I've started working on PSD for seismic signals. In theory, PSD signal can be expressed in 2 ways. One in $(PSD=g^2/Hz)$ and other in $PSD=((meter/second^2)^2/Hz)$ and also ASD=(√PSD). Here $g$ is the acceleration.
More details have found in the link https://ucum.org/ucum.html#section-Special-Units-on-non-ratio-Scales
I want to find the amplitude of the spectrum in $(meter.second)^2/Hz$ from the expression of PSD. I don't clearly find a way to get the amplitude at a specific frequency in the unit of $(meter.second)^2/Hz$. How can I get the amplitude in the unit of $(meter.second)^2/Hz$? Probably the unit of amplitude may be derived from the unit of PSD, but I've no idea how to get the amplitude in the above unit?
OR
Without correlating the above PSD/ASD, what is the process to express amplitude (e.g. seismic signals) in terms of $(meter.second)^2/Hz$?
Answer (Confused)
So far I understand, one can find the amplitude from the $PSD$ in sunch a way that amplitude, $A = √PSD * scaling_factor$. $scaling_factor= 2/(fs*S)$ depends on the size of window and the sampling frequency of the signal (https://dsp.stackexchange.com/questions/32187/what-should-be-the-correct-scaling-for-psd-calculation-using-tt-fft/32205#32205). Am I correct?
$S$ - sum of squared samples of window function $f_s$ - sampling frequency Scaling coefficient $2$ takes into account removal of energy at negative frequencies (we drop this side of PSD).
Can anyone have any explanations?