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Table of Contents
Glimpse of the RAAF Meteorological Service Preface Foreword Introduction Chapter 1: Growing Up Chapter 2: Port Moresby Before Pearl Harbour Chapter 3: Port Moresby After Pearl Harbour Chapter 4: Allied Air Force HQ and RAAF Command, Brisbane General Douglas MacArthur We Join Allied Air Headquarters, Brisbane Ralph Holmes Forecasting Procedure WAAAFs and Other Staff Briefing MacArthur & Co Domestic Affairs The Yanks Are Coming Japanese Advance Across Owen Stanley Range General George C. Kenney Additional Staff Staff Arrangements Long Range Forecast Investigations into Tropical Meteorology Radiosondes Analysis Statements MacArthur's Remarkable Strategy A New Direction Tropical Weather Research Bulletin RAAF Command, Pat Squires and Henry Phillpot Chapter 5: Japan Surrenders and We Are Demobilised Epilogue Acknowledgements Appendix 1: References Appendix 2: Milestones Appendix 3: Papers Published in Tropical Weather Research Bulletins Appendix 4: Radiosonde Observations 194146 Index Search Help Contact us |
Forecasting ProcedureIn addition to his duties as officer-in-charge, Ralph shared with me the routine of producing forecasts and other information for Allied Air Headquarters. For this we plotted and analysed weather observations over an area extending from west to east from the longitude of Singapore to that of Fiji and from about latitude 20°N to about 40°S. As had been the case in Port Moresby, pilot balloon observations were represented on the chart using the 'snake' method of representation. We continued to suffer from a lack of knowledge of the behaviour of the atmosphere in low latitudes. In those days some progress was being made in developing an understanding of the mechanism of the atmosphere in higher northern hemisphere latitudes but there was little if any investigation of the atmosphere in low latitudes.A feature of synoptic analysis in the RAAF Meteorological Service and many other meteorological services in other parts of the world at that time, was the air-mass and frontal model (alternatively called the polar front model) first developed by Scandinavian meteorologists during World War I. The term 'front' had been adopted to indicate the boundary between different air-masses from the use of the same word to indicate the dividing line between two opposing armies. This model had been viewed with little enthusiasm by other meteorological services between the two World Wars except for isolated far-seeing meteorologists such as Kidson and Palmer in New Zealand. Treloar and Squires had studied the application of these models in the headquarters of the RAAF Meteorological Service in Melbourne but with the rather meagre observational network, particularly in the upper air, there was a considerable amount of subjectivity in the practical application of the model. This model was of a character much different from the geophysical fluid dynamic models developed after World War II, improved versions of which run on computers today. Although Richardson had developed a primitive numerical model in World War I, the full potential of such models could only be achieved by the use of a sophisticated electronic computer which did not become available until the late 1940s.
People in Bright Sparcs - Kidson, Edward; Squires, Patrick; Treloar, Harry Mayne
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