1、地球物理流体动力学导论地球物理流体动力学导论d第y一zhng章 y预bi备zh知shi识1.1 d地qi球w物l理li流t体l力xu学 Geophysical Fluid Dynamics1.2 lu罗s斯bi贝sh数 Rossby number 1.3 密度层结 Density stratification1.4 非xun旋zhun转坐标系中的运动方程 The equation of motion in the non-rotating coordinate system 1.5 旋转坐标系non-rotating coordinate system1.6 旋转坐标系中的运动方程 The e
2、quation of motion in the rotating coordinate system1.7 科氏加速度与罗斯贝数Coriolis acceleration and Rossby number1.8 bo包xn辛ni内s斯k克(Boussinesg)jn近s似 Boussinesq approximation第二章 j基ch础zh知shi识 Basic knowledge2.1 w涡d度vorticity2.2 环流2.3ki凯r尔文定理Kelvin theorem2.4 涡度方程Vorticity equation2.5 位势涡度Potential vorticity （位涡
3、）2.6 热成风Thermal wind2.7 ti泰l勒- 普劳德曼定理Taylor - Proudman theorem2.8 地转运动Geostrophic motion2.9 地转近似和jng静l力近似的结果Geostrophic approximation and the results of the static approximation2.10 地转tu退hu化 Geostrophic degradation2.11 地转适应进程Geostrophic adjustment process2.12 大气和海洋中ro扰dng动的分类与特点Classification and ch
4、aracteristics of the disturbance in the atmosphere and oceans第三章 w无zhn粘qin浅shu水理论Inviscid shallow water theory3.1 yn引yn言Introduction3.2 浅水模式Shallow water model3.3 浅水方程Shallow water equations3.4 wi位w涡shu守hng恒：浅水理论Conservation of potential vorticity3.5 积分关系Integral relations3.6 小zhn振f幅运动Small amplitud
5、e movement 振 = chn ng; 幅 bc, bin () 幅度 3.7 线性地转运动Linear geostrophic motion3.8 等深流体层中的平面波3.9 邦加莱(Poincare)波和凯尔文波(Kelvin) Poincare s wave and Kelvins wave3.10 罗斯贝波Rossby wave3.11 罗斯贝波的动力学zhn诊dun断 Prediction with Rossby wave dynamics3.12 浅水理论的准地转尺度分析Geostrophic scale of the shallow water theory3.13 定常的
6、准地转运动quasi-geostrophic motion3.14 gun惯xng性边界流Inertial boundary current3.15 准地转罗斯贝波Quasi-geostrophic Rossby waves3.16 罗斯贝波的机制3.17 平面3.18 wi纬xing向流中的罗斯贝波the zonal flow Rossby waves3.19 qn群速度Group velocity3.20 多时刻尺度方式3.21 罗斯贝波中的能量和能通量Energy flux3.22 能量chun传b播图Energy propagation diagram3.23 反射进程和辐射条件Ref
7、lection process and Radiation conditions3.24 初始ro扰dng动产生的罗斯贝波Initial perturbation Rossby waves3.25 b闭q区y域中的准地转标准波型quasi-geostrophic standard wave in closed basins3.26 共振彼此作用Resonant interaction 3.27 能量和拟能Energy and enstrophy第四章 m摩c擦h和nin粘xng性li流Friction and viscous flow4.2 tun湍li流xu雪nu诺yng应l力Turbule
8、nt Reynolds stress4.3 i艾k克mn曼cng层 Ekman layer 4.4 近于无摩擦的流动之性质The natural of nearly frictionless flow 4.5 边界层理论4.6 有摩擦时的准地转动力学quasi-geostrophic dynamics in presence of friction4.7 xun旋zhun转jin减ru弱 Spin-down4.8 定常运动4.9 xi斜min面shng上de的i艾k克mn曼cng层Ekman layer on the inclined plane4.10 自由面上的艾克曼层Free surfa
9、ce Ekman layer4.11 有摩擦和地形的准地转位涡方程the quasi-geostrophic potential vorticity equation with Friction and topography4.12 罗斯贝波的shui衰jin减 Rossby waves attenuation、decay4.13 c侧边界摩擦层lateral boundary friction layer第五章 大洋风生环流的jn均zh质模式Homogeneous model of Oceanic wind-driven circulation 5.2 均质模式Homogeneous mod
