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1. Clouds
The classification of clouds is based upon that originated
by Luke Howard (1772-1864), a London pharmacist and amateur
meteorologist. In 1803 Howard, wrote a book entitled 'The
Modifications of Clouds' and named the various cloud structures
he had studied...
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Fact Sheet 1 (PDF, 1.3 Mb) |
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2. Thunderstorms
Most thunderstorms are associated with towering clouds
known as cumulonimbus. These clouds usually form on warm
sunny days or on a cold front if conditions are right
for their formation. Moist air near the ground rises as
it warms and if cooled sufficiently cumulus clouds form
at the condensation level...
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Fact Sheet 2 (PDF, 1.2 Mb) |
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3. Water in the atmosphere
When a jug full of iced drink is taken out of the refrigerator,
water droplets condense on the outside of the container.
This happens because the jug is at a lower temperature
than the dew point of the air. 'Dew point' is defined
as the temperature at which the air, when cooled, will
just become saturated...
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Fact Sheet 3 (PDF, 1.1 Mb) |
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4. Climate of the British Isles
The British Isles lie in the latitude of predominantly
westerly winds where depressions and fronts move bands
of cloud and rain eastwards or north-eastwards across
the North Atlantic. Between the depressions there are
often small mobile anticyclones bringing welcome fair
weather...
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Fact Sheet 4 (PDF, 1.5 Mb) |
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5. White Christmases
Snow at Christmas is deep-seated in British culture,
and many of us long for the likes of the scenes depicted
on traditional Christmas cards. The interest in snowy
Christmases has its origins in the colder climate of 1550-1850
when Britain was in the grip of the 'Little Ice Age'...
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Fact Sheet 5 (PDF, 146 kb) |
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6. The Beaufort Scale
It is often said that Francis Beaufort, of the British
Royal Navy, was the first to devise a scale of wind force
— towards the start of the 19th century. However,
in reality he was not, in fact, the originator of such
a scale. A similar one was actually in use at least a
century earlier — and probably long before that...
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Fact Sheet 6 (PDF, 1.0 Mb) |
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7. Climate of southwest England
The counties included in this area are Cornwall, Devon,
Somerset together with the Isles of Scilly. A brief description
of the landscape and topography is included here, followed
by statistics on temperature, sunshine, rainfall, snowfall
and wind...
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Fact Sheet 7 (PDF, 1.0 Mb) |
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8. The shipping forecast
The Met Office was established as the Meteorological
Department of the Board of Trade in 1854 when Captain,
later Vice Admiral, Robert FitzRoy became its first head.
FitzRoy introduced the first storm warning service for
shipping in 1861...
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Fact Sheet 8 (PDF, 867 Kb) |
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9. Weather extremes
We can all recall weather we have experienced which seemed
'extreme' or remarkable. In fact the Met Office and others
in the UK and elsewhere have been recording extremes of
temperature, sunshine, rainfall, snow, wind and atmospheric
pressure; a number of these are summarised here...
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Fact Sheet 9 (PDF, 347 kb) |
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10. Air masses and weather fronts
Air masses are parcels of air that bring distinctive
weather features, the air making up an air mass is very
uniform in temperature and humidity. Air masses are separated
by transition zones or boundaries that may be more sharply
defined; these are called fronts...
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Fact Sheet 10 (PDF, 853 kb) |
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11. Interpreting weather charts
On a weather chart, lines joining places with equal sea-level
pressures are called isobars. Charts showing isobars are
useful because they identify features such as anticyclones
(areas of high pressure), depressions (areas of low pressure),
troughs and ridges which are associated with particular
kinds of weather...
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Fact Sheet 11 (PDF, 1.1 Mb) |
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12. National Meteorological Archive
material
The Meteorological Office, then located at its Headquarters
at South Kensington, London, at a meeting of the Meteorological
Committee on 29 April 1914, accepted the responsibility
of custodian of appropriate Public Records...
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Fact Sheet 12 (PDF, 1.2 Mb) |
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13. Upper-air observations and the
tephigram
Knowledge of temperature, humidity and wind at levels
well above the ground form an essential part of the meteorologist's
basic data. The state of the upper air can be obtained
in many ways, but the main one is by observations from
balloon-borne equipment...
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Fact Sheet 13 (PDF, 700 kb) |
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14. Microclimates
A microclimate is the distinctive climate of a small-scale
area, such as a garden, park, valley or part of a city.
The weather variables in a microclimate, such as temperature,
rainfall, wind or humidity, may be subtly different to
the conditions prevailing over the area as a whole...
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Fact Sheet 14 (PDF, 504 kb) |
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15. Weather radar
The word radar is an acronym, from RAdio Detection And Ranging.
Although some primitive work on radio location had been carried
out in the United Kingdom as early as 1904, it wasn't until
the mid 1930s before any serious development work on radar
was instigated...
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Fact Sheet 15 (PDF, 827 Kb) |
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16. World climates
The climate of a locality is the synthesis of the day-to-day
values of the meteorological elements that affect the locality.
The main climatic elements are precipitation, temperature,
humidity, sunshine, wind velocity...
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Fact Sheet 16 (PDF, 1.1 Mb) |
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17. Weather observations
Meteorological observations are made for a variety of reasons.
The aim of all these observations are essentially to provide
data and are a valuable source of information, which is used
in a variety of different ways...
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Fact Sheet 17 (PDF, 1.85 Mb) |
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