Remote reference transfer function¶
It is possible to calculate out the remote reference transfer function for each window (and evaluation frequency). Whilst the geoelectric and geomagnetic fields may vary with time, the components of the remote reference transfer function should stay constant through time. Calculating out transfer function components on an evaluation frequency basis for each window allows the study of the variation in remote reference transfer function components over time and the identification of noisy windows which should be removed from further analysis.
Note
Currently, the only remote reference transfer function calculated out by statistics is the impedance tensor
Important
The resistics name for the remote reference transfer function statistic is: RR_transferFunction.
The components of the remote reference transfer function statistic are:
Ex Hx RealRR
Ex Hx ImagRR
Ex Hy RealRR
Ex Hy ImagRR
Ey Hx RealRR
Ey Hx ImagRR
Ey Hy RealRR
Ey Hy ImagRR
An example of window-by-window remote reference transfer function esimates over time is shown below.
In general, the values appear quite consistent but there is significant spread. The result is illustrated in the histogram plots below, which are quite Gaussian apart from outliers.
Crossplots are a useful way of visualising the remote reference transfer function in the complex plane. In best cases, there should be a tight spread.
2-D histogram plots or density plots can help show the spread in the remote reference transfer function estimates. Here, there does appear to be some spread around the central point, however it does appear largely 2-D Gaussian.