
User Manual
9
5. Using the CNR4 in the Four Separate Components
Mode
In the four separate components mode configuration (measuring two short-wave
radiation signals, two long-wave signals), all signals are measured separately.
Calculation of net-radiation and albedo can be done on-line by the datalogger, or
off-line by the user during post-processing, using the stored raw data.
The two pyranometers will measure the short-wave radiation, both incoming and
reflected. The two pyrgeometers will measure the long-wave radiation. For
proper analysis of the pyrgeometer measurement results, they must be temperature
corrected using the temperature measurement performed by the onboard
thermistor or Pt-100 sensor.
The following paragraphs describe how one should treat the instrument, and how
different parameters like net short-wave radiation, net long-wave radiation, soil
temperature, sky temperature, and net (total) radiation can be calculated.
5.1 Measuring Short-wave Solar Radiation with Pyranometer
The pyranometer generates an mV signal that is simply proportional to the
incoming short-wave radiation. The conversion factor between voltage, V, and
W/m2of solar irradiance E, is the so-called calibration constant C (or sensitivity).
For each pyranometer
E = V/C (5-1)
Measuring with a pyranometer can be done by connecting two pyranometer wires
to a datalogger. Incidental light results in a positive signal. The pyranometer
mounting plate and ambient air should be at the same temperature, as much as
possible. Conversion of the voltage to irradiance can be done according to
equation 5-1, and this is done inside the datalogger program.
With the upward-facing pyranometer the so-called global (solar) downwelling
radiation is measured. The downward-facing pyranometer measures the reflected
upwelling solar radiation. When calculating the net radiation, the upwelling
radiation must be subtracted from the downwelling radiation. See Section 5.5.
5.2 Measuring Long-wave Far Infrared Radiation with
Pyrgeometer
When using the pyrgeometer, you should realize that the signal that is generated
by the pyrgeometer represents the exchange of long-wave far infrared (thermal)
radiation between the pyrgeometer and the object that it is facing. This implies
that the pyrgeometer will generate a positive voltage output, V, when it faces an
object that is hotter than its own sensor housing, and that it will give a negative
voltage signal when it faces an object that is colder. This means that for
estimating the far infrared radiation that is generated by the object that is faced by
the pyrgeometer, usually the sky or the soil, you will have to take the pyrgeometer
temperature, T, into account. This is why the temperature sensors are
incorporated in the CNR4's body near the pyrgeometer sensing element, and has,
therefore, the same temperature as the pyrgeometer sensor surface. The
calculation of the long-wave far infrared irradiance, E, is done according to the
following equation: