Practical Exercises in Elementary MeteorologyWard, Robert DeCourcy
Science
Practical Exercises in Elementary Meteorology
Ward, Robert DeCourcy
Meteorology
This process of evaporation needs energy to carry it on, and this energy
often comes from the heat of some neighboring body. When you fan yourself
on a very hot day in summer, the evaporation of the moisture on your face
takes away some of the heat from the skin, and you feel cooler. The drier
the air on a hot day, the greater is the evaporation from all moist
bodies, and hence the greater the amount of cooling of the surfaces of
those bodies. For this reason a hot day in summer, when the air is
comparatively dry, that is, not saturated with moisture, is cooler, other
things being equal, than a hot day when the air is very moist. Over
deserts the air is often so hot and dry that evaporation from the face and
hands is very great, and the skin is burned and blistered. Over the
oceans, near the equator, the air is hot and excessively damp, so that
there is hardly any cooling of the body by evaporation, and the conditions
are very uncomfortable. This region is known as the “Doldrums.”
The temperatures that are felt at the surface of the skin, especially
where the skin is exposed, as on the face and hands, have been named
_sensible temperatures_. Our sense of comfort in hot weather depends on
the _sensible_ temperatures. These sensible temperatures are not the same
as the readings of the ordinary (dry-bulb) thermometer, because our
sensation of heat or cold depends very largely on the amount of
evaporation from the surface of the body, and the temperature of
evaporation is obtained by means of the wet-bulb thermometer. Wet-bulb
readings at the various stations of the Weather Bureau are entered on
all our daily weather maps. In summer (July) the sensible (wet-bulb)
temperatures are 20° below the ordinary air temperature in the dry
southwestern portion of the United States (Nevada, Arizona, Utah). The
mean July sensible temperatures there are from 50° to 65°; while on the
Atlantic coast, from Boston to South Carolina, they are between 65° and
75°. Hence over the latter district the temperatures actually experienced
in July average higher than in the former.
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