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Webster 1913 Edition


Barometer

Ba-rom′e-ter

,
Noun.
[Gr.
βάροσ
weight +
-meter
: cf. F.
baromètre
.]
An instrument for determining the weight or pressure of the atmosphere, and hence for judging of the probable changes of weather, or for ascertaining the height of any ascent.
☞ The barometer was invented by Torricelli at Florence about 1643. It is made in its simplest form by filling a graduated glass tube about 34 inches long with mercury and inverting it in a cup containing mercury. The column of mercury in the tube descends until balanced by the weight of the atmosphere, and its rise or fall under varying conditions is a measure of the change in the atmospheric pressure. At the sea level its ordinary height is about 30 inches (760 millimeters). See
Sympiesometer
.
Nichol.
Aneroid barometer
.
See
Aneroid barometer
, under
Aneroid
.
–
Marine barometer
,
a barometer with tube contracted at bottom to prevent rapid oscillations of the mercury, and suspended in gimbals from an arm or support on shipboard.
–
Mountain barometer
,
a portable mercurial barometer with tripod support, and long scale, for measuring heights.
–
Siphon barometer
,
a barometer having a tube bent like a hook with the longer leg closed at the top. The height of the mercury in the longer leg shows the pressure of the atmosphere.
–
Wheel barometer
,
a barometer with recurved tube, and a float, from which a cord passes over a pulley and moves an index.