Dew point is that unique temperature to
which the air (or any gas) must be cooled in order that
it shall be saturated with respect to water.
Frost Point (FP)
Frost point is that unique temperature
to which the air (or any gas) must be cooled in order
that it shall be saturated with respect to ice.
The dew point or frost point DEFINES
the partial pressure of the water vapor in the gas, from
the Smithsonian Meteorological Tables.
Relative Humidity (RH)
Relative Humidity (RH) is the ratio of the
actual vapor pressure in the mixture to the saturation
vapor pressure, with respect to water, at the prevailing
dry bulb temperature.
NOTE: RH is arbitrarily defined with
respect to water even though it seems that it should be
with respect to ice at -40&186;C (-40&186;F).
Dalton's Law (Pm)
John Dalton was the first to surmise that
the total pressure (PM) exerted by a mixture of gases
or vapors is the sum of the pressures of each gas if it
were to occupy the same volume individually. The pressure
which each gas component of a multiple constituent gas
(such as air) exerts is called its partial pressure. If
Px, Py, and Pz represent the respective partial pressure
of gases X, Y, and Z in a mixture, Dalton's Law states:
PM = Px + Py + Pz + ...
Elementary as it may seem, the concept
of Dalton's Law is often overlooked when considering problems
in humidity, because one forgets that the "water vapor"
in a gas is actually a gas itself and must therefore be
treated in accordance with the gas laws. Air must be considered
a mixture of gases: oxygen, nitrogen, and water vapor
(neglecting the minor constituents). All discussions of
humidity can then be reduced to discussions of water vapor
pressure, and all definitions encountered in humidity
can be expressed in terms of vapor pressure.