Airopaidia : $b Containing the narrative of a balloon excursion from Chester, the eighth of September, 1785, taken from minutes made during the voyage; hints on the improvement of balloons ... To which is subjoined, mensuration of heights by the barometer, made plain; with extensive tables. The whole serving as an introduction to aërial navigation.Baldwin, Thomas
History
Airopaidia : $b Containing the narrative of a balloon excursion from Chester, the eighth of September, 1785, taken from minutes made during the voyage; hints on the improvement of balloons ... To which is subjoined, mensuration of heights by the barometer, made plain; with extensive tables. The whole serving as an introduction to aërial navigation.
Baldwin, Thomas
Aeronautics -- Early works to 1900; Balloons -- Early works to 1800
The same Attraction which raises Water 10 Feet and a half, will raise
Air, whose Density is 800 Times less, to almost one third of that to
which the whole Pressure of the Atmosphere can raise Fluids:[94] Now it
has been before seen, that the Pressure of the Atmosphere raised the
Air 45 Miles: so that the Air is raised by the united Actions of the
Moon and Sun, at the New and Full Moon, to one-third Part of 45; i.e.
to 15 Miles. And for the same Reason, the Air is raised at the Moon’s
Quarters to 10 Miles:[95] the Difference between which is 5 Miles.
There is consequently a real _Tide of Air_ five Miles higher at
each New and Full Moon, than at her Quarters: which Tide rolls
with incredible Velocity along the Verge or highest Limit of the
Atmosphere; and is generally productive of Wind below.
292. The Elasticity of the Air must likewise be brought into the
Account, as contributing greatly to its Motion: the Spring of Air
always increasing as the Pressure encreases.
Considerable Changes must therefore ensue in the inferior Parts of the
Atmosphere.
For as the Effect of the Moon’s Attraction is to diminish the Weight of
the Atmosphere (tho’ its Quantity be increased) by elevating the Column
of Air in the Line of her Meridian; the Rarefaction of the Air is
therefore encreased, first _at the Top_ of the Atmosphere; afterwards
it gradually descends to the Bottom, or Surface of the Earth: so that
the incumbent Weight being diminished, the Air beneath will be greatly
_expanded_.
At whatever Height therefore any _Quantity of Vapour_ or superior
Cloud _rested_, while the Moon was in her Quarter; it woud _gradually
descend_ at the Approach of the next New or Full: at which Times it
woud remain suspended at a Height, where an Expansion took Place
equivalent to the former Expansion, at the Moon’s Quarter: and, if
the Height during the Moon’s Quarter was only equal to that of common
Clouds; such Vapour woud, at the New and Full Moon, _descend_ in Mist,
Rain, Snow, or Wind.
293. Little Reliance is to be placed, in these _Northern_ Climates, on
the aggregate Weight (_or elastic Power_) of the Air, indicated by the
Height of the Barometer, near the Times of the New and Full Moons:
tho’, in general, it will _descend_ about those Times.
[Sidenote: Proper Days for Ascent.]
These Things being so; it woud be improvident to undertake an aërial
Excursion, either three Days before, or three Days after the Day,
either of the New, or Full Moon: the Ascent shoud be forborne every
other Week; at least till the Art is a little more advanced.
Public-domain text, read in full here on John Shaqi.
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