Climate and Weather in Great Britain (Климат и погода в Великобритании)
Climate and Weather in Great Britain
Weather is not the same as climate. The weather at a place is the
state of the atmosphere there at a given time or over a short period. The
weather of the British Isles is greatly variable.
The climate of a place or region, on the other hand, represents the
average weather conditions over a long period of time.
The climate of any place results from the interaction of a number of
determining factors, of which the most important are latitude, distance
from the sea, relief and the direction of the prevailing winds.
The geographical position of the British Isles within latitudes 50o to
60o N is a basic factor in determining the main characteristics of the
climate. Temperature, the most important climatic element, depends not
only on the angle at which the sun’s rays strike the earth’s surface, but
also on the duration of daylight. The length of day at London ranges from
16 hours 35 minutes on June to 7 hours 50 minutes on 21 December. British
latitudes form the temperate nature of the British climate, for the sun is
never directly overhead as in the tropical areas.
Britain’s climate is dominated by the influence of the sea. It is much
milder than that in any other country in the same latitudes. This is due
partly to the presence of the North Atlantic Drift, or the Gulf Stream, and
partly to the fact that north-west Europe lies in a predominantly westerly
wind-belt. This means that marine influences warm the land in winter and
cool in summer. This moderating effect of the sea is in fact, the cause of
the relatively small seasonal contrasts experienced in Britain.
The moderating effect of the ocean on air temperature is also stronger
in winter than in summer. When the surface water is cooler than the air
above it – as frequently happens during the summer months – the air
tends to lose its heat to the water. The lowest layers of air are chilled
and become denser by contradiction, and the chilled air tends to remain at
low levels. The surface water expands because it is warmed, and remains on
the surface of the ocean. Unless the air is turbulent, little of it can be
cooled, for little heat is exchanged.
Opposite conditions apply in winter. The air in winter is likely to be
cooler than the surface water, so that the heat passes from water to air.
Air at low levels is warmed and expands and rises, carrying oceanic heat
with it, while the chilled surface water contracts and sinks, to be
replaced by unchilled water from below. This convectional overturning both
of water and of air leads to a vigorous exchange of heat.
The prevailing winds in the British Isles are westerlies. They are
extremely moist, as a result of their long passage over warm waters of the
North Atlantic. On their arrival to Britain, the winds are forced upwards,
and as a result large-scale condensation takes place, clouds form and
precipitation follows, especially over the mountainous areas.
North and north-west winds often bring heavy falls of snow to north
Britain during late October and November, but they are usually short-lived.
Continental winds from the east sometimes reach the British Isles in summer
as a warm, dry air-stream, but they are more frequently experienced in
winter when they cross the north sea and bring cold, continental-type
weather to eastern and inland districts of Great Britain.
Relief is the most important factor controlling the distribution of
temperature and precipitation within Britain. The actual temperatures
experienced in the hilly and mountainous parts are considerably lower than
those in the lowlands. The effect of relief on precipitation is even more
striking. Average annual rainfall in Britain is about 1,100 mm. But the
geographical distribution of rainfall is largely determined by topography.
The mountainous areas of the west and north have more rainfall than the
lowlands of the south and east. The western Scottish Highlands, the Lake
District (the Cumbrian mountains), Welsh uplands and parts of Devon and
Cornwall in the south-west receive more than 2,000 mm of rainfall each
In contrast, the eastern lowlands, lying in a rain-shadow area, are
much drier and usually receive little precipitation. Much of eastern and
south-eastern England (including London) receive less than 700 mm each
year, and snow falls on only 15 to 18 days on the average.
Rainfall is fairly well distributed throughout the year, although
March to June are the driest months and October to January are the wettest.
Ireland is in the rather a different category, for here the rain-
bearing winds have not been deprived of their moisture, and much of the
Irish plain receives up to 1,200 mm of rainfall per year, usually in the
form of steady and prolonged drizzle. Snow, on the other hand, is rare,
owing to the warming effects of the Gulf Stream. The combined influences of
the sea and prevailing winds are equally evident in the general pattern of
rainfall over the country.
Because of the North Atlantic Drift and predominantly maritime air
masses that reach the British Isles from the west, the range in temperature
throughout the year is never very great. The annual mean temperature in
England and Wales is about 10oC , in Scotland and Northern Ireland about
9oC. July and August are the warmest months of the year, and January and
February the coldest.
The mean winter temperature in the north is 3OC,the mean summer
temperature 12oC. The corresponding figures for the south are 5oC and 16oC.
The mean January temperature for London is 4oC, and the mean July
During a normal summer the temperature may occasionally rise above
30oC in the south. Minimum temperatures of –10oC may occur on a still clear
winter’s night in inland areas.
The distribution of sunshine shows a general decrease from south to
north – the south has much longer periods of sunshine than the north.
It is frequently said that Great Britain does not experience climate,
but only weather. This statement suggests that there is such a day-to-day
variation in temperature, rainfall, wind direction, wind speed and sunshine
that the “average weather conditions”, there is usually no very great
variation from year to year or between corresponding seasons of different
No place in Britain is more than 120 km from the sea. But although the
British are crowded very closely in a very small country, there is one
respect in which they are very fortunate. This is their climate. Perhaps,
this is a surprising statement because almost everyone has heard how
annoying the weather usually is in England. Because of the frequent clouds
and the moisture that hangs in the air even on fairly clear days, England
has less sunshine than most countries, and the sunlight is weaker then in
other places where the air is dry and clear. What is worse, sunshine rarely
lasts long enough for a person to have time to enjoy it. The weather
changes constantly. No ordinary person can guess from one day to another
which season he will find himself in when he wakes in the morning.
Moreover, a day in January may be as warm as a warm day in July and a day
in July may be as cold as the coldest in January.
The most remarkable feature of English weather, the London fog, has as
exaggerated reputation. What makes fog thick in big industrial areas is not
so much the moisture in the air as the soot from millions of coal fires.
Such smogs (smoke + fog) are not frequent today. Since 1965 as a result of
changes in fuel usage and the introduction of clean air legislation, they
have become less severe. It is quite natural that in fine, still weather
there is occasionally haze in summer and mist and fog in winter.
The amount of rainfall in Britain is exaggerated, too. Britain seems
to have a great deal of rain because there are so many showers. But usually
very little rain falls at a time. Often the rain is hardly more than
floating mist in which you can hardly get wet. Although a period of as long
as three weeks without rain is exceptional in Britain.
It is no wonder that, living in such an unbearable climate with so
many rules and with still more exceptions, the Englishmen talk about their
weather, whatever it may be, and their climate, too.
1.Baranovski L.S., Kozikis D.D.. How Do You Do, Britain? – Moscow