Meteorology: The Science of the AtmosphereTalman, Charles Fitzhugh
Science
Meteorology: The Science of the Atmosphere
Talman, Charles Fitzhugh
Meteorology
Off the west coast of Africa, between the Canaries and the Cape Verde
Islands, haze due to dust blown up from the Sahara Desert is frequently
encountered by vessels, especially during the first four months of the
year. This haze probably gave rise to the ancient legend of a Sea of
Darkness--the _Mare Tenebrosum_--one of the mysterious terrors of the
ocean reported by the navigators who first sailed toward the New World.
Extensive deposits of atmospheric dust have attracted attention from
the earliest times. Ehrenberg, in 1849, collected records of 349 such
cases, and published a map showing their distribution, which embraces
the greater part of the world. Atmospheric dust is always brought down
in greater or less quantities by rain. When it consists of fine powdery
sand, the rain sometimes acquires a brownish or reddish tinge, staining
objects on which it falls and constituting the “showers of blood” that
have been regarded as prodigies from remote antiquity. Homer describes
such a shower, and many similar occurrences are recorded by the Roman
historians. Italy, owing to its proximity to the African coast, is
often visited by these showers, which still strike superstitious terror
into the hearts of the peasantry.
The millions of meteors that enter the earth’s atmosphere every day
contribute their quota of dust, though the total amount is small
compared with that of the material lifted from the earth. Fine
ferruginous particles are often seen on the snowy summits of high
mountains and the polar ice fields, and both their appearance and their
composition indicate that they are derived from meteors.
Forest fires, burning peat beds, and other conflagrations on a large
scale discharge quantities of dust into the atmosphere. Cinders from
the great Chicago fire spread over a large part of the globe. They are
said to have reached the Azores some forty days after the beginning
of the catastrophe. In Europe, the once common practice of burning
the moors to prepare them for cultivation gave rise to huge volumes
of smoke, which was carried by the wind hundreds and even thousands
of miles. The stronghold of this old custom--which still survives to
some extent--was East Friesland, in northwestern Germany, and the
characteristic haze to which it gave rise, known as “moor smoke”
(German, _Moorrauch_), was sometimes observed as far away as Spain,
Italy, and Greece.
Public-domain text, read in full here on John Shaqi.
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