Sounding the Ocean of Air: Being Six Lectures Delivered Before the Lowell Institute of Boston, in December 1898 — John Shaqi
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)
It was arranged to record the observations
on ruled paper with a silver pen, because the doctor would not trust a
common pen or pencil as liable to accident. He also had a map of
England to determine the direction which the balloon took. Jeffries'
English sentiments are shown by this quotation from his narrative: "I
had provided a handsome British flag, invidiously represented the next
day in one of the public papers to have been the flag of the American
States." The barometer and thermometer were observed every few
minutes, and the hygrometer occasionally. The electrometer did not
change its indications. Samples of air were obtained and sent to the
Royal Society, but it does not appear that they were ever analyzed.
The balloon rose nearly two miles, and descended safely in Kent after
an hour and a half. Jeffries' observations compare favourably with
those made until recently; indeed, for nearly a century there was
little improvement in the apparatus. The decrease of temperature which
Jeffries found, viz. 1∞ for 360 feet rise, and the decreasing humidity
with height agree very well with later observations.
Jeffries and Blanchard undertook a more perilous voyage on January 7,
1785, from Dover across the Channel, landing in the province of
Artois, after, so runs the announcement, "we were suspended and
floating in the atmosphere two hours over the sea and forty-seven
minutes over the land of France." The voyagers were cordially
welcomed, and were entertained lavishly in Paris as being, Jeffries
says, "the first who passed across the sea from England into France by
the route of the air." No instruments but a barometer and a compass
were carried, and the only scientific result worthy of notice was that
the balloon seemed to lose buoyancy over the sea, due to what Jeffries
thought might be "the power of attraction over the water." The height
of the balloon was measured trigonometrically by French officers in
Calais, who found by angular measures, when the balloon was midway
across the Channel, that its height was 4500 feet. Jeffries' voyages
have been described somewhat at length because the first scientific
balloon voyage is generally attributed to the Belgian physicist,
Robertson, who ascended from Hamburg in 1803 to the improbable height
of 24,000 feet. Robertson made his third ascent the next year from St.
Petersburg, accompanied by the Academician Sacharoff. This was a
scientific voyage, instituted at the request of the Russian Academy,
to ascertain the physical state of the atmosphere and the component
parts of it at different heights, also the difference between the
results of vertical ascents and the observations of Deluc, De
Saussure, von Humboldt and others on mountains, which it was rightly
concluded could not be so free from terrestrial influences as those
made in the open air. Among the experiments which the Academy proposed
were the following: change of rate of evaporation of fluids, decrease
Public-domain text, read in full here on John Shaqi.
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