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BAROTROPIC INSTABILITIES OF THE TYPE OF SELF-ORGANIZATION IN ZONAL WESTERLY FLOW

机译:区域西风中自组织类型的正压失稳

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In the paper the modern thermodynamics of processes occuring far from the equilibrium, formulated by I. PRIGOGINB and P. GLANSDORPP in, has been used for investigations of the atmospheric instabilities of the westerly zonal flow. These are instabilities of the type of self-organization. To investigate these instabilities, the method of the Lyapunov function has been applied. As the Lyapunov function the second variation of the so-called excess entropy has been assumed. In the introduction the range of most of investigations on the stability of the stationary, zonal flow is presented. It is confirmed there that investigations, which allow us to establish the threshold parameters for the zonal instabilities, were mainly performed until now. It concerns the barotropic, baroclinic and mixed instabilities of the zonal flows. In the second section the outline of the classical thermodynamics of the quasi-equilibrated processes is presented and on its background, the criteria of the local thermodynamic equilibrium and the stability of the non-equilibrated processes of arbitrary intensity are formulated. In the third section, utilising the general formulations presented in the second one, the set of conditions having the form of some constraints for the fields of perturbations are obtained. Under these conditions the production of the excess entropy in the investigated area is negative. These investigations have been performed for the barotropic zonal flow in the classical formulation. According to the interpretation resulting from the theory of information, it means the increase of the level of organization in the investigated area or the decrease of the level of its indefiniteness. This is the instability of the type of selforganization. For the investigated zonal flow the constraints for the field of velocity, its deformations and for the gradients of perturbations have been obtained. Some of them are new ones. The program of further investigations of instabilities of the type of self-organization has been formulated.
机译:在本文中,由I. PRIGOGINB和P. GLANSDORPP提出的远离平衡发生的现代过程热力学已用于研究西风纬向流的大气不稳定性。这些是自组织类型的不稳定性。为了研究这些不稳定性,已经应用了李雅普诺夫函数的方法。作为李雅普诺夫函数,假设了所谓的过剩熵的第二种变化。在引言中,介绍了大部分关于固定带状流稳定性研究的范围。可以确认的是,迄今为止,主要进行了调查工作,这些调查工作使我们能够确定区域不稳定性的阈值参数。它涉及纬向流的正压,斜压和混合不稳定性。在第二部分中,介绍了准平衡过程的经典热力学概述,并在其背景下,制定了局部热力学平衡的标准以及任意强度的非平衡过程的稳定性。在第三部分中,利用第二部分中介绍的一般公式,获得了一组条件的形式,该条件形式具有对摄动场的一些约束。在这些条件下,研究区域内过量熵的产生为负。对经典配方中的正压纬向流进行了这些研究。根据信息理论得出的解释,它意味着被调查区域中组织水平的提高或不确定性水平的降低。这是自组织类型的不稳定。对于所研究的纬向流,已经获得了对速度场,其变形和扰动梯度的约束。其中一些是新的。已经制定了进一步调查自组织类型不稳定性的程序。

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