Science in Short ChaptersWilliams, W. Mattieu (William Mattieu)
Science
Science in Short Chapters
Williams, W. Mattieu (William Mattieu)
Science
“The cold during the night ranged from a few degrees below to the
freezing point. As morning advanced the rushing of waters was heard,
and so little were the aeronauts aware of the course which they had
been pursuing during the night, that they supposed themselves to have
been thrown back upon the shores of the German Ocean, or about to enter
the Baltic, whereas they were actually over the Rhine, not far from
Coblentz.”
All this blind drifting for hours, during which the balloon may be
carried out to sea, and opportunities of safe descent may be lost, is
averted in an Arctic balloon voyage, which would be made in the summer,
when the sun never sets. There need be no break in the survey of the
ground passed over, no difficulty in pricking upon a chart the course
taken and the present position at any moment. With an horizon of 50 to
100 miles’ radius the approach of such a danger as drifting to the open
ocean would be perceived in ample time for descent, and as a glance
at the map will show, this danger cannot occur until reaching the
latitudes of inhabited regions.
The Arctic aeronauts will have another great advantage over those who
ascend from any part of England. They can freely avail themselves
of Mr. Green’s simple but most important practical invention—the
drag-rope. This is a long and rather heavy rope trailing on the ground.
It performs two important functions. First, it checks the progress of
the balloon, causing it to move less rapidly than the air in which it
is immersed. The aeronaut thus gets a slight breeze equivalent to the
difference between the velocity of the wind and that of the balloon’s
progress. He may use this as a fulcrum to effect a modicum of steerage.
The second and still more important use of the drag-rope is the very
great economy of ballast it achieves. Suppose the rope to be 1000 feet
long, its weight equal to 1 lb. for every ten feet, and the balloon
to have an ascending power of 50 lbs. It is evident that under these
conditions the balloon will retain a constant elevation of 500 feet
above the ground below it, and that 500 feet of rope will trail upon
the ground. Thus, if a mountain is reached no ballast need be thrown
away in order to clear the summit, as the balloon will always lift its
500 feet of rope, and thus always rise with the up-slope and descend
with the down-slope of hill and dale. The full use of this simple and
valuable adjunct to aerial traveling is prevented in such a country as
ours by the damage it might do below, and the temptation it affords to
mischievous idiots near whom it may pass.
In the course of many conversations with various people on this
subject I have been surprised at the number of educated men and women
who have anticipated with something like a shudder the terrible cold to
which the poor aeronauts will be exposed.
This popular delusion which pictures the Arctic regions as the abode of
perpetual freezing, is so prevalent and general, that some explanation
is demanded.
Public-domain text, read in full here on John Shaqi.
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