the Air; and since I have found, by several Experiments
made on places comparatively not very high, and have
yet found the pressure sustain’d by those parts
of the Air at the top and bottom, and also their differing
Expansions very considerable: Insomuch that I
have found the pressure of the
Atmosphere lighter
at the top of St.
Paul’s Steeple in
London
(which is about two hundred foot high) then at the
bottom by a sixtieth or fiftieth part, and the expansion
at the top greater then that at the bottom by neer
about so much also; for the
Mercurial Cylinder
at the bottom was about 39. inches, and at the top
half an inch lower; the Air also included in the Weather-glass,
that at the bottom fill’d only 155. spaces, at
the top fill’d 158. though the heat at the top
and bottom was found exactly the same with a scal’d
Thermometer: I think it very rational to
suppose, that the greatest Curvature of the Rays is
made nearest the Earth, and that the inflection of
the Rays, above 3. or 4. miles upwards, is very inconsiderable,
and therefore that by this means such calculations
of the height of Mountains, as are made from the distance
they are visible in the Horizon, from the supposal
that that Ray is a straight Line (that from the top
of the Mountain is, as ’twere, a Tangent to the
Horizon whence it is seen) which really is a
Curve,
is very erroneous. Whence, I suppose, proceeds
the reason of the exceedingly differing Opinions and
Assertions of several Authors, about the height of
several very high Hills.
8. Whether this Inflection of the Air will not
very much alter the supposed distances of the Planets,
which seem to have a very great dependence upon the
Hypothetical refraction or inflection of the Air, and
that refraction upon the hypothetical height and density
of the Air: For since (as I hope) I have here
shewn the Air to be quite otherwise then has been hitherto
suppos’d, by manifesting it to be, both of a
vast, at least an uncertain, height, and of an unconstant
and irregular density; It must necessarily follow,
that its inflection must be varied accordingly:
And therefore we may hence learn, upon what sure grounds
all the Astronomers hitherto have built, who have
calculated the distance of the Planets from their
Horizontal Parallax; for since the Refraction
and Parallax are so nearly ally’d, that
the one cannot be known without the other, especially
by any wayes that have been yet attempted, how uncertain
must the Parallax be, when the Refraction is
unknown? And how easie is it for Astronomers
to assign what distance they please to the Planets,
and defend them, when they have such a curious subterfuge
as that of Refraction, wherein a very little variation
will allow them liberty enough to place the Celestial
Bodies at what distance they please.