Thanks Lynn.
The intensity graph does look better in the sense that it looks less
complicated. However, can you help me in correlating the arbit signal
eta, that I am currently simulating, with this intensity chart?
What is finally available to me is only the output intensity from which
I have to find out the height of the wave (eta in the VI) at the point
where the sensor is located.
Incidentally, if you look at the eta that I am generating, at X= 7 and
8, the value is only 0.2 and 0.5 m respectively. This is the height of
the tsunami at the said depth (4000m). However, if you look at the
corresponding wavelength, (Arbit Signal2 in the VI) at X= 7 and 8, Y =
150 Kms!! This long wavelength is what is distinguishing a tsunami from
a surface wave and it is only this tsunami wave which generates a
significant dynamic pressure which the sensor is sensing. Even a freak
wave with say eta = 20m will not cause any change in the pressure (
only about 10^-37)being recorded at the bottom as its wavelength will
be typically only a few meters, say 500m.
Do you think I should employ some kind of a demodulation to the output
intensity ( of course I don't have the demodulation toolkit!!)? would
be grateful if you could assist me in finding some relation between the
STFT output (or any other function) and wave height.
Thanks again.