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
Now it is universally agreed, that the Sea, is sooner heated by the Sun
than the Land: and on Account of the marine Acid exhaled,[70] is also
less cold,[71] during that Season, in the same Latitude.
In Spring, therefore, the great Atlantic or Western Ocean, being
_less_ cold than England, Holland, and Eastwards; the Air pendent over
the most extensive Tract of _dry and cool Land_ in the World, rushes
Westwards to supply the Equilibrium of _warm light_ Air rising upwards,
and causing a temporary mediocèanal Accumulation: which (altho’ the
specific Gravity of the cold Air is greater) must produce an actual
Deficiency in the aggregate Weight of the Atmosphere over England and
Holland: consequently the Barometer falls.
Again: the West Winds which blow at other Seasons; if, in Winter;
are not frequent, except about Noon after frosty Nights which have
equalized the Air for the Transmission of vigorous Sunshine: and shoud
be looked upon as (what they are really observed to be) _low_ partial
Sea-Breezes, or +eddy+ _Currents_, insinuating themselves near the
Surface, and setting Eastwards frequently against the upper and more
general Winds; and therefore produce a temporary Accumulation.
If, in Summer; the Supply of cool Air to the heated Land, being
made not only from the _Northern Ocean_, and lofty _Mediterrànean
Mountains_; but also from the _Atlantic Breezes_; the latter, tho’
_moist and temperate_, must also tend towards an Accumulation of the
Atmosphere over England and Holland: and therefore the Barometer rises.
CHAPTER XXXXVIII.
[Sidenote: Facts and Observations tending to confirm the Doctrine of
Accumulation and depression.]
Section 260. Before the Subject of mediocèanal Accumulation and
Depression of Air, is wholly quitted; it may be well mention and
compare a few Facts and Observations, which will elucidate the
Doctrine; and in their Turn, receive Light from it.
261. If, in the Middle of a _hot sunny_ Day, Vapours lighter than the
Air, were to rise from the Ocean, (which they will continue to do, in
hollow Vesicles or Bladders, till the Expansion breaks the Bubble, at
which Time the Water woud fall to the Earth, if not drank up by the
Attraction of _dry_ Spunges of Air;) there woud be a constant Wind
blowing from _Land to Sea_, to fill up the Chasm: but at such Time, the
Land is more heated than the Sea: therefore hot Air and Vapour arise
from both; and the Breeze, on the contrary, blows from _Sea to Land_;
consequently if the Vacuities were not _continually_ supplied from the
etherial Regions, and from the Ocean, all Animals woud actually die,
for Want of Air, as in a _hot close_ Room.
Such Supply is therefore constantly made, by Depression of the
Atmosphere, and Absorption of the Water.
Public-domain text, read in full here on John Shaqi.
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