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Table of Contents
Memories of the Bureau, 1946 to 1962 Foreword Terminology Prologue Preface Chapter 1: The Warren Years, 1946 to 1950 Chapter 2: International Meteorology Chapter 3: The Timcke Years, 1950 to 1955 Chapter 4: A Year at the Massachusetts Institute of Technology Chapter 5: The Dwyer Years, 1955 to 1962 Leonard Joseph DwyerA Complex Character Reorganising the Bureau Public Weather Services Forecasts for the General Public Importance of Radio Stations The Advent of Television Automatic Telephone Forecast Service Beacons Wording and Verification of Forecasts Warnings Services for Aviation Atomic Weapons Tests Atomic Weapons TestsMosaic G1 and G2 Atomic Weapons TestsBuffalo 1, 2, 3 and 4 Atomic Weapons TestsOperations Antler, 2 and 3 Atomic Weapons TestsMinor Trials Instruments and Observations Radiosondes Radar/Radio Winds and Radar Weather Watch Automatic Weather Stations Sferics Meteorological Satellites Telecommunications Tropical Cyclones Bureau Conference on Tropical Cyclones International Symposium on Tropical Cyclones, Brisbane Hydrometeorology Design of Water Storages, Etc Flood Forecasting Cloud Seeding Reduction of Evaporation Rain Seminar Cloud Physics Fire Weather Research and Special Investigations International Activities The International Geophysical Year The Antarctic and Southern Ocean International Symposium on Antarctic Meteorology International Antarctic Analysis Centre ADP, EDP and Computers Training Publications Management Conference Services Conference CSIRO and the Universities Achievements of the Dwyer Years Chapter 6: A Springboard for the Future Appendix 1: References Appendix 2: Reports, Papers, Manuscripts Appendix 3: Milestones Appendix 4: Acknowledgements Appendix 5: Summary by H. N. Warren of the Operation of the Meteorological Section of Allied Air Headquarters, Brisbane, 194245 Endnotes Index Search Help Contact us |
SfericsIn his reminiscences (Metarch Papers No 8, February 1996) Allan Cornish describes how early in the war Bill Boswell of the PMG's Research Laboratories was keen to employ direction finding radio apparatus to locate lightning. Older readers will recall that in the early days of radio, lightning caused static, the noise of which interfered with reception of their favourite radio programs.Weather News No 3 of October 1956 records that the Bureau had acquired equipment for three atmospheric direction finding (sferics) stations. The equipment was relatively simple, consisting of two crossed loop aerials tuned to 10 kc/s (the radio frequency of the signal produced by a lightning discharge) which with suitable circuitry could provide the bearing of the lightning discharge. Similar equipment had been used on ships and aerodromes to obtaining bearings of radio signals from shore stations or from aircraft. I believe a similar locally built sferics system had been tested during the war by Boswell and Cornish. The sferics network commenced operation in May 1957 with stations at Eagle Farm, Charleville and Garbutt. A fourth station was established in Cloncurry in April 1959. An additional southern network was established in April 1960, originally with stations at Laverton (Melbourne) and Wilkes (Antarctica), a third station being established at Guildford (Perth) in August 1960. This southern network had the advantage of three widely-spaced stations which assisted accuracy. The sferics system was an interesting experiment in supplementing the Bureau's overall observations system. It could not be considered as a solution to the problem of routine synoptic analysis as the detection of lightning depended on the occurrence of well-developed thunderstorms, which are daily occurrences in northern Australia and New Guinea at certain times of the year but are relatively rare over the southern coastline of Australia and the Southern Ocean. In certain parts of Australia a thunderstorm is not always accompanied by heavy rain. It is a sign of convective turbulence. Some thunderstorms accompany fronts, others do not. In summary it may be said that the sferics system was successful in detecting thunderstorms, often in areas of deficient observations. As thunderstorms occur less frequently in higher latitudes there were less occurrences detected in those regions. Sferics were useful for the forecaster, and in alerting electricity authorities of the possibility of power failures. The advent of the meteorological satellite largely replaced the need for sferics observations.
People in Bright Sparcs - Cornish, Allan William; Dwyer, Leonard Joseph
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