Meteorology: The Science of the AtmosphereTalman, Charles Fitzhugh
Science
Meteorology: The Science of the Atmosphere
Talman, Charles Fitzhugh
Meteorology
People who never travel far from their own homes usually cherish quite
erroneous ideas regarding the climates of distant lands. It is hard for
most Americans to realize, for example, that the Isthmus of Panama,
in the heart of the tropics, never experiences temperatures nearly so
high as those which occur every summer in the United States. A citizen
of South Dakota, where the mercury, in the shade, frequently rises
above 100° Fahr., and has been known to reach 115°, will be inclined
to revise his definition of the term “tropical” when he learns that
at Colon, the Atlantic terminus of the Canal, a temperature as high
as 90° is decidedly exceptional, and that the maximum reading during
a period of six years was only 92°. In thirteen years Canal Zone
vital statistics showed only two deaths from sunstroke and twenty-one
non-fatal cases of heat prostration among a population of 120,000. It
will also surprise most Americans to learn that the highest natural
air temperatures that have been recorded anywhere on earth were not
observed near the equator, but in a California desert. At a place on
the edge of Death Valley, rejoicing in the ironical name of Greenland
Ranch, a temperature of 134° Fahr. was registered in July, 1913. The
thermometer which furnished this remarkable reading was a tested
instrument, installed in a standard screen over an alfalfa sod, and
not exposed to the reflected heat of the desert. At the same place the
temperature reached 100° or more on 548 days in four years. Outside
of the United States the highest temperature ever recorded at a
meteorological station was 127° Fahr. at Wargla (Ouargla), Algeria.
The lowest temperatures encountered by polar explorers are considerably
higher than those experienced each winter by the inhabitants of
northern Siberia. The “record,” so far as instrumental observations go,
is held by the town of Verkhoyansk, at which the temperature fell to
90° below zero (Fahrenheit) in February, 1892. Strange to say, this
“winter cold pole” of the earth has warm summers. At Verkhoyansk the
temperature sometimes rises to 80° above zero, or higher. At Yakutsk,
Siberia, the thermometer has been known to fall to 84° below zero in
winter and to rise 102° above zero in summer; a range of temperature
exceeding the interval between the freezing point and the boiling point
of water!
Another climatic paradox is that experienced by mountaineers who, in
scaling peaks mantled in eternal snow, often suffer with the heat,
on account of the intensity of solar radiation in the pure, dry air
of high altitudes. At the health resort of Davos, in the high Alps
(altitude 5,250 feet), invalids sit out-of-doors without wraps in
midwinter, and, indeed, are sometimes driven into the shade to escape
the too ardent rays of the sun. At the same time the temperature of the
air itself may be far below freezing, and the ground covered with snow.
Public-domain text, read in full here on John Shaqi.
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