| Humidity
When
a lot of water vapor is in the air, we say the air is humid. Scientists
frequently use the term relative humidity, which describes how much
water vapor is in the air at a particular temperature compared with
how much water the air at that same temperature is able to hold.
An easy way to understand this is to imagine that the air is a towel.
If you spill a glass of water, you can wipe up the water with a
towel. But the towel probably could absorb more than just a glassful
of water. Perhaps it could hold water spilled from 5 or 10 glasses
before becoming completely soaked. The amount of water vapor actually
present in the air is often only a fraction of the total amount
that the air can hold, so relative humidity is expressed as a percentage.
When the relative humidity is 100 percent, the air is saturated.
Like a towel totally soaked with water, the air can hold no more
moisture. When the relative humidity is 100 percent and the air
is saturated, evaporation and precipitation are in a state of balance.
As moisture precipitates, the amount of evaporation increases to
reach a balanced state again.
Water vapor in the air is called humidity. Because molecules of
water vapor are so small they can't be seen, people who study humidity
have developed creative ways to measure the amount of vapor in the
air.
Probably the first person to think of an instrument to measure the
vapor content of the air was Leonardo da Vinci, a man who was born
in Italy in the 15th century. He placed a small wad of dry cotton
on one side of a balance scale. Then he placed an object of exactly
the same weight as the wad of cotton on the other side of the scale.
As the dry cotton absorbed water vapor from the air, it became heavier
and the balance pan lowered. The difference between the two weights
was the measure of the humidity.
Now scientists use an instrument called a psychrometer to measure
relative humidity. A psychrometer is made of two thermometers that
are fastened next to one another. The bulb of one thermometer is
wrapped in material that is soaked with purified water. To begin
measuring relative humidity, a person whirls the psychrometer around
until the thermometer with the wet material reaches a steady temperature,
which is always lower than the temperature on the dry bulb. The
actual air temperature is measured by the thermometer with the dry
bulb. The difference between the two temperatures is called the
wet-bulb depression and is the result of the evaporation of water
from the material. Scientists mark the dry-bulb temperature and
the wet-bulb depression on two charts, called Psychrometric Tables,
to calculate relative humidity and dew point temperature.
Scientists
also measure humidity with an instrument called a hair hygrometer.
Materials such as wood, cotton, skin, and hair absorb moisture from
the air. Human hair gets longer as it absorbs water, increasing
its length by about 21/2 percent over a relative humidity range
of 0 to 100 percent.
On a hair hygrometer, strands of hair are attached to a pointer
on a mechanical dial that has been specially marked to indicate
relative humidity. The pointer moves as the hair lengthens or shortens.
If a written record of relative humidity is needed, a hair hygrometer
can be connected to a hygrograph, which has a clock-driven pen that
marks a continuous line on graph paper.
The
amount of water vapor in the air determines how comfortable we feel
on a given day. One way the human body releases heat is by sweating.
Evaporation of sweat from our skin helps us cool down on hot days.
We feel cooler because during the evaporation process, water molecules
require energy to change into vapor. The kind of energy they use
is heat energy taken from the water molecules' environment, which
in this case is our skin. If the air already contains a lot of water
vapor, however, sweat does not evaporate quickly, and we continue
to feel hot and uncomfortable.
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