Meteorology; or, Weather ExplainedM'Pherson, J. G. (John Gordon)
Science
Meteorology; or, Weather Explained
M'Pherson, J. G. (John Gordon)
Meteorology
The process of decay in clouds takes place in various ways. A careful
observer may witness the gradual wasting away and dilution into thin air
of even great stretches of cloud, when circumstances are favourable. In
May 1896 my attention was particularly drawn to this at my manse in
Strathmore. In the middle of that exceptionally sultry month, I was
arrested by a remarkable transformation scene. It was the hottest May for
seventy-two years, and the driest for twenty-five years. The whole parched
earth was thirsting for rain. All the morning my eyes were turned to the
clouds in the hope that the much-desired shower should fall. Till ten
o'clock the sun was not seen, and there was no blue in the sky. Nor was
there any haze or fog.
But suddenly the sun shone through a thinner portion of the enveloping
clouds, and, to the north, the sky began to open. As if by some magic
spell there was, in a quarter of an hour, more blue to be seen than
clouds. At the same time, near the horizon, a haze was forming, gradually
becoming denser as time wore on. In an hour the whole clouds were gone,
and the glorious orb of day dispelled the moisture to its thin-air form.
This was a pointed and rapid illustration of the decay from cloud-form to
haze, and then to the pure vapoury sky. It was an instance of the
_reverse_ process. As the sun cleared through, the temperature in the
cloud-land rose and evaporation took place on the surface of the
cloud-particles, until by an untraceable, but still a gradual process
through fog, the haze was formed. Even then the heat was too great for a
definite haze, and the water-vapour returned to the air, leaving the
dust-particles in invisible suspension.
But clouds decay in another way. This I will illustrate in the next
chapter on "It always rains."
What strikes a close observer is the difference of structure in clouds
which are in the process of formation and those which are in the process
of decay. In the former the water-particles are much smaller and far more
numerous than in the latter. While the particles in clouds in decay are
large enough to be seen with the unaided eye, when they fall on a properly
lighted measuring table, they are so small in clouds in rapid formation
that the particles cannot be seen without the aid of a strong magnifying
glass.
Public-domain text, read in full here on John Shaqi.
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