| 1. | Geostrophic adjustment and frontogenesis
地转适应与锋生 |
| 2. | The effect of neglect of geostrophic action shall be considered in making a physical simulation for a large - scale sea area
对具有较大尺度海域的模拟需要考虑地转缺失的影响。 |
| 3. | With two - dimensional quasi - geostrophic motion , a series of numerical experiments are made to prove the theoretical results
； gj ）传统识别模式误差和奶始误差的方法，是把一系列的初始场输入到。 |
| 4. | Several regression models , with an independent variable of sea surface geostrophic current , were set up to simulate the real trajectories of drifters
对南海中伴随涡旋运动的2个浮标模拟试验显示，诸多模型中以海表地转流、风海流及背景流为自变量的回归模型模拟浮标漂流轨迹效果较好。 |
| 5. | The regimes of turbulence include homogeneous flows in two and three dimensions , geostrophic motions , shear flows , convection , boundary layers , stably stratified flows , and internal waves
扰流的形式包括二维和三维的均匀流动、因地球自转而引起的运动、切向流动、对流、边界层流、稳定层流和内部波动。 |
| 6. | Experiments on the two drifters showed that the model , with independent variables of sea surface geostrophic current , ekman drift , and mean circulation , has the best efficiency of simulating real trajectories
利用该回归模型，模拟出南海2个漂流浮标轨迹和真实轨迹距离偏差较小且二者运动趋势基本一致。 |
| 7. | Inertial instability barotropic advection of potential vorticity the subsidence of the large value of potential vorticity above cyclone and geostrophic adjustment process is dynamical factors which make the cyclone developed violently
惯性不稳定，正压位涡平流以及正压位涡大值下沉至气旋上空和地转适应过程是气旋强烈发展的动力因子。 |
| 8. | Through performing six experiments by means of a beta - plane quasi - geostrophic model and a high resolution f - plane quasi - geostrophic model , the effect of initial tangential wind profile on typhoon ' s track and intensity is examined
用一个平面的准地转模式和一个高分辨率的f平面准地转模式分析研究了不同水平廓线对台风路径和台风强度的影响。 |
| 9. | Firstly , this paper designs a polar coordinate barotropic vorticity equation semi - spectral model and a quasi - geostrophic grid model in order to research the propagation of vortex rossby waves and tropical cyclone intensity change entirely
本文首先设计了一个极坐标系正压涡度方程的半谱模式、一个准地转格点模式对涡旋rossby波传播和热带气旋强度变化进行了较为系统的研究。 |
| 10. | 2 . dynamic meteorology : equations of motion ; geostrophic , ageostrophic and gradient winds ; thickness and thermal wind ; continuity equation ; stream function ; vorticity equation ; divergence equation ; omega equation ; rossby wave ; ekman layer ; numerical weather prediction
2 .动力气象学：运动方程地转风非地转风及梯度风厚度及热成风连续方程流函数涡度方程辐散方程奥米茄方程罗斯贝波埃克曼层数值天气预报。 |
