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)
Until quite recently Glaisher's results were accepted as representing
the conditions of the free air up to the greatest height which it was
possible to reach. These results showed that the temperature did not
fall uniformly with height, but that it fell most rapidly near the
earth and much less rapidly at great heights. In cloudy weather up to
the height of a mile the mean decrease of temperature in the day-time
differed little from the theory of 1∞ per 300 feet, but in clear or
partly clear weather the decrease was more rapid, commencing with 1∞
for 160 feet near the ground and diminishing to 1∞ for 1000 feet at an
elevation exceeding six miles. The observations in the captive balloon
up to a third of a mile indicated a daily range in the vertical
decrease of temperature. The observations of relative humidity agreed
with Welsh's in showing a slight increase up to about half-a-mile,
then a decrease up to above five miles, where there seemed to be an
almost entire absence of water. The other observations were
inconclusive, except that the time of vibration of a magnet was found
to be somewhat longer than on the earth, which was contrary to
Gay-Lussac's experience. The most remarkable of Glaisher's ascents was
made from Wolverhampton on September 5, 1862, when in less than one
hour he had passed the altitude of five miles, exceeding the greatest
height hitherto reached. To quote from Glaisher's narrative: "Up to
this time I had taken observations with comfort and experienced no
difficulty in breathing, whilst Mr. Coxwell, in consequence of the
exertion he had to make, had breathed with difficulty for some time.
Having discharged sand, we ascended still higher; the aspirator became
troublesome to work, and I also found a difficulty in seeing
clearly.... About 1 hour 52 min., or later, I read the dry-bulb
thermometer as minus 5∞; after this I could not see the column of
mercury in the wet-bulb thermometer, nor the hands of the watch, nor
the fine divisions of any instrument. I asked Mr. Coxwell to help me
to read the instruments. In consequence, however, of the rotatory
motion of the balloon, which had continued without ceasing since
leaving the earth, the valve-line had become entangled, and he had to
leave the car and mount into the ring to readjust it. I then looked at
the barometer, and found its reading to be 9-3/4 inches, still
decreasing fast, and implying a height exceeding 29,000 feet. Shortly
after, I laid my arm upon the table, possessed of its full vigour, but
on being desirous of using it, I found it powerless.... Trying to move
the other arm, I found it powerless also. Then I tried to shake myself
and succeeded, but I seemed to have no limbs.... I dimly saw Mr.
Coxwell, and endeavoured to speak, but could not. In an instant
intense darkness overcame me, so that the optic nerve lost power
suddenly, but I was still conscious, with as active a brain as at the
present moment whilst writing this. I thought I had been seized with
Public-domain text, read in full here on John Shaqi.
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