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In 1643 Evangelista Torricelli whilst conducting experiments on
notes from the astronomer Galileo, led to the discovery, that by
using mercury he could create a vacuum in an inverted glass tube
and the level of the mercury would rise and fall with the day to
day changes in the atmospheric pressure. It was not until around
1675 that barometers came in to use domestically for weather prediction,
although they had been used experimentally since 1644. Torricellis
concept was developed by Robert Boyle taking it from the experimental
apparatus state into the usable domestic version. During this period
it had been used mainly for measuring height, as air pressure decreases
the higher you are. From this came the realisation that that local
climatic conditions and air pressure were somehow connected.
The stick Barometer was the first made as a scientific instrument;.
As the popularity of the barometer grew so did their decoration
and attractiveness and were considered prize pieces of furniture
as well as being useful. The early stick barometer was joined in
around 1663 by the wheel barometer devised by Hooke but it did not
gain popularity till around the 1700s. A problem with these
mercury barometers was that they were not easily portable and had
to be handled with extreme care to prevent the spillage of the mercury.
By 1843 Vidie had invented a barometer without mercury this was
called an aneroid mechanism and consisted of the vacuum chamber
being connected to the pointer by levers to enhance the movement.
This meant that they immediately became more portable and could
be used by scientists and engineers in the field for measuring heights
of hills and at sea.
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From around 1660's the plans for the wheel barometer devised
by Hooke
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