Familiar Talks on Science: World-Building and Life; Earth, Air and Water.Gray, Elisha
Science
Familiar Talks on Science: World-Building and Life; Earth, Air and Water.
Gray, Elisha
Science
The earth in its diurnal revolutions travels at the rate of a little
more than 1000 miles an hour at the equator. But if we should travel
northward to within four miles, say, of the north pole, the surface
point would be moving at the rate of only about a mile an hour. At some
point equidistant between the north pole and the equator the surface of
the earth will be moving at a rate, say, of 500 miles an hour. If we
could fire a projectile from this point that would have a carrying power
to take it to the equator some time after the projectile was fired,
although it would fly in a perfectly direct line, it would appear to
anyone at the equator who observed its approach to be moving from a
northeasterly direction. The reason is that the earth is traveling twice
as fast at the equator as it is at the point whence the projectile is
fired. Therefore it will overshoot, so to speak, at the equator, and not
be dragged around by the increased motion we find there.
To make this still plainer, suppose the earth to be standing still and a
projectile be fired directly across from the north pole in the direction
of the lines of longitude and required one hour to reach the equator,
the projectile would appear to anyone standing at the equator to come
directly from the north. If, however, the earth is revolving at the rate
of 1000 miles an hour at the equator to the eastward, and the
projectile was fired from the pole, where there is practically no
motion, in the same direction along the longitudinal lines as before,
the observer would have to be in a position on the equator 1000 miles
west of this longitudinal line in order to see the projectile when it
arrived; therefore the apparent movement of the projectile would not be
along the line at the instant that it was fired, but along a line that
would cross the equator at a point 1000 miles west. When a southward
impulse is given to the air it follows, to some extent, the same law, so
that to one standing on the equator the northern trade wind will blow
from the northeast and the southern trade wind from the southeast.
Public-domain text, read in full here on John Shaqi.
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