The most intense of these systems have many of the characteristics of subtropical cyclones.[5] They develop between 25˚ south and 40˚ south and within 5˚ of the eastern Australian coastline,[1] mostly during autumn and early winter with a peak in June.[6][7][8] Prior to the introduction of satellite imagery in the early 1960s, many east coast lows were classified as tropical cyclones. ECLs are responsible for more than half of all days with rainfall above 50 mm (2.0 in) in the southeastern seaboard.[9]
^Harper, Bruce; Ken Granger (2000). "Chapter 5: East coast low risks"(PDF). In K. Granger & M. Hayne (ed.). Natural hazards and the risks they pose to South-East Queensland. Australian Geological Survey Organisation in conjunction with Bureau of Meteorology. ISBN0642467080. Retrieved 7 April 2013.