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1、4、时间的显隐，时间层数显式差分格式和隐式差分格式迎风格式（时间向前差，空间 向后差）数学上不喜欢用这种格式,精 度不高,但物理上它的物理意 义明确（当U0时）蛙跳格式（跳背格式） 时间、空间均为中央差显式、三时间层 差分格式 时间 、空间均为二阶精度隐式差分格式没有明显的计算方程来计算出初边值问题 n迎风格式（二时间层）n蛙跳格式（三时间层）则则所有时时刻能解已知还还需要另一时间时间 层层的数据。 相容性 Consistency n要求差分系统和微分系统相协调。如果有这一 条件不被满足，该差分格式绝不能模拟我们研 究的初值问题。我们可以说这个条件是基本的 ，如果它被满足了，我们才有必要详细的
2、研究 差分格式。n相容性条件：主要是要求在小的时间步长和小 的空间格距趋于零的极限条件下，差分方程应 等同于微分方程。n相容性条件的英文表述：nThe consistency: nwhen nthe FDE concides with PDE.收敛性convergence 设设差分方程的解为为微分方程的解为为如果时，则则称：差分方程的解收敛敛到.差分算子收敛敛到微分算子叫相容 ，收敛到而收敛是指稳定性 n差分近似的稳定性是指对于任意给定的初值， 当n无限增大时，任意时刻的数值是否有界的 问题。假如数值解是稳定有界的，则相应的数 值格式称为稳定的格式。n计算稳定性的分析方法：n 冯纽曼方法（Vo
3、n-Neumann方法，又称谐 波分析法）：通过测试差分格式近似解一个谐 波分量的稳定性，研究差分格式的稳定性。拉克斯（LAX）等价定理n对于一个适定的初值问题和它的一个具有相容性的差分格式，收 敛性的充分必要条件是其稳定性。n或者:如果差分格式是相容的,那么差分格式稳定等价于收敛。n或者:如果差分格式是相容的,那么差分解收敛的充要条件是差分 格式是稳定的。n其英文是:LAX theoremn Given a properly posed linear initial value problem, and a finite difference scheme that satisfies th
4、e consistency condition, then the stability of the FDE is the necessary and sufficient condition for convergence.CFL判据n对于迎风差分格式n称为线性稳定性判据,又称CFL判据 (Courant, Friedrichs和Lewyt)，中文常说成库朗判据。nCFL condition is a necessary condition for stability, but not sufficient.五、数值天气预报的概念和历 史回顾 nnumerical weather predi
5、ction uses numerical methods to approximate a set of partially differential equations on discrete grid points in a finite area to predict the weather systems and processes in a finite area for a certain time in the future. nIn order to numerically integrate the partial differential equations, which
6、govern the atmospheric motions and processes, with time, one needs to start the integration at certain time. An initial- and boundary- value problemnIn order to do so, the meteorological variables need to be prescribed at this initial time, which are called initial conditions. Mathematically, this c
7、orresponds to solve an initial-value problem. nDue to practical limitations, such as computing power, numerical methods, etc., we are forced to make the numerical integration for predicting weather systems in a finite area. In order to do so, it is necessary to specify the meteorological variables a
8、t the boundaries, which include upper, lower, and lateral boundaries, of the domain of interest. Mathematically, this corresponds to solve a boundary-value problem. nThus, mathematically, numerical weather prediction is equivalent to solving an initial- and boundary- value problem. An initial- and b
9、oundary- value problemThe accuracy of the numerical weather predictionndepends on the accuracies of the initial conditions and boundary conditions. n The more accurate these conditions, the more accurate the predicted weather systems and processes. nthe lack of sufficient and accurate initial condit
10、ions, as well as more accurate and sufficient boundary conditions and appropriate ways in implementing them at the lateral boundaries of a finite domain of interest. nwe do not have enough observed data over the oceans and polar regions. nSome unconventional data, such as those retrieved from radar
11、and satellite observations, have been used to help supply the data in data-void regions. nImprovement of global numerical weather predition model is also important in improving the accuracy of the regional numerical weather prediction model since the former are often used to provide the initial and
12、boundary conditions for the latter. The inaccuracy of numerical weather prediction nthe numerical approximation of the partial differential equations governing atmospheric motions on the discrete points of a model domainnand the representation of the weather phenomena and processes occurred within g
13、rid points of a numerical model, i.e. the parameterization of subgrid-scale weather phenomena and processes. The accuracy of a numerical methodncan be improved by adopting a higher-order approximation of the partial differential equations used in the numerical weather prediction models, as well as u
14、sing a more accurate, but stable approximation methods. nThese require an increase of computing power as well as better understanding of numerical approximation methods.nThe accuracy of subgrid-scale parameterizations can be improved by a better understanding of the weather phenomena and processes a
15、s well as reducing the grid interval of a numerical weather prediction model. Another challenge of numerical weather predictionnAnother challenge of numerical weather prediction is whether the weather systems are predictable or not. n If they are intrinsically unpredictable, then the improvements in
16、 more accurate initial and boundary conditions, numerical methods, and subgrid-scale parameterizations of a numerical weather prediction will have its limitations. nThe weather systems are considered to have limited predictability. The early history of Numerical Weather PredictionnThe roots of numerical weather prediction can be traced back to the work of Vilhelm Bjerknes, a Norwegian physicist who has been called
