Meteorology: The Science of the AtmosphereTalman, Charles Fitzhugh
Science
Meteorology: The Science of the Atmosphere
Talman, Charles Fitzhugh
Meteorology
There is, however, a particular reason why rain is rather more likely
to occur soon after a battle than shortly before one; viz., the fact
that intervals of fair weather, with consequent dry roads, are used
by commanders in carrying out the movement of troops that precede an
engagement. By the time such arrangements, often occupying several
days, are completed, the “spell” of fine weather is likely to be over,
and a rainstorm is due in accordance with the normal program of nature.
The most famous undertaking in the history of rain-making--and one
which has had an incalculable effect in fostering the credulity of the
public with respect to similar enterprises--was that carried out by
General Robert Dyrenforth on behalf of the United States Government
in 1891. Congress voted appropriations amounting to $9,000 for these
experiments, and Dyrenforth was appointed a “special agent” of the
Department of Agriculture to direct them. After some preliminary trials
in the suburbs of Washington, the experimenters proceeded to a ranch
near Midland, Texas. Here a few balloons filled with a mixture of
oxygen and hydrogen, as well as several sticks of dynamite carried
up by kites, were exploded in the air, but the only explosions of
considerable magnitude were set off on the ground. The experiments
continued over a period of three weeks and in some cases showers fell
within a few hours after an explosion, but, in spite of the somewhat
favorable tone of the official report, the consensus of scientific
opinion was that the undertaking was a failure, while the views of
the public at large were divided. The attitude of the Government is
sufficiently indicated by the fact that it has never since undertaken
experiments in this line. The one tangible outcome of this affair was
that a crop of private rain-makers sprang up all over the country, and
to this day the example set by the official experimenters is cited
in support of every sort of harebrained scheme for juggling with the
weather.
In 1911 and 1912 the late C. W. Post, of breakfast-food fame, expended
many thousand pounds of dynamite in efforts to produce rain in Texas
and Michigan. Showers undoubtedly occurred in conjunction with Post’s
experiments, but conditions favoring their occurrence were plainly
indicated on the current daily weather maps, and they had been duly
forecast by the Weather Bureau.
The professional rain-maker does not generally resort to the expensive
process of bombarding the clouds. His methods most frequently involve
the use of chemicals, and the details are shrouded in mystery. For
example, about a quarter of a century ago one Frank Melbourne, known as
“the Australian rain-maker,” enjoyed great celebrity and coined money
by his exploits in this field. His plan was to shut himself up in a
barn, freight car, or other structure, and manipulate his chemicals
and electric batteries for hours or days. Naturally rain sometimes came
after these operations, but as often it did not.
Public-domain text, read in full here on John Shaqi.
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