10、el5.3 s斯wi维r尔d德l鲁p普gun关x系 The Sverdrup Relation 5.4 jng经xing向边界层： mng蒙k克cng层 boundary layers: The Munk layer5.5 斯多美尔模式： 底摩擦层Stommels model: bottom friction layer5.6 惯性边界层理论Inertial boundary layer theory5.7 有摩擦时的惯性流Inertial current in the presence of friction5.8 罗斯贝波和大洋环流的西部强化Rossby waves and the wes
11、tward intensification of the oceanic circulation5.9 定常环流ho耗sn散之积分Dissipation integrals for steady circulation (耗散 hao tan, ho耗sn损hao ton)5.10 自由惯性波Free inertial wave5.11 数值实验5.12 洋底地形的阻碍The effect of bottom topography5.13 对均质模式的总结Concluding Remarks on the homogeneous model第六章 层结流体在球面上的地转运动6.2 球坐标系中的
12、运动方程: 尺度分析6.3 地转jn近s似Geostrophic approximation6.4 静力wn稳dng定概念6.5 天气中天气尺度运动的准地转位涡方程Quasi-geostrophic potential vorticity equation for atmospheric synoptic scale6.6 层结流体中的艾克曼层Ekman layer in stratified fluid6.7 位涡方程的边界条件：大气6.8 海洋中天气尺度运动的准地转位涡方程quasi-geostrophic potential vorticity equation for Ocean Sy
13、noptic scale 6.9 位涡方程的边界条件：海洋6.10 地转能量方程和有效位能The geostrophic energy equation and the available potential energy6.11 层结流体中的罗斯贝波Rossby waves in a stratified fluid6.12 罗斯贝波标准模态: 重直结构方程The Rossby waves standards modes： The vertical structure equation6.13 大气中的强p迫zh驻波Forced sationary waves in the atmosphe
14、re6.14 波动- 纬向流彼此作用定理wave - zonal flow interaction theorem6.15 层结海洋中的地形波Topography wave in stratified ocean 6.16 多层模式Layers model6.17 两层模式中的罗斯贝波Rossby waves in the two-layer model6.18 多层模式与层差分模式的关系Relationship between the layer modes to the “level” model6.19 地转近似：。， s斯wi维r尔d德l鲁p普gun关x系- Geostrophic a
15、pproximation6.20 地转近似Geostrophic approximation6.21 sh湿yu跃层问题The thermocline problem第七章 不稳固理论7.2 不稳固问题的提出：lin连x续cng层ji结m模sh式 -Formulation of the Instability problem: Continuously stratified model7.3 线性稳固性问题： 不稳固的条件7.4 标准波型- Normal modes7.5 相速和增加率的范围Bound on the phase velocity and the growth rate 7.6
16、xi斜y压不稳固：基体机制Baroclinic instability: the basic mechanisms 7.7 y伊d迪模式Eadys model7.8 qi恰n尼模式和临界层 Charneys model and the critical layer7.9 两层模式的不稳固：问题的提出Instability in the Two-layer model: Formulation7.10 两层模式中的标准波型：不稳固的必要条件 Normal modes in the Two layer Model: a necessary condition for instability7.11
17、 两层模式中的斜压不稳固:fi菲l利p蒲模式Baroclinic instability in the two-layer model: Philips model7.12 摩擦效应Friction effect7.13 非纬向基体流的斜压不稳固The baroclinic instability of non-zonal Flows7.14 正压不稳固Barotropic instability7.15 具有水平和重直切变的基体流之不稳固instability of currents with horizontal and vertical shear stress7.16 斜压不稳固的非线性理论Non-linear theory of baroclinic instability第八章 非地转运动Ageostrophic motion8.1 各向异性尺度Anisotropic Scale8.2 大陆架波Continental shelf waves8.3 有耗散的层结流体重的慢环流The slow circulation of a stratifed, dissipative Fluid8.4 fng锋shng生理论Frontogenesis theory 8.5 ch赤do道波动Equatorial fluctuations
