Irene, Federico
Figure 1 compares Kagra seism (PEM-SEIS_EXV_GND_X) and Virgo End station (Guralp 60T, here one horizontal channel): while Microseism region is similar, in the region between 1 and 30Hz kagra is 10 to 100 times quiter(wow!), above 30Hz seism increases (both Virgo and kagra), but in this region likely the seimometers's response is probably not flat.
Figure 2 compares sound spectra in Kagra center area (we used the Virgo infrasound microphone B&K 4193 that we carried with us) and Virgo central experimental hall now during O3 science mode (same model of microphone). NOTE that at Kagra during this period of time the center area was silenced by switching off several fans (see 8887). See that the acoustic noise level is similar(!).
Figure 3 compares magnetic spectra at KAGRA and Virgo (Metronix MFS-06 magnetometer). In this plot the PEM-MAG_BS_BOOTH magnetometer was temporary placed next to the IYC cryocooler (see 8881) that probably explains some of the noise peaks (1.6Hz and 1.6Hz spaced sidebands around 31Hz for example).
Figure 4 (similar to figure 3) compares Virgo magnetometer with KAGRA magnetometer at EYC.