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A novel method for the extraction of local gravity wave parameters from gridded three-dimensional data: description, validation, and application

机译:从网格三维数据提取局部重力波参数的新方法:描述,验证和应用

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For the local diagnosis of wave properties, we develop, validate, and apply a novel method which is based on the Hilbert transform. It is called Unified Wave Diagnostics (UWaDi). It provides the wave amplitude and three-dimensional wave number at any grid point for gridded three-dimensional data. UWaDi is validated for a synthetic test case comprising two different wave packets. In comparison with other methods, the performance of UWaDi is very good with respect to wave properties and their location. For a first practical application of UWaDi, a minor sudden stratospheric warming on 30 January 2016 is chosen. Specifying the diagnostics for hydrostatic inertia–gravity waves in analyses from the European Centre for Medium-Range Weather Forecasts, we detect the local occurrence of gravity waves throughout the middle atmosphere. The local wave characteristics are discussed in terms of vertical propagation using the diagnosed local amplitudes and wave numbers. We also note some hints on local inertia–gravity wave generation by the stratospheric jet from the detection of shallow slow waves in the vicinity of its exit region.
机译:对于局部诊断波属性,我们开发,验证,并应用基于Hilbert变换的新型方法。它被称为统一波诊断(UWADI)。它在任何网格点提供用于网格三维数据的网格点的波幅和三维波数。 UWADI被验证用于包括两个不同波包的合成测试案例。与其他方法相比,UWADI的性能对于波属性及其位置非常好。对于Uwadi的首次实际应用,选择了2016年1月30日的突然间流层变暖。指定欧洲中距离预测中心的分析中静水压惯性重力波的诊断,我们检测整个中间大气中的引力波的局部发生。在使用诊断的局部幅度和波数的垂直传播方面讨论了局部波特性。我们还注意到局部惯性 - 重力波通过平流层喷射从其出口区域附近的浅慢波检测到局部惯性重力波。

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