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Wave-activity conservation laws and stability theorems for semi-geostrophic dynamics: part 2. pseudoenergy-based theory

机译:半地转动力学的波活动守恒定律和稳定性定理:第2部分。基于伪能量的理论

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摘要

This paper represents the second part of a study of semi-geostrophic (SG) geophysical fluid dynamics. SG dynamics shares certain attractive properties with the better known and more widely used quasi-geostrophic (QG) model, but is also a good prototype for balanced models that are more accurate than QG dynamics. The development of such balanced models is an area of great current interest. The goal of the present work is to extend a central body of QG theory, concerning the evolution of disturbances to prescribed basic states, to SG dynamics. Part 1 was based on the pseudomomentum; Part 2 is based on the pseudoenergy.ududA pseudoenergy invariant is a conserved quantity, of second order in disturbance amplitude relative to a prescribed steady basic state, which is related to the time symmetry of the system. We derive such an invariant for the semi-geostrophic equations, and use it to obtain: (i) a linear stability theorem analogous to Arnol'd's ‘first theorem’; and (ii) a small-amplitude local conservation law for the invariant, obeying the group-velocity property in the WKB limit. The results are analogous to their quasi-geostrophic forms, and reduce to those forms in the limit of small Rossby number.ududThe results are derived for both the f-plane Boussinesq form of semi-geostrophic dynamics, and its extension to β-plane compressible flow by Magnusdottir & Schubert. Novel features particular to semi-geostrophic dynamics include apparently unnoticed lateral boundary stability criteria. Unlike the boundary stability criteria found in the first part of this study, however, these boundary criteria do not necessarily preclude the construction of provably stable basic states.ududThe interior semi-geostrophic dynamics has an underlying Hamiltonian structure, which guarantees that symmetries in the system correspond naturally to the system's invariants. This is an important motivation for the theoretical approach used in this study. The connection between symmetries and conservation laws is made explicit using Noether's theorem applied to the Eulerian form of the Hamiltonian description of the interior dynamics.
机译:本文代表了半地球物理(SG)地球物理流体动力学研究的第二部分。 SG动力学与更广为人知的准地转(QG)模型具有某些吸引人的特性,但它也是比QG动力学更精确的平衡模型的良好原型。这种平衡模型的开发是当前引起人们极大兴趣的领域。当前工作的目标是将QG理论的中心部分扩展到SG动力学方面,该理论涉及扰动向规定的基本状态的演变。第1部分基于伪动量;第2部分基于伪能量。 ud ud伪能量不变量是相对于规定的稳定基本状态处于扰动幅度第二级的守恒量,这与系统的时间对称性有关。我们为半地转方程推导了这样的不变量,并用它获得:(i)类似于Arnol'd的“第一定理”的线性稳定性定理; (ii)服从不变式的小幅度局部守恒定律,服从WKB限制中的群速度特性。结果类似于它们的准地转形式,并且在小Rossby数的极限内简化为这些形式。 ud ud对于半地球动力学的f平面Boussinesq形式及其对β的扩展都得到了结果。 Magnusdottir&Schubert提出的平面可压缩流。半地转动力学特有的新颖特征包括明显未被注意的横向边界稳定性准则。但是,与本研究第一部分中发现的边界稳定标准不同,这些边界标准并不一定会阻止可证明的稳定基本状态的构建。 ud ud内部半地转动力学具有潜在的哈密顿结构,从而保证了对称性系统中的自然对应于系统的不变量。这是本研究中使用的理论方法的重要动机。对称性和守恒定律之间的联系是通过将Noether定理应用于内部动力学的哈密顿量描述的欧拉形式来明确的。

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