NAVAER-50-1P-521
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Bureau of Aeronautics - The Jet Stream
It is true in many fields Of science that the requisite data for the revision Of an antiquated hypothesis or the development of a new tneory are available long before the actual formulation Of a neoteric concept. Such has bæn the case Of the Jet Stream in the science Of Meteorology. As early as 1933, a cross.section depicting a relatively narrow, high.speed stream of air in the upper weterlies was published in the text, Physikalische Hydrodynamik. The implications of thie cross-section were disregarded by the authors themælves, possibly in view of the inadequacy of the observational material upon which it was bag-d. Eleven years later, in 1944, Dr. Hurd C. Willett published mean crow-sections to the North American continent which also substantiated the existence Of a meandering, high.velocity stream of air particles in the uwr tropospheric regions. It wasn't until the year however, that this lat—t meteorological phenomeuon bæame the Of rather intensive reæarch at a Navy•gpnsored researgh project at the University of Chicago and that its numerous potentialities were gradually l*ing to that time, considerable research on the has conducted by various individuals and institutions at different geographical locations, with the that a great deal of uncoordinated and sometimes controversial material has been presented. material has in divers profesional journals, bulletins and periodicals, not readily available to the Naval Aerologist in the field or afloat. Becauæ of the tremendous import and the numerous potentialities of this newly• discnvered *enomenon, it was demed imperative that an evaluation and summary 0? ex•szing research and data on the Jet Stream be compiled under a single cover and distributed to the Naval Aerological Service as soon as possible. Accordingly, Task 6 (TED-UM-MA-501.6), JET STREAM ANALYSIS, was assigned to Project AROWA by Bureau Of Aeronautics serial 2'W)3 dated 14 March, 1951, for proecution and/or coordination. This document is the coordinated effort in the fulfillment Of this purpoæ. Much Of the material •preænted herein is bawd on l&tures by Dr. Riem of the Department of Meteorology, University of Chicago, who also edited the manuscript. Intimately associated with the entire project, also, were Mesrs. M. A. Alaka, C. L Jordan, and R. J. Renard of the Department of Meteorology, University Of Qiicago. This publication encompasses the synoptic structure Of the Jet Stream, as well as its climatology and relation to middle latitude cyclones and extended forecasting. In addition, one chapter is devoted to the techniques and procedures Of high-level wind analysis. The dynamic principles relating to Jet Siream formation and maintenance are also incorporated. Much of the information presented herein has been derived from a great variety Of material, with the result that several different units of Wind are ex• presed throughout. It is regretted that time did not permit the conversion Of the various units to one system.
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