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
Nor can it otherways be accounted for, why the Snow is perpetual,
and the Cold so intense, on Mountains under the Equinoctial, and
between the Tropics: but which admits an easy Solution on the above
Hypothesis.[67]
CHAPTER XXXXVI.
Section 254. The Subject of +depressing torrents+ requires an accurate
Investigation: as it will serve to point out the proper Time of Day or
Night, when an Aironaut ought so to calculate his Voyage, as to arrive
over the Middle of the Channel, or Arm of the Sea, at some particular
Hour: in order to wait for a Sea Breeze which may waft him to the other
Side.
A Point not difficult to be ascertained.
Also, this Idea of +depression+, if properly considered and digested;
may prove a sufficient Foundation on which to establish a new Theory
of the _Weather_, so ill determined at present, from its _aggregate
Weight_ or _Elasticity_ only, as indicated by the Barometer.
255. If a Conjecture may be formed on a Subject, material in itself,
yet of which so little is actually known; woud not _the proper Time_ of
undertaking a Voyage over the Channel be such, that the Aironaut shoud
find himself three Parts of the Way across, by +nine+ _o’Clock_ in the
Morning?
256. In _warmer_ Climates, where the Seasons are more regular; the
_Land-Breeze_ blows to Sea from Midnight till X. in the Morning: at
which Time, the _Sea-Breeze_ blows to Land; continues till V. or VI. in
the Evening; and is succeeded by a +calm+, which lasts till Midnight.
Whence it follows, that during the Time of the Sea-Breeze, there is
a constant Tendency towards a +gulph of air+, _along the Middle_ of
the Channel: the Equilibrium of which is as constantly supplied by a
_Depression_ of the upper and in general cooler Strata of Air; and
therefore a _dangerous_ Time for the Passage of Balloons.
On the contrary, during the Night, and till ten in the Morning, there
is an _Accumulation_ of Air, _along the Middle of the Channel_: which
consequently is a proper Time to ensure a _safe_ Passage; by the
Assistance of +wings+, or some +propulsive+ Machinery.
[Sidenote: Of the horizontally calm mediocèanal depressing Current.]
257. The Deficiency or Vacuity being supplied from the etherial
Regions; it might be taken for granted, that such Ether must be
_considerably_ lighter than the adjacent common Air on an equal Level,
and therefore _proportionably_ dangerous for the Passage of Balloons.
Public-domain text, read in full here on John Shaqi.
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