BAMOS Vol 30 No. 3 2017 | Page 25

BAMOS Sept 2017 Figure 2. Mr John Moss, an old aged pensioner, sits amidst the ruins of his house in Naremburn. Image: The Town and Country Journal, 4 April 1906. These were some of the earliest images of damage produced by an Australian tornado and indicate a possible rating of EF 3 on the Enhanced Fujita Scale. It is likely that it was a similar strength to the Brighton tornado that struck the bayside suburbs of Melbourne some 12 years later, on 2nd February 1918. A low-pressure cell was located over southwest NSW and rainfall reports indicated widespread totals across NSW from 9 am on the 26th to 9 am on the 27th of March. These included 335 points (85 mm) at Moruya, 265 points (67 mm) at Bowral, and 155 points (39 mm) at Gundagai. The meteorological situation This indicates that the thunderstorm activity on the eastern flank of the low — Sydney in particular — was only part of a significant rainfall event that affected much of NSW. Despite the fact that Australia’s first “weather map” was printed in The Sydney Morning Herald on 5 February 1877, the synoptic chart was not a regular daily feature in New South Wales newspapers across the next 30 years. Attempts to find the synoptic chart of 27 March 1906 were unsuccessful in either The Sydney Morning Herald or The Age from Melbourne, but copies were found in two Adelaide newspapers: The Register and The Advertiser, the former of which is reproduced here (Figure 3). Comments by Meteorologist the Acting Government The Acting Government Meteorologist Mr. Henry Ambrose Hunt was consulted for an explanation and this was printed in The Sydney Morning Herald article of 28 March: “The tornado”, he remarked, “was due to local ascending currents of air — a whirlwind on a violent scale. Tornadoes are but occasionally experienced to the eastward of the mountains and but rarely in the city. In the west, however, tornadoes are of common occurrence. The reason for this is that the convectional action is more intense to the west of the highlands than to the eastward”. Just a few months later, in November, Hunt would leave Sydney for Melbourne as the Head of the newly formed Commonwealth Meteorological Bureau. Figure 3. The synoptic chart for 27 March 1906 as it appeared in The Register, Adelaide the next day. Image: The Register, 28 March 1906. 25