Reading the WeatherLongstreth, T. Morris (Thomas Morris)
Science
Reading the Weather
Longstreth, T. Morris (Thomas Morris)
Weather forecasting
The hunter had to rely on local weather signs. The commuter can go him one
better by investing $10 (how finance will creep in!) in a little aneroid
barometer. The local weather signs were good for twelve hours at the
longest. The barometer is a faithful instrument that adds another twelve
hours to a man's knowledge. Half a day, or even a day before any local
sign of changing wind or growing cloud appears the barometer is on the
job. It will register in Philadelphia the news of a disturbance
approaching the Mississippi. So sensitive is it that it is the slave to
every wave of the great air ocean.
The barometer gauges for the eye the amount of atmosphere that is piled
above one. If the amount is normal and at sea-level the instrument will
measure 30.00 inches. This air pressure is equivalent to a column of water
30 feet high. As this would make unwieldy prognosticators the scientists
use mercury instead, which requires a column less than three feet long.
And for general purposes this is supplanted by the handy little aneroid
(which means "without fluid"). This is so fixed that the pressure of the
air influences the upper surface of a vacuum chamber, balanced perfectly
between this pressure and a main spring. This action is transmitted to an
index hand moving across the dial marked into fractions of inches after
the manner of the recognized standard, the mercurial barometer.
When the warm moist light air of a cyclone invades a locality the pressure
is partially removed, the vacuum chamber is not pressed so hard and the
dial hand or the mercury subsides. When the cold, dry, heavy air of the
anticyclone lumbers in more pressure is applied and the mercury, or the
dial hand, climbs. So a falling barometer means a storm, a rising one fair
weather.
That is a generality that glitters. If that were all there was to it
weather officials would have a sinecure. But each cyclone varies in size,
intensity, and rate of progress. Some do not advance for days. Therefore
there has grown up a pretty large body of information as each storm has
had to be watched and the barometric movements recorded. The most
important variations follow:
Remembering that 30.00 inches is sea-level normal, if the barometer is
steady at 30.10 or 30.20 the weather will remain fair as long as the
steadiness continues, and on the turn, if the fall proceeds slowly with
the wind from a westerly direction fair to partly cloudy weather with
slowly rising temperature will follow for two days.
If the barometer rises rapidly from 30.10 the fall will be equally rapid
and rain or snow may be expected within a couple of days. Since the
depressions of the atmosphere tend to a certain regularity about the
center of the storm it follows that the reactions will follow the actions
in similar manner,--a long rise portending a long fall and a variable
glass meaning unsettled conditions.
Public-domain text, read in full here on John Shaqi.
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