伍荣生文选

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 ApproximationBaroclinic 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 MotionThe 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 ApplicationThe 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 MotionGeostrophic Adjustment of a Zero Potential Vorticity Flow Initiated by a Mass ImbalanceGeostrophic Adjustment：Frontogenesis and Energy ConversionA Study on Frontal Motion over OrographyFrontogene sis，Evolution and the Time Scale of Front FormationA Numerical Study of Geostrophic Adjustment and FrontogenesisInteraction of Orographic Disturbance with FrontEvolution 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 OscillationsMechanism of Balanced Flow and FrontogenesisInteraction of Diabatic Frontogenesis and Moisture Processes in Cold—Frontal Rain BandⅣ 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 CyclonesⅤ 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 FlowAn Optimal Spatial Finite—Difference Operator Which Reduces Truncation Error to a MinimumShearing Wind Helicity and Thermal Wind Helicity附件