
OPERATION
35
4.1.3 Clear sky conditions
Clear sky conditions differ in the way that there is a relative large heat
loss caused by the atmospheric window. In this way the amount of re-
emitted radiation by a clear sky is smaller compared to the cloud
overcast sky condition. Because of the heat-lost in upward direction,
the sensors hot junctions will cool-down and show a relative large
negative net radiation value (from -90 to -130 W/m
2
). In this case the
calculated atmospheric long wave radiation (L
d
) shows a relative small
positive value. A clear sky condition is illustrated in figure 4.1B
Figure 4.1B Clear sky condition
4.1.4 Measurements during a sunny day
CG 4 allows accurate daytime measurements on sunny days without
the need for a moving shading device. Despite solar radiation up to
1000 W/m
2
the window heating will be less than 4 W/m
2
in the overall
calculated downward radiation.
Formula 1 can be applied without any problems with the following
exception: One must take note of the amount of Infrared radiation in
the solar spectrum. The amount of solar infrared radiation depends
Net radiation (from -90 to -130 W/m
)
Downwelling radiation
(Relative small value)
Atmosphere T
atm
Earth surface T
earth
>> T
atm
Upward radiation
Comments to this Manuals