Meteorology: The Science of the AtmosphereTalman, Charles Fitzhugh
Science
Meteorology: The Science of the Atmosphere
Talman, Charles Fitzhugh
Meteorology
The value of such publications has not been lessened by the gradual
substitution of steam for sails on ocean-going vessels. While wind is
no longer all-important, it is a factor in determining the speed, and
hence the earning capacity, of all classes of ocean shipping, and the
same is true of marine currents. Fog and drifting ice are, in general,
more serious obstacles to steamers than to sailing ships. A glance
at one of the Hydrographic Office Pilot Charts will suffice to show
that these publications are indispensable to the mariner. On these
charts we find, first of all, in the center of each five-degree square
of latitude and longitude a “wind rose” showing the frequency of the
winds that have been observed in that region from each of the cardinal
points, and their average force from each direction. On the charts
will also be found the routes recommended for full-power and low-power
steamers and sailing vessels, lines of magnetic variation, tracks of
storms in past years for the month in question, location and force of
currents, average limits and prevalence of fog for the month, recent
information about drifting ice and derelicts, descriptions of storm
signals, and an abundance of other information of vital importance to
the seaman.
[Illustration: OCEAN WEATHER MAP PREPARED FROM VESSEL REPORTS
JAN. 11, 1913, GREENWICH MEAN NOON
_U. S. Weather Bureau_
Solid black lines are isobars. Arrows fly with the wind, the center of
the arrowhead marking the position of the vessel, and the number of
feathers denoting the force of the wind on the Beaufort scale. Shading
of the head shows degree of cloudiness.]
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