Sounding the Ocean of Air: Being Six Lectures Delivered Before the Lowell Institute of Boston, in December 1898Rotch, Abbott Lawrence
Science
Sounding the Ocean of Air: Being Six Lectures Delivered Before the Lowell Institute of Boston, in December 1898
Rotch, Abbott Lawrence
Atmosphere; Balloons; Clouds; Kites (Meteorology)
However, the phenomena of atmospheric electricity, which have become
noticeable since the use of wire, may be described here. Generally,
whenever the kites rise above seventeen hundred feet, the wire becomes
strongly charged with electricity, and when the great heights are
reached the electricity is discharged in long and brilliant sparks at
the reel, often to the inconvenience of the attendants. Usually, the
electrical potential increases with altitude, and it is greatest
during snow-storms or when the conditions favour thunder-storms.
Notwithstanding its intensity, the quantity of electricity in the
atmosphere is probably insufficient to make its collection and
storage for practical purposes worth while.
It must not be imagined that kite-flying for meteorological purposes
is a sinecure. At Blue Hill about two hundred flights have been made
in all seasons and in all weathers, with temperatures varying from
-5∞ to +90∞, in gales, in rain, and in snow-storms, though not in
thunder-storms. Sometimes the kites are invisible from almost the time
they leave the earth until their return, but when the upper kites are
visible it is necessary to observe them with theodolites every few
minutes. Remembering that a high flight occupies ten or twelve hours,
and frequently terminates late at night, or even continues until
morning, it will be obvious that the work requires skill, energy, and
perseverance, which have been shown by my assistants at the Blue Hill
Observatory who have conducted the flights.
Occasionally, for lack of wind or from breakage of the line, the kites
fall to the ground, usually intact. If they were visible,
trigonometrical measurements on the hill enable the place of descent
to be located, and then the kites and meteorograph are sent for and
the wire is reeled up. But at night, or when clouds hide the kites,
the direction in which they fall is not known, because the azimuth of
the wire at the reel often differs from that of the kites; so last
autumn several hundred miles of road, path, wood, and swamp were
traversed before the aÎrial apparatus, which had been lost during a
flight at night, was found comparatively close at hand.
Public-domain text, read in full here on John Shaqi.
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