Estimates of the atmospheric Integrated Water Vapor (IWV) for 30 GPS sites
in Europe, covering the period from January 1997 until August 1999 are anal
yzed. For every month the diurnal cycle in the IWV is estimated by averagin
g the data referred to that particular hour for that month. The average pea
k-to-peak value of the diurnal cycle during the winter months is between 0.
6 mm and 1.5 mm, while during the summer months the peak-to-peak value is b
etween 0.8 mm and 3.2 mm. The GPS results at the Onsala Space Observatory a
re compared to those obtained from a co-located microwave radiometer and ne
arby (distance 37 km) radiosonde launches. We find that the estimated diurn
al variations are comparable to the uncertainties in the measurements and t
he models used. However, a clear dependence between the peak-to-peak value
and latitude of the observations is seen during the summer months. No such
dependence is detected for the winter period. (C) 2001 Elsevier Science Ltd
. All rights reserved.