Since daily meteorological records began in Britain in the 17th century, there have been a number of severe winters. The coldest of all was probably 1684, when the diarist John Evelyn took a coach to Lambeth along the frozen River Thames.

There was an exceptionally cold and protracted winter in 1739/40 when, between November 1739 and May 1740, snow fell on 39 days in the London area. January in both 1795 and 1814 were colder than January 1740, and the month of February in 1855, 1895 and 1947 were colder than February 1740.

England and Wales would have to wait 223 years for a winter as cold as 1740: 1963.

But what was so remarkable about the 1739/40, however, is that the mean temperatures of both January and February were below 0 °C in the Midlands and southern England. The only other known instance of two successive months with mean temperatures below freezing took place in December 1878 and January 1879.

From 22 January to 17 March in 1947, snow fell every day somewhere in the UK, with the weather so cold that the snow accumulated. The temperature seldom rose more than a degree or two above freezing.

There were several snowfalls of 60 cm or more, and depths of level snow reached 150 cm in upper Teesdale and the Denbighshire Hills. Across Britain, drifts more than five metres deep blocked roads and railways. People were cut off for days. The armed services dropped supplies by helicopter to isolated farmsteads and villages, and helped to clear roads and railways.

In mid January 1947, no-one expected the winter to go down in the annals as the snowiest since 1814 and among the coldest on record. After two cold spells that had failed to last - one before Christmas 1946, the other during the first week of January - the weather had turned unseasonably mild.

During the night of 15-16 January, the temperature at Leeming in North Yorkshire didn't fall below 11.7 °C. The following day, maximum temperatures close to 14 °C were recorded in Norfolk, Herefordshire and Flintshire. All this was soon to change.

An area of high pressure moved northwards from France on 18 January. Two days later, the anticyclone was centred off north-west Norway. It then drifted south-east to southern Scandinavia, and dominated weather over the British Isles for the rest of the month. The first night frost came on the 20th and the winter began in earnest on the 23rd, when snow fell heavily over the south and south-west of England. Even in the Isles of Scilly, a few centimetres of snow fell. The blizzard in south-west England was the worst since 1891; many villages in Devon were isolated.

Fig 2 0600 UTC on 31 January 1947. A low near the channel islands and high over southern Scandinavia, a typical pressure situation during the 1947 winter. Occlusion giving snow over southern counties of England.

• On no day in February 1947 did the temperature at Kew Observatory top 4.4 °C, and only twice in the month was the night minimum temperature above 0 °C
• The mean maximum temperature for the month was 0.5 °C (6.9 °C below average) and the mean minimum was -2.7 °C (4.6 °C below average)
• On 26 of the month's 28 days, snow was lying at 0900 UTC
• South of a line from The Wash to the River Dee, mean maximum temperatures were everywhere more than 5.5 °C below average and, in some places, more than 7 °C below average
• Mean minimum temperatures were more than 4 °C below average everywhere in the south and south-west of England, and almost 6 °C below average in some places

February 1947 was the coldest February on record in many places and, for its combination of low temperatures with heavy snow, bore comparison with January 1814.

One notable feature of February 1947 was the lack of precipitation in parts of western Scotland. Because of the persistent anticyclonic conditions, some places that were normally very wet had no rain at all. A completely dry month in western Scotland is unusual. It was unprecedented in February

Another unusual feature of February 1947 was the lack of sunshine in the Midlands and south of England - a complete contrast to the north-west of Scotland, where the weather was unusually sunny.

At Kew, Nottingham and Edgbaston, there was no sun on 22 of the month's 28 days. At Kew, there was none at all from the 2nd to the 22nd. Hardly anywhere in the Midlands and southern England did the sunshine totals for the month exceed 40 percent of average.

When skies did clear, night-time temperatures plunged. A minimum of -21 °C was recorded at Woburn in Bedfordshire early on 25 February. Without the cloud, the month would almost certainly have been even colder than it was, certainly at night.

Meanwhile, mild air with a temperature of 7-10 °C edged into the extreme south-west of the British Isles on 10 March, bringing rain. The ensuing thaw was rapid. By the evening of 11 March, vast areas of southern England were under water. After weeks of frost, the ground was frozen hard. The rain and melt-water couldn't soak into the ground. Surface run-off was the only option.

The warm air spread northwards and eastwards. Melt-water from the Welsh mountains poured into the valleys of the Severn and Wye, flooding Herefordshire and Gloucestershire. The rivers of the English Midlands burst their banks. By 13 March, Fenland rivers were close to overspilling.

On 15 March, a deepening depression from the Atlantic approached the British Isles, bringing rain and severe gales. During the afternoon of 16 March, mean winds over southern England reached 50 knots, with gusts of 80-90 knots.

Buildings were damaged and waves were whipped up on floodwaters. In East Anglia, where the major rivers flow north-eastwards, the south-westerly wind drove water before it and waves pounded the dykes. Water levels rose and the dykes gave way. Most of Fenland was inundated. Troops were called in, but they could do little to stop water pouring through the breached dykes.

