Rarely
in the UK - or anywhere, for that matter - is a train
completely buried in snow. But that's exactly what
happened on Dartmoor in March 1891 and in northern
Scotland in January 1978. The winters that produced
such phenomenal snowstorms were not, however, generally
snowy - unlike the remarkable winter of 1947, the
snowiest since 1814.
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Fig 1: A car stuck
in snow at Hebden Bridge – 1963
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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.
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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. |
| Unrelenting
harsh weather |
The cold, snowy weather continued through February and into March. Any breaks
in the cold weather were short-lived.
- 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 per cent 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.
| More snow, flooding and then gales |
In some parts of the British Isles, snow fell on as many
as 26 days in February 1947. Much of the snow was powdery and was soon
whipped into deep drifts by strong winds.
If February hadn't been enough, March was even worse. In the first
half of the month, there were more gales and heavy snowstorms.
On 4 and 5 March, heavy snow fell over most of England and Wales, with
severe drifting. On 6 March, drifts were five metres deep in the Pennines
and three metres deep in the Chilterns. In some places, glazed frost
occurred. On 10 and 11 March, southern Scotland had its heaviest snowfall
of the winter, and the snowstorm reached the Scottish Highlands, where,
on 12 March, drifts more than seven metres deep were reported. |
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Fig 3: The
flooding of 1947
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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
meltwater couldn't soak into the ground. Surface run-off was the only option.
The warm air spread northwards and eastwards. Meltwater 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. Seventy per cent 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 coldest winter since 1740 |
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.
Ten 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 continuously under snow. 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.
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. |
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