Global Positioning System (GPS) receivers, water vapor radiometers (WV
Rs), and surface meteorological equipment were operated at both ends o
f a 50-km baseline in colorado to measure the precipitable water vapor
(PWV) and wet delay in the line-of-sight to GPS satellites. Using hig
h precision orbits, WVR-measured and GPS-inferred PWV differences betw
een the two sites usually agreed to better than 1 mm. using less preci
se on-line broadcast orbits increased the discrepancy by 30%. Data sim
ulations show that GPS measurements can provide mm-level separate PWV
estimates for the two sites, as opposed to just their difference, if b
aselines exceed 500 km and the highest accuracy GPS orbits are used.