Condensation On Exterior
Surfaces Of Glazing
With the increasing use of high performance glazing in homes, there have been a
number of inquiries regarding formation of condensation on the exterior surfaces
of windows.
Condensation will start forming on surfaces when the moisture content in the air
reaches the saturation point (100% relative humidity). When this occurs, the air
contains maximum amount of moisture that it can hold under the present
conditions. The amount of moisture air can hold depends mainly on the air
temperature. As the air temperature drops, the amount of moisture the air can
hold decreases. If the air is already close to 100% r. h., and the
temperature drops, the excess moisture will condense and form liquid water.
If the air is at 100% r. h. at a given temperature, and if it comes in contact
with surfaces of lower temperature, the air close to the surfaces will be cooled
further and condensation will occur. A common example of this is condensation
being present in the grass in the morning. Another example is spandrel panels on
buildings, having condensation early in the morning. This usually occurs during
the fall and spring on mornings when the r. h. is very high and the temperature
is moderate.
Under certain conditions the exterior surface temperatures may be several
degrees C lower than the ambient air temperature. This is the case when ground
frost forms during clear conditions even when the air temperature is + 2 to + 4
degrees C. The reason that the surfaces can reach temperatures lower than the
ambient air is the radiation heat loss to the sky. On clear nights, surfaces
such as windows, leaves and grass, will radiate energy to the sky. The sky acts
as a surface of very low temperature (may be – 10 to – 50 degrees C, depending
on conditions). Because of this radiation loss, the surface temperature will
drop well below the ambient air temperature if the relative humidity is already
at – or near 100%, condensation may form.
In this case of conventional low performing window glass, there is a relatively
high heat flow from the interior of the house to the exterior that will keep the
exterior glass surface temperature high enough to prevent condensation. With the
use of high performance glazing this heat flow is reduced and results in a lower
exterior glass surface temperature with much higher risk of condensation
forming. The better the insulating
value of the glazing, the lower the exterior glass surface temperature and the
higher the risk of condensation. Spandrel panels are better insulated than
window glazing (typically around R 15) and external condensation is relatively
common.
External condensation on high performance window glass can be a nuisance. It is,
however, quite normal and is an indication that the window has a high insulation
value. External condensation on window glass, with the use of more high
performing glazing, is becoming more common, but should not be a cause of
concern.
A second type of exterior condensation is quite common in tropical climates with
high humidity, particularly for monolithic glazing. When the interior is kept
cool with air-conditioning, the surface temperature of the exterior surfaces of
the glass will also be lowered. If the surface temperature is lowered
sufficiently by the air-conditioning to reach the dew-point, condensation will
form on the exterior surfaces of the glass. As mentioned, this is common with
monolithic glazing, but can also occur with sealed IG units if the humidity is
sufficiently high. The lower the u-value of the glazing, the lower the risk of
condensation. This type of condensation can occur during all hours of the day
and night. If the glazing is exposed to sunshine, the glass temperature will
increase and condensation will not normally occur.
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