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The data coming from the bolometers is characterized by long drifts
that are correlated to the temperature variations inside the cryostat,
pendulations and altitude variations. There is also a scan synchronous
parasitic signal that can be monitored using high frequency channels.
These extra signal are decorrelated and we are left with a time stream
that still exhibits low frequency drifts due to imperfections in the
decorrelation and residual signals.
Jean-Christophe Hamilton ISN
2001-12-01