Published analyses of HALOE water vapour data have shown an increase in stratospheric water vapour. Here the latest version of the data has been analysed for trends from Jan 1992 to April 1999. This shows an increase in stratospheric water vapour over this period although in the past few years the magnitude of the trend appears to have decreased. A seasonal analysis suggests that large increases in upper tropospheric water vapour in autumn are the source for the stratospheric increases. An analysis of trends in the seasonal amplitude supports this. It is suggested that an increase in the extremity of the Asian monsoon over Indonesia could be responsible.