this night a large range variation has been observed and it is due to a worsening of the DIFF(+) loop, see Figure 1.
The angular error signals shows a strong instability at 350mHz (to be investigated) while the microseismic noise is more or less stationary.It is worth to be noted that the low frequency worsening of the angular error signal generates a strong worsening of the noise above 10Hz which behaves as timing noise (1Hz harmonics), see Figure 2.
to be investigated