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LI-COR pyranometer
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The LI-COR
pyranometer (LI-200R) measures global solar radiation. It is a photodiode
covered by a plastic disk.
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Specifications
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Calibration: against an Eppley PSP
under natural daylight conditions, typical error is
±5%. |
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Sensitivity: 90 µA per 1000
W/m2. |
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Stability: < ±2% change
over a 1 year period. |
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Response Time: 10µs. |
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Temperature Dependence: 0.15%
per °C maximum. |
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Cosine Correction: corrected up to
an 80° angle of incidence. |
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Azimuth: < ±1% error
over 360° at 45° elevation. |
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Tilt: No error induced from
orientation |
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Operating Temperature: -40 to
65°C. |
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Relative Humidity: 0 to
100%. |
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Detector: high stability silicon
photovoltaic detector (blue enhanced). |
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Sensor Housing: weatherproof
anodized aluminum case with acrylic diffuser and stainless steel
hardware. |
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Spectral responsivity
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![LI-COR
pyranometer responsivity graph](Assets/GraphLICORPyranometerResponsivity.gif)
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While thermopile based pyranometers
such as an Eppley PSP have fairly uniform spectral response over the wavelength
of interest, solar cell based pyranometers, such as the LI-COR have a marked
spectral response to incident solar radiation. In the graph above, the LI-COR
shows maximum sensitivity to wavelength in the 900 µ wavelengths and does
not see an solar radiation with wavelengths over 1100 µ or under 400
µ.
A good study of the spectral responsivity
of the LI-COR pyranometer can be found in a paper by David L. King, William E.
Boyson, and Barry R. Hansen, "Improved Accuracy for Low-Cost Solar Irradiance
Sensors",
Sandia National Laboratories, Albuquerque, New Mexico, USA. Clear day responsivity was examined
in that paper; responsivity to the diffuse irradiance was studied in one of our papers:
Diffuse
Responsivity of Solar Cell Based Pyranometers.
Under cloudy conditions, the diffuse
responsivity of the LICOR pyranometer is approximately the same as found for the
total responsivity under clear skies. However, under clear sky conditions, the
diffuse responsivity is about 30% lower than that found in cloudy conditions.
The percentage of solar radiation detected by the solar cell base pyranometer varies
depending on whether the sky is blue (clear) or gray (cloudy). Since the diffuse
component only makes up about 10% of the total irradiance on a clear day, this
difference is hard to detect when the uncertainty in the calibration is on the order
of ±5%. Of course, this is a systematic error and can present problems
if the diffuse component is of importance.
On a daily basis, the total solar radiation
measurement of a LI-COR pyranometer is fairly close to that of an Eppley PSP.
However on an hourly or shorter time basis, this comparison varies systematically
over the day. It also changes depending on the cloud cover. Therefore, it is very
difficult to obtain a good calibration number for a LI-COR pyranometer with a
thermopile pyranometer.
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© 2022, UO Solar Radiation Monitoring
Laboratory.
Last
revised: March 15, 2022.
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