目录 自序 伍荣生小传 Ⅰ 波动动力学 大地形与扰动的不稳定 大地形与正压扰动的移行 正压大气中波动共振与能量变化 基本气流和大地形对于正压波动的作用 长波近似与大气中的线性与非线性Rossby波 Rossby波的能量、能量通量与Lagrange函数 关于非均匀介质中波的传播问题 非线性Rossby波及其相互作用——I.Rossby包络孤立波的碰撞 Ⅱ 边界动力学 An Apnalysis of Ekman Boundary Layer Dynamics Incorporating the Geostrophi, Momentum Approximation Baroclinic Instability and Frontogenesis with Ekman Boundary Layer Dynamics Incorporating the Geostrophic Momentum Approximation 半地转气流的动力学特征 非线性Ekman层的动力特征 The Influences of Orography upon the Flow Within Ekman Boundary Layer under the Approximation of Geostrophic Momentum 论赤道地区的大气边界层 Ekman动量流的动力特征与锋生 The Ekman Boundary Layer over Orography:An Analysis of Vertical Motion The Surface Friction and the Flow over Mountain 边界层动力学中的Ekman动量近似 The Ekman Momentum Approximation and Its Application The Influence of the Geostrophic Wind Advection Approximation on a Well Mixed Layer Ⅲ锋面动力学 The Theory Study of the Influence of the Topography on the Cold Frontal Motion Geostrophic Adjustment of a Zero Potential Vorticity Flow Initiated by a Mass Imbalance Geostrophic Adjustment:Frontogenesis and Energy Conversion A Study on Frontal Motion over Orography Frontogene sis,Evolution and the Time Scale of Front Formation A Numerical Study of Geostrophic Adjustment and Frontogenesis Interaction of Orographic Disturbance with Front Evolution and Fmntogenesis of an lmbalanced Flow the Influence of Vapor Distribution and Orographic Forcingt 地形上空边界层流中低层锋面结构的理论研究I:冷锋、均匀地转流 Investigation on Geostrophic Adjustment,Frontogenesis and Oscillations Mechanism of Balanced Flow and Frontogenesis Interaction of Diabatic Frontogenesis and Moisture Processes in Cold—Frontal Rain Band Ⅳ 热带气旋动力学 The Conservation of Helicity in Hurricane Andrew(1 992)and the Formation of the Spiral Rainband 热带气旋碧丽斯(2000)发生的数值模拟:非对称流的发展及转换 北太平洋夏季热带海区大气运动的平衡关系 冷空气入侵对热带气旋发生发展的影响 The Effect of Surface Friction on the Development of Tropical Cyclones Ⅴ 其他动力学问题 提高差分与微分逼近程度的一个新方案 旋转大气中运动的多时态特征和时间边界层(1I) 准地转演变过程中的多时态特征 论涡度拟能的变化 CISK理论中的若干问题 广义涡度与位势涡度守恒定律及其应用 Helicity Dynamics of Atmospheric Flow An Optimal Spatial Finite—Difference Operator Which Reduces Truncation Error to a Minimum Shearing Wind Helicity and Thermal Wind Helicity 附件
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