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)
The reorganization of balloon observations was accomplished by the
German Society for the Promotion of AÎrial Navigation, which has been
assisted by the Prussian Meteorological Institute, and by officers of
the German Army Balloon Corps. The German Emperor takes a personal
interest in the work, and has aided it by the gift of a considerable
sum of money. The first voyage under the direction of the Society was
made in 1888, and many notable ones followed. In 1891, through the
courtesy of the president, Dr. Assmann, the writer made an ascent
from Berlin in a balloon equipped for accurate observations, with the
special purpose of comparing the sling with the aspiration
thermometer. The car of the balloon is shown in Fig. 3. A companion
was the now famous Dr. Berson, who then made his second ascent, but
who has now become an expert aeronaut by reason of more than fifty
ascensions, some of them to great heights. On December 4, 1894, he
ascended alone from Stassfurt, Prussia, in the _Phoenix_, to
probably the greatest height ever reached by man, at least in a
conscious state. By breathing oxygen he was able to keep his senses
and to read the barometer at 9∑1 inches, indicating approximately an
altitude of 30,000 feet, and the aspirated thermometer at 54∞ below
zero. An ordinary thermometer read 11∞ below zero in the sun, showing
its heat was much diminished in consequence of the haze that prevailed
even at this enormous height. The cirriform clouds which surrounded
the balloon were found to have the structure of snow-flakes rather
than that of ice-crystals. The chief result of this record-breaking
ascent was the extraordinarily low temperatures recorded at great
heights, as compared with those observed by Glaisher, Tissandier, and
others. An inversion of temperature--that is an increase of
temperature with height--prevailed up to a mile, but above that the
temperature fell at a rapid and accelerated rate which approached the
adiabatic fall above 26,000 feet. The wind, which was almost calm at
the earth's surface, increased to a gale in the high atmosphere, and
carried the balloon along at an average speed of thirty-six miles an
hour. Wishing to demonstrate conclusively whether the insular position
of England influenced the temperature of the high atmosphere, as had
been suggested, Dr. Berson determined to execute a high ascension in
England during the prevalence of a barometric maximum in summer, when
the air column would be abnormally warmed and the upper isothermal
surfaces elevated. An opportunity was afforded Berson to follow in
Glaisher's footsteps on September 14, 1898, when abnormal heat
prevailed in Europe. Berson, with the aeronaut Spencer, in the balloon
_Excelsior_, rose from the Crystal Palace in London to the height of
27,300 feet, where he observed a temperature of -29∞. The oxygen
inhaled prevented harmful physiological effects except for the
discomfort caused by the enormous reduction of temperature from 80∞ at
Public-domain text, read in full here on John Shaqi.
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