally the warmest month. Months with mild to warm weather with least rainfall are May, June, September and October.

The biggest influences on the climate of England comes from the proximity to the Atlantic Ocean, its northern latitude and warming of the waters around the Gulf Stream. England receives quite a significant proportion of rainfall during the year, with autumn and winter being the wettest time—geographically the Lake District receives more rain than anywhere else in the country. Since weather recording records began, the highest temperature received was 38.5 °C (101.3 °F) on 10 August 2003 at Brogdale in Kent, while the lowest was −26.1 °C (−15.0 °F) on 10 January 1982 in Edgmond, Shropshire.

Geography of England

Geographically England comprises the central and southern two-thirds of the island of Great Britain, plus such offshore islands as the Isle of Wight and the Isles of Scilly. It is bordered by two fellow countries of the United Kingdom—to the north by Scotland and to the west by Wales. England is closer to the European Continent than any other part of mainland Britain. It is separated from France by a 34-kilometre (21 mi) sea gap, though the two countries are connected by the Channel Tunnel near Folkestone. As England is on an island, it is surrounded by the water of the Irish Sea, North Sea and Atlantic Ocean.

Geography of England: The most important rivers in England, because of their ports of London, Liverpool, and Newcastle, are the tidal rivers Thames, Mersey and Tyne. The tides raise the level of water in their estuaries and enable ships to enter the ports. At 354 kilometres (220 mi), the Severn is the longest river flowing through England. It empties into the Bristol Channel and is notable for its Severn Bore tidal waves, which can reach 2 metres (6.6 ft) in height. However, the longest river entirely in England is the Thames, which is 346 kilometres (215 mi) in length. There are many lakes in England but the majority are in the aptly named Lake District; the largest of which is Windermere, it is known by the nickname "Queen of Lakes".

In geological terms, the Pennines, known as the "backbone of England", are the oldest range of mountains the country, originating from the end of the Paleozoic Era around 300 million years ago. The total length of the Pennines is 400 kilometres (250 mi), peaking at Cross Fell in Cumbria. The material of which they are composed is mostly sandstone and limestone, but also coal. There are karst landscapes in calcite areas such as parts of Yorkshire and Derbyshire. The Pennine landscape is high moorland in upland areas, indented by fertile valleys of the region's rivers. They contain three national parks, the Yorkshire Dales, Northumberland, and the Peak District. The highest point in England, at 978 metres (3,209 ft), is Scafell Pike in Cumbria. Straddling the border between England and Scotland are the Cheviot Hills.

The English Lowlands are to the south of the Pennines, consisting of green rolling hills, including the Cotswold Hills, Chiltern Hills, North and South Downs—where they meet the sea they form white rock exposures such as the cliffs of Dover. The granitic Southwest Peninsula in the West Country provides upland moorland, such as Dartmoor and Exmoor, which flourish with a mild climate; both are national parks.

Geography of England