Practical Exercises in Elementary MeteorologyWard, Robert DeCourcy
Science
Practical Exercises in Elementary Meteorology
Ward, Robert DeCourcy
Meteorology
The =ordinary thermometer= (Greek: _heat measure_), the most commonly used
and most widely known of all meteorological instruments, was in an
elementary form known to Galileo, and was used by him in his lectures at
the University of Padua during the years 1592 to 1609. Thermometers enable
us to measure the temperatures of different bodies by comparison with
certain universally accepted standards of temperature. These standards are
the freezing and boiling points of distilled water. In its common form the
thermometer consists of a glass tube, closed at the top, and expanding at
its lower end into a hollow spherical or cylindrical glass bulb. This bulb
and part of the tube are filled with mercury or alcohol. As the
temperature rises, the liquid expands, flows out of the bulb, and rises in
the tube. As the temperature falls, the mercury or alcohol contracts, and
therefore stands at a lower level in the tube. In order that the amount of
this rise or fall may be accurately known, some definite scale for
measurement must be adopted. The scale commonly used in this country owes
its name to Fahrenheit (born in Danzig in 1686; died in 1736), who was the
first to settle upon the use of mercury as the liquid in thermometers, and
also the first definitely to adopt two fixed points in graduating the
scale. The division of this scale into 180° between the freezing point
(32°) and the boiling point (212°) seems to have been taken from the
graduation of a semicircle. Fahrenheit was a manufacturer of all sorts of
physical apparatus, and it has been thought probable that he had some
special facilities for dividing his thermometer tubes into 180 parts.
Mercury is most commonly used as the liquid in thermometers, because it
readily indicates changes of temperature, and because over most of the
world the winter cold is not sufficient to freeze it. The freezing point
of mercury is about 40° below zero (-40° F.). Alcohol, which has a much
lower freezing point, is therefore used in thermometers which are to be
employed in very cold regions. Alcohol thermometers must, for instance, be
used in Northern Siberia, where the mean January temperature is 60° below
zero.
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