Meteorology: The Science of the AtmosphereTalman, Charles Fitzhugh
Science
Meteorology: The Science of the Atmosphere
Talman, Charles Fitzhugh
Meteorology
Most of the material used in the preparation of the charts above
described is obtained from a great corps of volunteer marine observers,
who enter their observations at stated hours in forms provided for
the purpose and send these records to the establishment in charge
of the work at the end of each voyage. The forms furnished by the
United States Weather Bureau prescribe only one regular observation
a day, to be taken at Greenwich mean noon. Each observation shows
the position of the ship, the direction of the wind, the force of
the wind on the Beaufort scale, the height of the barometer, the
readings of the dry-bulb and wet-bulb thermometers, the temperature
of the water at the surface, the state of the weather, and the kind,
amount, and movement of clouds. In order to check the accuracy of the
barometric readings, the observer is instructed to read his barometer
at prescribed hours on three successive days when in port and send the
readings to the Weather Bureau. On receipt of these readings the Bureau
compares them with those of the nearest meteorological station, and
then mails the observer a “barometer tag,” showing the results of the
comparison and the error of his instrument. Besides keeping up these
routine observations, the observer keeps a record of fog encountered
at any hour of the day and makes detailed reports on storms. Many
marine observers also report observations at stated hours by wireless
telegraphy.
The enormous fund of information thus collected over the ocean is
applied to several purposes besides the construction of Pilot Charts.
Our Weather Bureau and certain foreign meteorological institutions
prepare daily charts, showing approximately the instantaneous
conditions over great oceanic areas, especially the North Atlantic.
These maps are analogous to the daily weather maps published for land
areas, but the drawing of each map is, necessarily, delayed for
several months after the date to which it refers, in order to allow
time for the receipt of as many reports as possible from ships at sea.
As a rule such charts are prepared in manuscript only, but, though they
cannot be distributed after the manner of ordinary weather maps, they
are valuable for studies in the institution itself on the movements
of storms and other atmospheric processes. They also enable the
meteorological officials to answer inquiries concerning the winds and
weather that have prevailed over a particular part of the ocean on any
specified date. Such inquiries come from vessel owners, underwriters,
and others, and the replies are frequently used as evidence in
admiralty suits.
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