Meteorology: The Science of the AtmosphereTalman, Charles Fitzhugh
Science
Meteorology: The Science of the Atmosphere
Talman, Charles Fitzhugh
Meteorology
Meteorologists are still so much under the influence of the popular
idea of a “cyclone” that they hesitate to apply this term to a
disturbance of moderate force, except in a few special phrases (such
as “extra-tropical cyclone”), though the adjective “cyclonic” is
used freely without reference to the force of the wind. British
meteorologists speak mostly of “depressions,” while American
meteorologists speak of “lows.” The status of the latter term, as well
as that of the term “high,” is, however, paradoxical. Though both
words have been used for years, they are nearly always printed with
quotation marks around them, as if they had not yet been assimilated in
the vocabulary. The Weather Bureau has lately taken to printing these
words in capital letters. Neither of these practices will be followed
in the present book.
[Illustration: PHOTO BY PROF. ELLERMAN SHOWING CLOUDS OR FOG CASCADING
THROUGH LAST FORK CAÑON AND INTO THE SANTA ANITA CAÑON. (_Letter from
F. A. Carpenter, May 29, 1919._)]
Tropical cyclones are called “hurricanes” in the West Indies and the
South Pacific, “typhoons” off the east coast of Asia, “baguios” in
the Philippines, and “cyclones” in the Indian seas. They form in the
doldrums, and generally take a long, sweeping course, curving westward
and poleward, and sometimes passing into the temperate zones, where
they either die out or increase in size, diminish in violence, and
become similar to the storms originating in the higher latitudes. One
of the curious features they often exhibit within the tropics is the
calm center at the “eye of the storm,” to which Tennyson alludes when
he writes of the blast (unknown to meteorologists) that drove a ship
Across the whirlwind’s heart of peace,
And to and thro’ the counter-gale.
These cyclones are the worst of all storms found at sea, and also
exercise their destructive effects over islands and along continental
coasts. The greatest disasters attending them have been due to the
inundation of low-lying shores by the huge waves they generate, as
in the Galveston hurricanes of 1900 and 1915 and in the far worse
catastrophes that have occasionally visited the coast of India.
Hurricanes of the West Indies occur chiefly from August to October,
inclusive. The number varies from none to a dozen a year (with four as
an average).
[Illustration: Copyright, Ewing Galloway
A CLOUDBURST NEAR CEDAR BRAKES, UTAH
A snapshot taken from the edge of the cañon.]
Public-domain text, read in full here on John Shaqi.
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