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In ordinary seismographic observation, the time of initiation of ground oscillations is recorded.
Studying this kind of mystery is what Noνa was built for, and this confirmation of neutrino oscillations is just the start.
Dissipation of the Alfven oscillations is small enough.
b The magnitude of oscillations is gradually decreased.
The occurrence of dynamic impatt oscillations is analyzed.
The existence of periodic oscillations is numerically established.
The nature of the single and multipeak oscillations is discussed.
A unified approach to analysis of impact oscillations is proposed.
But the number of oscillations is much lower since the LCR is a low-order retarder.
Note how the amplitude of the oscillations is reduced in the low part of the spectrum.
Duration of tsunami oscillations is around 1 day at the Bodrum station (Fig. 3a).
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