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An Efficient Solution Method for the Buoyancy Wave Equation at Variable Wind and Temperature

机译:风和温度变化时浮力波动方程的有效求解方法

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To solve a horizontally spectral, vertically discrete buoyancy wave equation in conditions of arbitrary wind and temperature distribution with height, a novel method is applied, which consists of a presentation of the solution in the form of a cumulative product of complex decrease factors. For decrease factors, a nonlinear, inhomogeneous, two-member recurrence formula follows that is initiated, assuming the radiative condition at the top. Singularities of the wave equation, corresponding to a critical layer in the vicinity of evanescent wind, are eliminated by turbulent friction. The estimation of minimal vertical resolution is derived, enabling solution stability and accuracy. The areas of application of the developed numerical scheme are the high-precision modeling of orographic waves for arbitrary orography in general atmospheric stratification conditions and testing of adiabatic kernels of numerical weather prediction models.
机译:为了在任意风和温度分布随高度变化的条件下求解水平谱,垂直离散浮力波方程,应用了一种新颖的方法,该方法包括以复杂的折减因子的累积乘积形式表示解。对于减小因子,遵循非线性,非均质,两元递归公式,该公式假定顶部处于辐射条件。通过湍流摩擦消除了波动方程的奇异性,该奇异性对应于van逝风附近的临界层。得出最小垂直分辨率的估计值,从而实现了解决方案的稳定性和准确性。所开发的数值方案的应用领域是在一般的大气分层条件下对任意地形进行地形波的高精度建模,以及对数值天气预报模型的绝热核进行测试。

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