Meteorology: The Science of the AtmosphereTalman, Charles Fitzhugh
Science
Meteorology: The Science of the Atmosphere
Talman, Charles Fitzhugh
Meteorology
In order to connect the readings of this device with human sensations,
Hill and his collaborators have used the instrument under a great
variety of atmospheric conditions, both indoors and out, and compared
the readings with independent estimates of comfort and discomfort. On
an ideal summer day the “wet kata” fell from 110 to 100 in 25 seconds,
and the “dry kata” in 85 seconds. Indoors at the seaside in summer,
under comfortable conditions, the readings were 50 seconds and 140
seconds, respectively. A large number of other readings, taken under
different conditions in various parts of the word, have been published.
The katathermometer is now used in both Great Britain and the United
States in the study of ventilation problems, and has acquired a rather
extensive literature. According to its inventor, “the heating and
ventilation of rooms should be arranged so that the wet-bulb falls from
100 to 90 degrees in about one minute, and the dry-bulb in about three
minutes.”
[Illustration: A WEATHER BUREAU KIOSK, IN UNION SQUARE, SAN FRANCISCO.
(_Photograph, U. S. Weather Bureau._)]
[Illustration: THE UNITED STATES WEATHER BUREAU STATION, OBSERVATORY
TYPE, AT PEORIA, ILLINOIS. (_Photograph, U. S. Weather Bureau._)]
Regardless of the merits of these particular instruments, it is
certain that the cooling power of the air--which is quite a different
thing from the temperature of the air--is a very important factor in
determining our comfort and our health. Within certain limits the body
can easily adjust itself to changes in the cooling power of the air;
within wider limits the adjustment is effected with difficulty, and we
experience discomfort and possibly suffer in health; and finally
there are extreme conditions, in either direction, to which adjustment
is not possible; the internal temperature is then either lowered or
raised, as the case may be, and a comparatively small change of this
sort is fatal; i. e., death results by chilling or by heat stroke.
[Illustration:
Photo U. S. Weather Bureau
THE CENTRAL OFFICE OF THE UNITED STATES WEATHER BUREAU IN WASHINGTON]
Public-domain text, read in full here on John Shaqi.
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