Abstract. Integrated Water vapour (IWV) has been measured since 1994 by the TROWARA microwave radiometer in Bern, Switzerland. Homogenization techniques were used to identify and correct step changes in IWV related to instrument problems. IWV from radiosonde, GPS and SPM was used in the homogenisation process as well as the IWV differences calculated between mountain and valley weather stations. The average IWV of the homogenised TROWARA time series was 14.4 mm over the 1996–2007 period, with maximum and minimum monthly average values of 22.4 mm and 8 mm occurring in August and January, respectively. A weak diurnal cycle in TROWARA IWV was detected with an amplitude of 0.32 mm, a maximum at 21:00 UT and a minimum at 11:00 UT. For 1996–2007, TROWARA trends were compared with those calculated from the Payerne radiosonde and the closest ECMWF grid point to Bern. The radiosonde midnight trend of +0.087 (standard error 0.046) mm/y was significant at the 90% level. The radiosonde trend for all measurement times, +0.098 (0.061) mm/y, and the TROWARA midday trends, 0.068 (0.043) mm/y, were significant at the 89% level. Seasonal Mann Kendall analysis revealed a significant positive trend in July of +0.19 (0.14) to +0.34 (0.25) mm/y for all three datasets. In December, the Payerne radiosonde showed a non-significant negative trend of −0.12 (0.13) mm/y, whilst ECMWF and TROWARA indicated a significant negative trend of −0.20 (0.14) and −0.36 (0.24) mm/y, respectively.