Infrared propagation at low altitudes is determined by extinction that is d
ue to molecules and aerosol particles and ray bending by refraction, three
effects that control the mean value of the signal. Interference causes the
signal to fluctuate, or scintillate, about the mean value. We discuss; the
design, calibration, and limitations of a held instrument for measuring opt
ical propagation inside the midwave and long-wave infrared atmospheric wind
ows. The instrument, which is accurate to +/-10%, has been used to investig
ate aerosol, refractive, and scintillation phenomena in the marine boundary
layer. (C) 2000 Optical Society of America.