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)
soon became invisible, or, when seen, was confounded with the stars.
Before and after the flight the meteorograph is hung upon a tripod in
the free air, in order that its thermometer and hygrometer may be
compared with the standards.
HEIGHTS ABOVE SEA-LEVEL OF KITE-FLIGHTS.
(_Blue Hill is 630 feet above the sea_)
----+----+----------------++-------------------------------------------
| No.|Heights in Feet || Percentages of Records above
Year| of +-------+--------++-------+--------+--------+--------+--------
|Rec-|Mean of|Absolute|| 500 m.| 1000 m.| 1500 m.| 2000 m.| 3000 m.
|ords|Maximum|Maximum || (1640 | (3280 | (4920 | (6560 | (9840
| | | || ft.) | ft.) | ft.) | ft.) | ft.)
----+----+-------+--------++-------+--------+--------+--------+--------
1894| 2 | 1,860 | 2,070 || 50 | 0 | 0 | 0 | 0
1895| 28 | 1,673 | 2,490 || 59 | 0 | 0 | 0 | 0
1896| 86 | 2,772 | 9,327 || 78 | 28 | 9 | 4 | 0
1897| 38 | 4,557 | 11,716 || 95 | 68 | 45 | 21 | 5
1898| 35 | 7,350 | 12,070 || 100 | 92 | 80 | 66 | 20
----+----+-------+--------++-------+--------+--------+--------+--------
Since the use of wire and more efficient kites, the heights have been
greatly increased. Thus the average height above the hill attained by
the meteorograph in thirty-five flights made during 1898 was more than
a mile and a quarter, whereas the average height of all the ascents
prior to 1897 was about a quarter of a mile (see Table). The average
height of the meteorograph above the hill, in all the flights during
August 1898, was nearly a mile and a half, and on August 26 the
meteorograph was raised 360 feet higher than ever before, its
altitude, determined trigonometrically, being 11,440 feet above Blue
Hill, or 12,070 feet above the neighbouring ocean. The meteorograph
was suspended from the topmost kite, one of the Lamson pattern, having
71 square feet of lifting surface, and this was increased to a total
of 149 square feet by four kites of the modified Hargrave type, that
were attached at intervals to the wire. The five miles of wire in the
air weighed 75 lbs., and the total weight including kites and
apparatus was 112 lbs. The meteorograph left the ground at 10:40 a.m.,
attained its greatest height at 4:15 p.m., and returned to the ground
at 8:40 p.m., a feat which it would be difficult for a man to equal on
a mountain. The cumulus clouds were traversed three-quarters of a mile
from the earth, and above them the air was found to be very dry. On
the hill the air temperature was 72∞, when it was 38∞ in the free air
11,440 feet above, and the wind velocity increased from twenty-two to
forty miles an hour. These figures give an idea of the change of
atmospheric conditions which occurs, but the conclusions deduced from
the Blue Hill kite-flights will be discussed in the next chapter.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account