Meteorology: The Science of the AtmosphereTalman, Charles Fitzhugh
Science
Meteorology: The Science of the Atmosphere
Talman, Charles Fitzhugh
Meteorology
Excessive dryness of the skin, which is a common cause of discomfort,
is not very closely related to the humidity of the air. “In winter,”
says Hill, “if there be a wind the rate of evaporation is so
accelerated that the skin feels dry, because in order to check the
loss of body heat the sweat glands are inactive and the blood vessels
of the chilled skin are constricted.” There has been a great deal of
discussion about the dry air of American buildings in winter, and
startling figures have been adduced to show that the air of such
buildings is dryer than that of deserts. So far as measurements of
relative humidity go, this is perfectly true; but, as Dr. G. T.
Palmer, of the New York State Commission on Ventilation, has pointed
out, there is an important difference between dryness and “dryingness.”
The latter depends upon the movement of the air, as well as the
relative humidity. The circulation of the air in a desert is generally
much more active than that of the air in a building with the windows
shut, and therefore much more conducive to rapid evaporation. There are
systems of ventilation in which the air is kept in steady and rapid
motion, and it is probably only in such cases that the air of our
heated houses can be compared to that of a desert. From the European
point of view American buildings are notoriously overheated, but this
is probably due to the fact that our hot summers--much hotter than
those of Europe--have adapted us to a tropical climate.
It is natural to inquire whether the atmospheric conditions that
affect the comfort of man do not also exercise a marked influence
upon his muscular efficiency and his mental powers. This question has
been answered in the affirmative by a number of ingenious writers,
who have sought to establish definite quantitative relations between
certain states of the atmosphere and the output of work in factories,
the grades attained by school children, etc. Thus, Dr. Ellsworth
Huntington, a well-known worker in this field, declares that the most
favorable daily mean temperature for mental activity (the temperature
being measured out-of-doors) is about 40 degrees F., and for physical
activity about 60 degrees F. Contrary to the common opinion, he holds
that our general efficiency is at low ebb in midwinter and fairly high
in summer. Variability in temperature, within certain limits, he finds
to be stimulating; equable temperature the reverse. He has drawn
charts showing the distribution of what he calls “climatic energy”--i.
e., the combination of certain weather factors supposed to control
human efficiency--throughout the world, and other charts showing a
more or less similar distribution of “civilization.” He has also made
an ambitious attempt to interpret the history of mankind in terms of
weather and climate.
Public-domain text, read in full here on John Shaqi.
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