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辜旭赞, 赵军, 唐永兰. 2016: 三次样条函数(格式)准拉格朗日积分方案Ⅱ --样条格式非静力全可压动力框架与密度流试验. 暴雨灾害, 35(6): 566-575. DOI: 10.3969/j.issn.1004-9045.2016.06.009
引用本文: 辜旭赞, 赵军, 唐永兰. 2016: 三次样条函数(格式)准拉格朗日积分方案Ⅱ --样条格式非静力全可压动力框架与密度流试验. 暴雨灾害, 35(6): 566-575. DOI: 10.3969/j.issn.1004-9045.2016.06.009
GU Xuzan, ZHAO Jun, TANG Yonglan. 2016: A quasi-Lagrangian integration scheme with unify finite-difference scheme of cubic spline function transformation, partⅡ:non-hydrostatic and fully compressible dynamic core with spline scheme and density current test. Torrential Rain and Disasters, 35(6): 566-575. DOI: 10.3969/j.issn.1004-9045.2016.06.009
Citation: GU Xuzan, ZHAO Jun, TANG Yonglan. 2016: A quasi-Lagrangian integration scheme with unify finite-difference scheme of cubic spline function transformation, partⅡ:non-hydrostatic and fully compressible dynamic core with spline scheme and density current test. Torrential Rain and Disasters, 35(6): 566-575. DOI: 10.3969/j.issn.1004-9045.2016.06.009

三次样条函数(格式)准拉格朗日积分方案Ⅱ --样条格式非静力全可压动力框架与密度流试验

A quasi-Lagrangian integration scheme with unify finite-difference scheme of cubic spline function transformation, partⅡ:non-hydrostatic and fully compressible dynamic core with spline scheme and density current test

  • 摘要: 采用样条格式二阶时空离散预报方程与显式-准拉格朗日积分方案, 建立非静力全可压数值模式动力框架, 对气压、气温(位温)、风及广义牛顿力(加速度)场做三次样条函数拟合, 实现各个变量场二阶可导, 并且按牛顿运动定律, 显式迭代插值求上游点"三次运动"路径(三维位移)与预报变量值, 同时求得一个时间步长三维位移的平均散度场, 并以此绝热变率预报压、温场。其中, 通过对静力方程做三次样条拟合, 可从非静力气压场分离出(满足静力方程)时变的静压场, 从而无须引入大气参考廓线, 并因此准确(二阶精度)计算出垂直气压梯度力与位移。密度流试验表明, 上述非静力全可压动力框架能够模拟出高度非线性的密度流, 初步验证样条格式做"三次"数值模式动力框架的一致性和精确性, 同时分析了与密度流试验benchmark参考解相比较存在差别的原因。

     

    Abstract: In this numerical analysis, the cubic spline function consists of cubic spline, bi-cubic surface and tri-cubic (3-D cubic) cube.All three are based on the spline algorithm (spline scheme), which posses the second-order differentiable"convergence"and "optimality" of mathematical laws.With the spline scheme, a set of explicit forecast equations of second-order space-time differential remainder is derived, which brings to a quasi-Lagrangian integration scheme as well as a fully compressible dynamic core of a new nonlinear numerical model. With fitting the cubic spline functions to pressure, temperature and wind fields, and to the field of the generalized Newtonian force acting to unit air mass on rotating earth in the wind equations, which made all of them second-order differentiable, the Lagrangian particle's 3D tracks follow the second Newton's law of motion and its forecast values of the variables can be refined by an explicit, iterative procedure.Meanwhile, we may get the averaged wind divergence in one time step of the 3D paths, and it is with the implicit 3D divergence as adiabatic variability that pressure and temperature fields will be changed (forecasted).With separating time-dependent, static pressure field, which satisfies the hydrostatic equilibrium, from non-static pressure field in the model's atmosphere, and replacing the reference atmosphere profile by the static pressure field of space-time function, the non-static pressure gradient force in vertical, as well as its acting path, is rightly determined.The density current test shows that its extra nonlinear flows can be simulated in model atmosphere with such a non-hydrostatic, fully compressible dynamic core, which primarily identifies its feasibility, accuracy, scientific evaluation and our programs correctness and verifies its consistency, convergence and stability with the cubic spline functions.We further analysed the differences of density current test between the Benchmark reference solution and ours.

     

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