The current SMA data from the on-line system has not been corrected
for system temperature. However the frequently measured T
values for each antenna are stored in the header of MIR data for
each pair of antennas. The antenna-based T
are computed
and stored in the header of uvdata in Miriad while the data are loaded
using smalod. The measured T
can be used
to calibrate the atmosphere. The effects of varying opacity,
both in time and in elevation, are then removed from the measured
fringe amplitude. Amplitude calibration is critical to the
achievable dynamic ranges in imaging.