旋转向量水平分量对大洋内波方程的影响
Effect of horizontal component of rotation vectoron equations for oceanic internal waves
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摘要: 在物理海洋学问题中,一般地采用固结在所研究海区中的直角笛卡尔坐标系(f-平面或β户平面近似),即原点在无扰动海面,z,y,x轴分别为向东、向北和向上.
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Key words:
- Oceanic internal waves /
- “traditional” approximation /
- rotating fluid
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Eckart C.Hydrodynamics of Oceans and Atmospheres.Pergamon,Oxford,1960,96 Garrett C J R,Munk W H.Space-time scales of internal waves.Geophys.Fluid Dyn.,1972,(2):225-264 Phillips O M著,徐德伦,李心铭译.上层海洋动力学.北京:科学出版社,1983 LeBlond P H,Maysak L A.Waves in the Ocean.Elsevier,Amsterdam-Oxford-New York,1978,40-76 Kamenkovich V M著,赵俊生,耿世江译.海洋动力学基础.北京:海洋出版社,1983,79 方欣华,王景明.海水压缩性对海洋内波的影响.山东海洋学院学报,1984,14(3):13-18 Müller P,Olbers D J,Willebrand J.The IWEX spectrum.J.Ueophys.Res.,1978,83,479-500 -
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