In the fall of 1997 the Atmospheric Radiation Measurement program conducted
a study of water-vapor-abundance-measurement at its southern Great Plains
site. The large number of instruments included four solar radiometers to me
asure the columnar water vapor (CWV) by measuring solar transmittance in th
e 0.94-mum water-vapor absorption band. At first, no attempt was made to st
andardize our procedures to the same radiative transfer model and its under
lying water-vapor spectroscopy. In the second round of comparison we used t
he same line-by-line code (which includes recently corrected H2O spectrosco
py) to retrieve CWV from all four solar radiometers, thus decreasing the me
an CWV by 8-13%. The remaining spread of 8% is an indication of the other-t
han-model uncertainties involved in the retrieval. (C) 2001 Optical Society
of America.