The Philosophy of the Weather. And a Guide to Its ChangesButler, T. B. (Thomas Belden)
Science
The Philosophy of the Weather. And a Guide to Its Changes
Butler, T. B. (Thomas Belden)
Weather; Weather forecasting
But Colonel Reid's descriptions are unmeaning and unintelligible. G.
M.--Gloomy, misty! Gloomy from what? fog, or stratus, or a stratum of
scud, or what? We can not know. Again, C. The table tells us this stands
for detached clouds. But of what kind? Cumulus, broken stratus, patches of
cirro-cumulus or cirro-stratus, or scud? All these, and indeed every kind
of cloud or fog formation, except low fog, may exist in detached portions.
These abbreviations will not answer; they do not describe the weather. The
clouds must be studied and described. There is no difficulty in doing it.
Sailors will learn them very soon after their teachers have; and those who
teach them should see to it that the logs contain terms of description
which convey the meaning which may, and ought to be, conveyed. The use of
these indefinite terms can not be continued without culpability.
Again, the observations of seamen off our coast are in accordance with the
progress of this class of storms on land, and prove that they continue S.
E. over the Atlantic, abating in action as they approach the tropics.
There is abundant evidence of this in the work of Colonel Reid, and the
charts of Lieutenant Maury, but I can not devote further space to them.
The third class form in the counter-trade, over some portion of the
country, from excessive volume or action of the counter-trade, or local
magnetic activity, without coming from the tropics or being connected with
a regular polar wave of magnetic disturbance.
The following diagram exhibits their form, progress, and accompanying
induced winds.
[Illustration: Fig. 22.]
The gentle rains of spring, particularly April, and the moderate and
frequent snow-storms of winter, are often of this character; and so are
the heavy rains, which commence at the morning barometric minimum, rain
heavily through the forenoon, and light up near mid-day in the south,
followed by gentle, warm, S. W. winds. This class are more frequent in
some years than others--probably the early years of the decade, while
polar storms are, during the later ones. It is this class which have
_violent_ easterly winds _in front_, and on the _south side_, with two or
more currents, and which Mr. Redfield has also supposed to be cyclones.
Public-domain text, read in full here on John Shaqi.
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