Physical science in the time of Nero : $b being a translation of the Quaestiones naturales of SenecaSeneca, Lucius Annaeus
Philosophy
Physical science in the time of Nero : $b being a translation of the Quaestiones naturales of Seneca
Seneca, Lucius Annaeus
Comets; Earthquakes; Meteorology -- Early works to 1800
There are some species of winds which issue from clouds that are rent 1
and pour down their contents. They are called by the Greeks cloud winds
(ἐκνεφίας). Their method of formation, as I suppose, is this: among the
particles given off by the earth’s vapour and carried aloft there is
great inequality and dissimilarity, some being dry and others moist.
When the particles have massed in one body there is great discord and
internal strife, which probably leads to the forming of certain hollow
clouds with narrow pipe-shaped spaces left between, much like a flute
in shape. In these gaps there is shut up rarefied air, which, being 2
buffeted about in the confined space and becoming heated, strives to
get more room. It expands and rends its envelope, breaking forth in
wind, which, as a rule, is squally, since it descends from above and
falls on us with fierce vehemence. It is not diffused, nor does it
come through a wide open space, but it struggles and opens up its way
by main force. As a rule, it is a brief gust. As it bursts through 3
the cloudy receptacle by which it was confined and overleaps the
battlements, it comes in tumultuous energy, sometimes not unattended
with fire and the sound of thunder in the heavens. Such winds are much
more violent and of longer duration if they have taken up in their
course other gusts proceeding from a like cause, and thus several
have conspired to form one. It is just like the flow of torrents of
moderate size, not serious as long as each has its separate course. But
when a number of them have combined their streams, they surpass in 4
size regular, constant rivers. The same thing may probably happen in
squalls; they are short-lived whenever they are alone. But when they
have joined forces, and the air expelled from several parts of the sky
at once has all combined in one, both force and duration are added to
them.
XIII
So, then, wind results from the breaking up of a cloud, which breach 1
is effected in several different ways. The accumulation of air is
burst sometimes by the internal struggle, as it seeks to gain an exit;
sometimes by the heat produced either simply by the sun or else by the
mutual ramming and friction of the roaming bodies.
Public-domain text, read in full here on John Shaqi.
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