This is the follow-up analysis of the measurements described in 44881. The method is quite simple: I demodulated the LSC signals (DARM, MICH, SRCL and PRCL) at 20Hz and 200Hz, using the excitation line in SRCL_OUT to set the I and Q phases (I extracted absolute phases of the two lines by band-passing the SRCL_OUT signal and fitting a sinusoid to a short period. Then I generate I and Q demodulation signals as numerical sines and cosines). The demodulated signals (I and Q for both 20Hz and 200Hz) are then decimated to 16 Hz and low passed at 4 Hz.
The two plots below shows the most interesting results, which is how the SRCL to DARM coupling is modulated byt the angular motions. In each panel, I show the demodulated I and Q signals (basically the DARM/SRCL transfer function at either 20 or 200 Hz) and a scaled and shifted version of the ASC input signal corresponding to where the 100 mHz excitation was injected at that time. Left plot is the DARM_IN1 signal demodulated at 20 Hz, the right plot is the DARM_IN1 signal demodulated at 200 Hz.
Note that the excitation amplitude is not calibrated, so we can't do a urad to urad comparison (yet). But in all cases the excitation was larger than the typical motion of the d.o.f. at low frequency, and of comparable size.
In summary
The other plots attached below show the demodulated signals in PRCL_IN, MICH_IN and SRCL_IN:
The code is attached as a ipynb
that's good to see. I think its consistent with what we see in the Summary Pages' Rayleigh grams:
On Saturday night, when the microseism was high (~1 um/s) the Rayleigh stat in the 40-100 Hz band shows a lot of red (many non Gaussian outliers).
On Sunday, when the microseism was down to ~0.5 um/s, the Rayleigh gram is mostly white (Gaussian) in this band.