GOTOH Kanefusa | Research Institute for Mathematical Science,Kyoto University
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概要
関連著者
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GOTOH Kanefusa
Research Institute for Mathematical Science,Kyoto University
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Gotoh Kanefusa
Research Institue For Mathematical Sciences University Of Kyoto
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MIZUSHIMA Jiro
Department of Information Science,Sagami Institute of Technology
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Mizushima Jiro
Department Of Information Science Sagami Institute Of Technology
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Mizushima J
Doshisha Univ. Kyoto Jpn
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Gotoh Kanefusa
Research Institute For Mathematical Science Kyoto University
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Mizusawa Jiro
Department Of Mechanical Engineering Faculty Of Engineering Doshisha University
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YANASE Shinichiro
Engineering Mathematics,Faculty of Engineering,Okayama University
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YANASE Shinichiro
Department of Mechanical Engineering, Faculty of Engineering, Okayama University
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FUJIMURA Kaoru
Japan Atomic Energy Research Institute,Tokai Research Establishment
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Y Chung
Department Of Physics And Astronomy Howard University
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Mizushima Jiro
Department Of Information Sciences Sagami Institute Of Technology
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Mizushima Jiro
Department Of Physics Faculty Of Science University Of Kyoto
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Fujimura K
Japan Atomic Energy Research Institute Tokai Research Establishment
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Fujimura Kaoru
Japan Atomic Energy Research Institute
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Gotoh K
Nagoya Univ. Nagoya
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Yanase Shinichiro
Engineerin Mathematics Faculty Of Engineering Okayama University
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Yanase Shinichiro
Department Of Engineering Sciences Okayama University
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Yanase Shinichiro
Department Of Engineering Sciences Faculty Of Engineering Okayama University
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GOTOH Kanefusa
Research Institute for Mathematical Sciences,Kyoto University
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Gotoh Kanefusa
Research Institute for Mathematical Science, University of Kyoto
著作論文
- The Weakly Nonlinear Stability of the Two-Dimensional Jet and Wake
- The Instability of Natural Convection in a Vertical Fluid Layer in the Presence of an Adverse Temperature Gradient
- Ultrasonic Attenuations in Magnetic Fluids
- Nonlinear Stability of Parallel Flows
- The Stability of Convection between Two Parallel Vertical Walls
- Nonlinear Evolution of the Disturbance in a Natural Convection Induced in a Vertical Fluid Layer