The 12-month running means of the surface-to-500 mb precipitable water
obtained from analysis of radiosonde data at seven selected locations
showed three types of variability viz: (1) quasi-biennial oscillation
s; these were different in nature at different latitudes and also diff
erent from the QBO of the stratospheric tropical zonal winds; (2) deca
dal effects; these were prominent at middle and high latitudes and (3)
linear trends; these were prominent at low latitudes, up trends in th
e Northern Hemisphere and downtrends in the Southern Hemisphere.