This is an old revision of the document!
Homestake Meeting Minutes, 08/11/16
Attending:
Agenda: Andrew, Gary, Jan, Michael, Victor, Voon, Zhi, Vuk, Pat
Data analysis
Levi (email): Tanner, Pat, and I met on Wednesday of last week to go over Tanner's parameter estimation routine. He mentioned that it was available on the SVN, but I haven't been able to access it. Either I am having troubles with SVN update, which would be unsurprising) or I need to checkout something which I don't have the name for. Anyway, I will talk to Pat about this to see if he is having any issues.
-
Michael: initially did the analysis with 4 stations and got 50x suppression at 0.2 Hz, with some residual structure left over. Now trying to repeat it with the larger array: more channels and larger area. For coherence, using all stations including surface and far-away ones.
Improved to 100x subtraction at 0.2 Hz, no left-over structure in the residual. Using only sub-surface stations for the filter, adding the surface stations did not make much difference. Some excess noise was included at low frequencies - not sure why, in principle the filter should not get worse if you include more data (but in practice, numerical issues could cause a difference).
At 1 Hz still have 5-10x subtraction, and higher frequencies less suppression (2-3x), affected by local disturbances. Might be able to improve at high frequencies. Have 1.3 Hz and its harmonics which are not plane waves.
-
Study of an EQ in Japan, looking at the structure of scattering. Looking at the direction of the incoming wave at different depths. Doing the fk analysis at a specific frequency at the first arrival (P-waves) and then 40 seconds later (well before the surface waves arrive). Using the vertical component of the wave, plotting the horizontal directionality (slowness). Divided the stations into deep (4850+4100) and shallow ones (surface + 300). Using 20sec of data for Fourier transform. Direction near vertical, ellipses peak near the origin.
Zhi: Strong difference between deep and surface stations suggests that the shallow structure modifies the wave.
Victor: think that the deep plots are stretched by the geometry of the stations.
Jan: there is a strong local peak at 1.3 Hz. Why this frequency?
Zhi: searching 1.2-1.4 Hz band and choosing the highest signal within this band.
Victor: during the EQ, the signals is orders of magnitude above the noise.
Zhi: for future, will look at how much station geometry matters, look at the incident angle