Irradiance measurement procedure

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SUMMARY

The discussion focuses on the procedure for measuring solar irradiance using filters and the implications of filter effects on spectral data. The proposed method involves calibrating the measurement system by capturing reference spectra both with and without a filter, allowing for a transformation of the data to estimate the sun's spectrum without the filter. Key equations are presented to illustrate the relationship between irradiance measurements, highlighting potential issues with low filter transmittance and the limitations of coarse-grained spectrometers, which complicate the division step into a deconvolution process.

PREREQUISITES
  • Understanding of irradiance measurement concepts
  • Familiarity with spectral analysis techniques
  • Knowledge of filter transmittance characteristics
  • Experience with deconvolution methods in signal processing
NEXT STEPS
  • Research the principles of filter transmittance and its impact on spectral measurements
  • Learn about deconvolution techniques for spectral data analysis
  • Explore calibration methods for spectrometers, particularly in high-intensity environments
  • Investigate the design and application of saturable absorbers in optical measurements
USEFUL FOR

Researchers and technicians involved in optical measurement, particularly those working with solar irradiance and spectral analysis, will benefit from this discussion.

elegysix
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Here's what I'm thinking. The sun is too bright to measure directly with our equipment. If I calibrate without a filter, and capture the reference spectrum with and without the filter, then I can model how the filter changes the spectrum. This way I can capture the sun spectrum with the filter, and transform the data as if I had not used it.

What I mean to say is, if
I_{r}(\lambda)=Y(\lambda)
and
I_{r+f}(\lambda)=G(\lambda)Y(\lambda)
then is it valid to argue that
I_{s}(\lambda)=\frac{I_{s+f}(\lambda)}{G(\lambda)}

Or is it that G(\lambda) is dependent on I?

where
I_{r} is the irradiance of the reference
I_{r+f} is the irradiance of the reference measured through a filter
I_{s} is the irradiance of the sample
I_{s+f} is the irradiance of the sample measured through the same filter
 
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As a first approximation, that approach is fine. The main shortcomings with this approach are 1) if G(λ) << 1 (the filter transmits very little light at some wavelengths) and/or 2) if your detector is a coarse-grained spectrometer (say a color camera). Problem (1) introduces error by amplifying noise, and problem (2) means that the measured spectrum is a convolution, not a multiplication, so the 'division' step is actually a deconvolution.

The filter transmittance should not vary with intensity unless it has been specifically designed to do so (e.g. a saturable absorber).
 
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