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
It assumes that moisture is evaporated and held in the atmosphere by
latent heat, which is given out during condensation, and actually warms
the surrounding atmosphere. Thus, the Kew Committee undertook to explain
the development of greater heat, at the elevation where they, in fact,
found the counter-trade. But how unphilosophical to suppose a portion of
the air or vapor contained in it, can give out to another adjoining
portion _more heat than is necessary to produce an equilibrium_. This can,
indeed, be done by experiment--_but the experiment is made with currents
of electricity_. How unphilosophical, too, to talk of latent heat in
connection with evaporation, _at the lowest temperature known_.
Meteorologists must revise their opinions on the subject of condensation.
This latent heat has never been actually met with; on the contrary, the
most sudden and complete condensations of the vapor of the atmosphere are
attended by as sudden and extraordinary productions of cold, and
consequent hail, and the connection between condensation and electricity
is shown by too many facts to permit the old theory to stand.
_Fog never forms with the thermometer below 32 deg.._ It is mainly a _summer
condensation_, especially high fog. It has been attributed to the cooling
effect of an atmosphere colder than the earth, but it often occurs when
the earth is the coldest, and when the vapor, as it rises, is colder than
the air, and could not give out heat to a warmer medium. (See American
Journal of Science, vol. xliv. p. 40.) Again, it is not mere condensation,
but a formation of globules or vesicles, hollow, and the air expanded in
them, by means of which they float like a soap bubble which contains the
warm air of the breath. Is not every vesicle a model shower, positively
electrified on the outside, negatively in the center, or the reverse,
according to the strata, with the air expanded in the middle by the excess
of heat which negative electricity detains? Look at them, as they attach
themselves to the slender nap of the cloth you wear, when passing through
them, and see how many of them it would require to form a large drop of
rain. The clouds are of a similar vesicular character, and rain does not
fall till the vesicles unite to form drops. Sudden and extreme cold is
indeed produced in the hail-storm, when, above, below, and around it, the
temperature is unaffected. Testu, Wise, and other aeronauts, have so found
it, and the hail tells us it is so. But it is idle to say it results from
radiation. All the phenomena of the sudden, violent hail-storms are
electric in an extraordinary degree. The electricity is disturbed and
separated--the associated heat continues with the negative, and leaves the
positive portion of the cloud, and a corresponding reduction of
temperature results. So Masson found in his eudiometrical analytical
experiments the _negative_ wire would heat to fusion, while the positive
was cold.
Public-domain text, read in full here on John Shaqi.
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