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)
[1] A tail will prevent any kite from turning over, or "diving,"
because its weight keeps the lower end down while the
pressure of the wind on the tail also pulls the lower end
backward and maintains the necessary angle of the kite to the
wind, the most efficient angle being about 22 degrees. Bending
back the ends of the cross-stick gives stability to a kite
because, when, on account of the eddies in the wind, a stronger
pressure is exerted on one side of the kite, this side is
driven backward, thereby presenting less effective surface to
the wind, while as the other side comes forward more nearly at
right angles to the wind, it receives greater pressure than
before. In this way the equilibrium about the central stick is
automatically maintained, the required inclination to the wind
being secured by the greater surface presented to the wind
below the point of attachment of the bridle.
In 1891 Mr. Eddy lifted a minimum thermometer by several of these
kites flown tandem, and proposed to obtain in this way data to
forecast the weather. In the _Proceedings of the Aeronautical
Conference_, held in connection with the Chicago Exposition, Prof. M.
W. Harrington, then Chief of the U. S. Weather Bureau, quoted Mr.
Eddy's estimate of the cost of exploring the air by means of kites
flown in series, and advocated their use.
Up to this time it does not appear that self-recording
instruments--that is to say, those which make continuous graphic
records--had been raised by kites. In the days of the early
experimenters such instruments were too heavy and cumbersome to be
lifted by the more or less unmanageable kites, but within the past few
years M. Richard of Paris has made the simple and light recording
instruments described in connection with balloons, which can be
attached to kites. In this way it is possible to obtain simultaneous
records at the kite and at a station on the ground, and from them to
study the differences of temperature and humidity, and this seems to
have been done first at Blue Hill Observatory. In August 1894 Mr. Eddy
brought his kites to Blue Hill and with them lifted a Richard
thermograph, which had been partly reconstructed of aluminium by Mr.
Fergusson so that it weighed but 1-1/4 lbs., to the height of 1500
feet, and so the earliest automatic record of temperature was obtained
by a kite. During the next summer, Mr. Eddy assisted again in the
experiments at Blue Hill, and secured photographs of the Observatory
and the hill by a camera carried between his kites to the height of a
hundred feet or more.
Public-domain text, read in full here on John Shaqi.
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