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Jule Charney : ウィキペディア英語版 | Jule Gregory Charney
Jule Gregory Charney (January 1, 1917 – June 16, 1981) was an American meteorologist who played an important role in developing weather prediction. He developed a set of equations (The Quasi-Geostrophic Vorticity Equation) for calculating the large-scale motions of planetary-scale waves. He gave the first convincing physical explanation for the development of mid-latitude cyclones known as the Baroclinic Instability theory. He is considered the father of modern dynamical meteorology. ==Professional life== Charney studied physics at UCLA where he completed his masters in 1940 and Ph.D. in 1946. In the 1950s, he was involved in early research on numerical weather prediction together with John von Neumann at the Institute for Advanced Study (IAS) in Princeton, New Jersey. He and von Neumann brought over from England a recent Ph.D. in meteorological calculations, Bruce Gilchrist, to work on this task using the institute's computer, the IAS machine.〔Gilchrist, Bruce, , ''Columbia University EPIC'', 2006, pp.7-9. (archived 2006) Contains some autobiographical material on Gilchrist's use of the IAS computer beginning in 1952.〕 Their collective work paved the way for the founding of the Geophysical Fluid Dynamics Laboratory. From 1956 until his death in 1981, Charney was a faculty member at the Massachusetts Institute of Technology.
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