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Federation and Meteorology |
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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 Melbourne to Cambridge, Massachusetts Long-range Forecasting Synoptic Meteorology Dynamic Meteorology I, II, III Dynamic Meteorology IV Physical Meteorology Seminars Audrey Joins Me in Boston Was it Worthwhile? Chapter 5: The Dwyer Years, 1955 to 1962 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 |
SeminarsDuring the semesters regular seminars were held at which staff and students presented papers. I had elected to enrol for the degree of M.Sc. which included the requirement for submission of a thesis. I was able to use the northern and southern hemisphere charts which Willet, Austin and Starr had used for their calculation of indices in studying the general circulation and the subject of my thesis was the distribution of high and low pressure centres at mean sea level in the two hemispheres, and a comparison of upper air zonal circulations roughly along longitude 150 deg E.My thesis concluded that the general circulation in the two hemispheres was similar but that the different distribution of land masses produced significant differences in the location of cyclones and anticyclones at mean sea level. My thesis and general performance in my course work were considered to justify the award of the M.Sc. An article based on the thesis was accepted for publication in the prestigious Quarterly Journal of the Royal Meteorological Society. I was asked to present a talk on my thesis to a Departmental seminar. One innovation I introduced into my seminar talk was a map of North America on which I superimposed a map of Australia using the same conical projection with identical parallels of latitude and with meridians of longitude both running from west to east. Longitude 120°E over Australia corresponded with 110°W over the US and longitude 150°E over Australia corresponded with 80°W over the US. The objective of this representation was to emphasise that Australia is located so much closer to the equator than the US and that there could be significant differences in the mechanisms of the atmosphere experienced in the two continents. To make the comparison valid I considered it necessary to have both west coasts on the left hand side of the illustration which meant that the chart of Australia was 'upside down' and a mirror image. Although I had no difficulty in seeing the logic of this arrangement Professor Houghton told Audrey, who attended the seminar, that he had considerable difficulty in getting my message. On later occasions, to emphasise this geographical difference between Australia and North America, I arranged a similar map to be included in the report of our international tropical cyclone symposium in Brisbane in 1956. This was intended to emphasise the geographical factors which might contribute to some differences in intensity and behaviour of hurricanes in North America and tropical cyclones in Australia.
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