Reference-assisted spectral offset separation uses an additional reference observation to distinguish a physical spectral change from an instrumental offset. The reference must respond to the offset in a known way while excluding, or separately modelling, the sample’s physical change. Merely collecting another signal does not guarantee spectral offset identifiability.
For a local linear measurement model, writewhere is the desired change, the shared offset and . With known sensitivities and zero-mean residual errors,removes the offset contribution. This is a subtraction of modelled responses, not a claim that the uncorrected sample and reference frequencies are physically identical.
An original example uses , and , giving . A reference may have a much larger offset response than the sample; the response ratio supplies the necessary conversion.
The uncertainty of a reference-corrected spectral change depends on joint errors. For fixed ,With , and correlation , this gives approximately ; assuming independence instead gives . The primary GUM supplies the correlated-input propagation rule used in this calculation.[ref]
If is itself estimated, its uncertainty also matters. Under an additional independent-input first-order approximation, the contribution is . Large uncertainties, correlations with the fitted ratio or nonlinear responses require a more complete analysis.
A controlled experiment records stable reference features through the same acquisition and processing chain while deliberately perturbing the instrumental offset. This can estimate and test whether the response is linear. Sample/reference timing must also match the assumed offset: a drifting offset at different acquisition times can leave an uncorrected residual. Repeated paired data, rather than unrelated error estimates, are needed to characterize the relevant covariance.