River levels rose relentlessly. For example, the banks of the Trent burst at Nottingham on 18 March and hundreds of homes were flooded, many to first floor level. When floodwater reached the tidal part of the Trent, it was impeded by a spring tide, and the whole of the lower Trent valley was flooded.

The floods in the West Country subsided after 20 March, but rivers continued to rise in eastern England. The Wharfe, Derwent, Aire and Ouse all burst their banks and flooded a huge area of southern Yorkshire. The town of Selby was almost completely under water. Only the ancient abbey and a few streets around the market place escaped inundation. 70 percent of all houses in the town were flooded.

The cold and snowy weather had, at last, ended, but the misery of the floods continued into the spring. And to make matters worse, the severe difficulties caused by the winter of 1947 were aggravated by the fuel and food shortages that remained after the Second World War.

Fig 4: Maximum and minimum temperatures
Edgbaston, Warwickshire 15 Dec 1946-16 Mar 1947

View the Central England Temperature pages

The winter of 1962/63 was the coldest over England and Wales since 1740. As in 1947, anticyclones to the north and east of the British Isles brought bitterly cold winds from the east day after day. As in 1947, depressions followed tracks to southward of the British Isles and their fronts brought snow to England, Wales and the southernmost parts of Scotland.

Mean maximum temperatures for January 1963 were more than 5 °C below average over most of Wales, the Midlands and southern England and in some places more than 7 °C below average. Mean minimum temperatures over this area were equally far below average. The story was much the same in February.

The winter began abruptly, just before Christmas 1962. The weather in the first three weeks of December was changeable and sometimes stormy. From the 4th to the 6th, London experienced its worst spell of fog since the Great Smog of 1952.

10 days later, the weather was particularly wet and stormy, with a gust of 88 knots recorded at Blackpool during the night of 15/16 December, the strongest since records began in 1946. The weather situation changed markedly on 22 December. On the 23rd, high pressure extended all the way from the southern Baltic to Cornwall, bringing cold easterly winds to much of England and Wales.

A belt of rain over northern Scotland on 24 December turned to snow as it moved south, giving Glasgow its first White Christmas since 1938. The snow belt reached southern England on Boxing Day and became almost stationary. The following day, snow lay five centimetres deep in the Channel Islands and 30 cm deep in much of southern England.

A blizzard over south-west England and South Wales on 29 and 30 December brought snowdrifts 6 m deep. Villages were cut off, some for several days. Roads and railways were blocked. Telephone wires were brought down. Stocks of food ran low. Farmers couldn't reach their livestock. Thousands of sheep, ponies and cattle starved to death.

Fig 5 The start of the winter: the cold front that brought the snow to England on 26 December 1962. Chart for 0600 UTC on 26 December.

From Boxing Day 1962 to early March 1963, much of England was under snow continuously. Unlike the winter of 1947, however, 1962/63 was sunnier than average in most parts of the area affected, considerably so in some places. Manchester's sunshine total for January was more than twice the average, for example. Even in the south of England, where snow fell frequently, sunshine totals were above average in most places. The most remarkable feature of the 1962/63 winter was not so much its snowiness as its coldness. The winter of 1947 was snowier than 1962/63, but not as cold.

In January 1963, there were 25 or more air frosts almost everywhere in southern England and South Wales. In February 1963, air frost occurred every night at Durham, and almost every night in the English Midlands. At several stations in southern England and South Wales, mean maximum temperatures were below 0 °C in January and little higher in February. Mean minimum temperatures were well below freezing almost everywhere in England, Wales and Scotland away from coasts. Extremely low temperatures were recorded - for example, a minimum of -22.2 °C was recorded at Braemar on 18 January.

Fig 6: Maximum and minimum temperatures
Leckford, Hampshire 8 Dec 1962 - 9 Mar 1963

Lakes and rivers froze. Ice formed on harbours in the south and east of England. Patches of ice formed on the sea. Huge blocks of ice formed on beaches where waves broke and the spray froze. Coastal marine life suffered severely.

Fig 7: Coastal areas were affected by ice Photo © Lynn Tait Gallery

As in 1947, so it was in the winter of 1962/63: brief thaws occurred from time to time, and winter didn't fully relax its grip before early March. In the last few days of February and the first few days of March 1963, sunny weather brought afternoon temperatures of 4 or 5 °C, but clear skies allowed temperatures to plummet at night. Frosts were moderate or severe. At last, on 4 March, a mild south-westerly flow of air reached the British Isles. There was occasional rain that day in most parts of Britain, and further rain the following day in the west and north, this time prolonged. On 6 March, there was no frost anywhere in the British Isles and the temperature in London reached 17 °C - the highest since 25 October 1962. The coldest winter over England and Wales since 1740, and the coldest over Scotland since 1879, had ended. With the thaw came flooding, but nothing like the scale of the 1947 floods. Soon after the winter of 1962/63, life returned to normal.

(using terminology in the latest version of the National Geography Curriculum)

Geographical enquiry and skills

• Use of maps at a range of scales
• Graphical techniques to present evidence on maps and diagrams

Knowledge and understanding of places

• Places and environments in the news

Breadth of study

• Human responses to hazards and extremes
• Weather and climate
• Spatial and temporal variations of weather