ON THE REFRACTION OF THE AIR
We have shown how the movement which constitutes light spreads by
spherical waves in any homogeneous matter. And it is evident that when
the matter is not homogeneous, but of such a constitution that the
movement is communicated in it more rapidly toward one side than
toward another, these waves cannot be spherical: but that they must
acquire their figure according to the different distances over which
the successive movement passes in equal times.
It is thus that we shall in the first place explain the refractions
which occur in the air, which extends from here to the clouds and
beyond. The effects of which refractions are very remarkable; for by
them we often see objects which the rotundity of the Earth ought
otherwise to hide; such as Islands, and the tops of mountains when one
is at sea. Because also of them the Sun and the Moon appear as risen
before in fact they have, and appear to set later: so that at times
the Moon has been seen eclipsed while the Sun appeared still above the
horizon. And so also the heights of the Sun and of the Moon, and those
of all the Stars always appear a little greater than they are in
reality, because of these same refractions, as Astronomers know. But
there is one experiment which renders this refraction very evident;
which is that of fixing a telescope on some spot so that it views an
object, such as a steeple or a house, at a distance of half a league
or more. If then you look through it at different hours of the day,
leaving it always fixed in the same way, you will see that the same
spots of the object will not always appear at the middle of the
aperture of the telescope, but that generally in the morning and in
the evening, when there are more vapours near the Earth, these objects
seem to rise higher, so that the half or more of them will no longer
be visible; and so that they seem lower toward mid-day when these
vapours are dissipated.
Those who consider refraction to occur only in the surfaces which
separate transparent bodies of different nature, would find it
difficult to give a reason for all that I have just related; but
according to our Theory the thing is quite easy. It is known that the
air which surrounds us, besides the particles which are proper to it
and which float in the ethereal matter as has been explained, is full
also of particles of water which are raised by the action of heat; and
it has been ascertained further by some very definite experiments that
as one mounts up higher the density of air diminishes in proportion.
Now whether the particles of water and those of air take part, by
means of the particles of ethereal matter, in the movement which
constitutes light, but have a less prompt recoil than these, or
whether the encounter and hindrance which these particles of air and
water offer to the propagation of movement of the ethereal progress,
retard the progression, it follows that both kinds of particles flying
amidst the ethereal particles, must render the air, from a great
height down to the Earth, gradually less easy for the spreading of the
waves of light.
[Illustration]
Whence the configuration of the waves ought to become nearly such as
this figure represents: namely, if A is a light, or the visible point
of a steeple, the waves which start from it ought to spread more
widely upwards and less widely downwards, but in other directions more
or less as they approximate to these two extremes. This being so, it
necessarily follows that every line intersecting one of these waves at
right angles will pass above the point A, always excepting the one
line which is perpendicular to the horizon.
[Illustration]
Let BC be the wave which brings the light to the spectator who is at
B, and let BD be the straight line which intersects this wave at right
angles. Now because the ray or straight line by which we judge the
spot where the object appears to us is nothing else than the
perpendicular to the wave that reaches our eye, as will be understood
by what was said above, it is manifest that the point A will be
perceived as being in the line BD, and therefore higher than in fact it
is.
Similarly if the Earth be AB, and the top of the Atmosphere CD, which
probably is not a well defined spherical surface (since we know that
the air becomes rare in proportion as one ascends, for above there is
so much less of it to press down upon it), the waves of light from the
sun coming, for instance, in such a way that so long as they have not
reached the Atmosphere CD the straight line AE intersects them
perpendicularly, they ought, when they enter the Atmosphere, to
advance more quickly in elevated regions than in regions nearer to the
Earth. So that if CA is the wave which brings the light to the
spectator at A, its region C will be the furthest advanced; and the
straight line AF, which intersects this wave at right angles, and
which determines the apparent place of the Sun, will pass above the
real Sun, which will be seen along the line AE. And so it may occur
that when it ought not to be visible in the absence of vapours,
because the line AE encounters the rotundity of the Earth, it will be
perceived in the line AF by refraction. But this angle EAF is scarcely
ever more than half a degree because the attenuation of the vapours
alters the waves of light but little. Furthermore these refractions
are not altogether constant in all weathers, particularly at small
elevations of 2 or 3 degrees; which results from the different
quantity of aqueous vapours rising above the Earth.
And this same thing is the cause why at certain times a distant object
will be hidden behind another less distant one, and yet may at another
time be able to be seen, although the spot from which it is viewed is
always the same. But the reason for this effect will be still more
evident from what we are going to remark touching the curvature of
rays. It appears from the things explained above that the progression
or propagation of a small part of a wave of light is properly what one
calls a ray. Now these rays, instead of being straight as they are in
homogeneous media, ought to be curved in an atmosphere of unequal
penetrability. For they necessarily follow from the object to the eye
the line which intersects at right angles all the progressions of the
waves, as in the first figure the line AEB does, as will be shown
hereafter; and it is this line which determines what interposed bodies
would or would not hinder us from seeing the object. For although the
point of the steeple A appears raised to D, it would yet not appear to
the eye B if the tower H was between the two, because it crosses the
curve AEB. But the tower E, which is beneath this curve, does not
hinder the point A from being seen. Now according as the air near the
Earth exceeds in density that which is higher, the curvature of the
ray AEB becomes greater: so that at certain times it passes above the
summit E, which allows the point A to be perceived by the eye at B;
and at other times it is intercepted by the same tower E which hides A
from this same eye.
[Illustration]
But to demonstrate this curvature of the rays conformably to all our
preceding Theory, let us imagine that AB is a small portion of a wave
of light coming from the side C, which we may consider as a straight
line. Let us also suppose that it is perpendicular to the Horizon, the
portion B being nearer to the Earth than the portion A; and that
because the vapours are less hindering at A than at B, the particular
wave which comes from the point A spreads through a certain space AD
while the particular wave which starts from the point B spreads
through a shorter space BE; AD and BE being parallel to the Horizon.
Further, supposing the straight lines FG, HI, etc., to be drawn from
an infinitude of points in the straight line AB and to terminate on
the line DE (which is straight or may be considered as such), let the
different penetrabilities at the different heights in the air between
A and B be represented by all these lines; so that the particular
wave, originating from the point F, will spread across the space FG,
and that from the point H across the space HI, while that from the
point A spreads across the space AD.
Now if about the centres A, B, one describes the circles DK, EL, which
represent the spreading of the waves which originate from these two
points, and if one draws the straight line KL which touches these two
circles, it is easy to see that this same line will be the common
tangent to all the other circles drawn about the centres F, H, etc.;
and that all the points of contact will fall within that part of this
line which is comprised between the perpendiculars AK, BL. Then it
will be the line KL which will terminate the movement of the
particular waves originating from the points of the wave AB; and this
movement will be stronger between the points KL, than anywhere else at
the same instant, since an infinitude of circumferences concur to form
this straight line; and consequently KL will be the propagation of the
portion of wave AB, as has been said in explaining reflexion and
ordinary refraction. Now it appears that AK and BL dip down toward the
side where the air is less easy to penetrate: for AK being longer than
BL, and parallel to it, it follows that the lines AB and KL, being
prolonged, would meet at the side L. But the angle K is a right angle:
hence KAB is necessarily acute, and consequently less than DAB. If one
investigates in the same way the progression of the portion of the
wave KL, one will find that after a further time it has arrived at MN
in such a manner that the perpendiculars KM, LN, dip down even more
than do AK, BL. And this suffices to show that the ray will continue
along the curved line which intersects all the waves at right angles,
as has been said.