Λ depression existed over the Australian Bight, the winds were moderate northerly and southerly, as usual in such conditions, there were a few light easterly winds. Isobars were close over eastern Victoria, but there was nothing which seemed to indicate the violent cyclone that developed during that day over southern parts of South Australia and south-west of New South Wales. (See Charts 27 and 28.) This storm formed in the rear of a very substantial anticyclone, then over the Tasman Sea, and it should be noted that it did not act as a secondary and travel round the southern and eastern parts of the high pressure, but it moved towards the northern side of it and against its circulation, thus proving its own Polar impulse and energy, and giving rise to very strong gales and steep barometric grades with great fall of temperatures; these conditions produced extremely heavy and wide spread rains, not only within the storm isobars, but over the whole of the eastern half of Australia. We have no means of tracing the rain to the west of the overland telegraph line, because there are no observing stations there.
May 28th was unfortunately a Sunday, and we have no observations for that day, but on the 29th the cyclone is seen in full
