具有噪声初始条件的理想斜压波生命周期实验中强大的极向喷流偏移

Felix Jäger, Philip M. Rupp, T. Birner
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引用次数: 0

摘要

摘要理想斜压波生命周期实验是研究中纬度斜压不稳定基本特性的一种广泛使用的工具。典型的生命周期是从初始的临床压不稳定射流,经过特定不稳定波型的指数增长阶段,随后在成熟阶段出现破波,在衰减阶段波浪-平均流相互作用驱动射流移位。许多作者区分了以反气旋(LC1)和气旋(LC2)波浪破碎为主的生命周期,两种类型之间的过渡通常是通过初始条件下气旋经向风切变的强度来控制的。斜压波的生长传统上是通过具有固定纬向波数的特定初始扰动触发的,而本研究通过分析随机初始扰动对生命周期演化的影响,扩展了斜压波生命周期的概念,而不依赖于任何优先的纬向依赖。我们发现,作为初始经向剪切的函数,生长阶段显示出强大的LC1-LC2区别,而在具有非单色初始扰动的所有生命周期的衰减阶段,观察到对lc1样特征的偏好。特别是,通常在LC2初始化过程中形成的持续截止气旋最终会变得不稳定,在更大的噪声扰动下,不稳定的开始会更快。无论初始剪切强度如何,所有非单色生命周期在其最终状态下都会导致向极地方向的射流移位。一致地,在成熟和衰减阶段,甚至在LC2初始化阶段,反气旋破波倾向于占主导地位。与气旋波破裂相关的赤道急流转移仍然存在,尽管纯粹是一种短暂的过渡状态。我们表明,由初始化随机波谱产生的波-波相互作用在生命周期的所有阶段都起着重要作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Robust poleward jet shifts in idealised baroclinic-wave life-cycle experiments with noisy initial conditions
Abstract. Idealised baroclinic-wave life-cycle experiments are a widely used tool to study fundamental characteristics of mid-latitude baroclinic instability. A typical life cycle evolves from an initialised baroclinically unstable jet through an exponential growth phase of a particular unstable wave mode, followed by wave breaking during the mature phase and wave–mean flow interaction driving a jet shift during the decay phase. Many authors distinguish between life cycles with predominantly anticyclonic (LC1) and cyclonic (LC2) wave breaking, and the transition between the two flavours is typically controlled via the strength of cyclonic meridional wind shear in the initial conditions. While baroclinic wave growth has traditionally been triggered via a specified initial perturbation with fixed zonal wave number, this study extends the concept of baroclinic-wave life cycles by analysing the influence of random initial perturbations without any preferred zonal dependency on the life-cycle evolution. We find that the growth phase shows a robust LC1–LC2 distinction as a function of initialised meridional shear, while a preference for LC1-like characteristics is observed during the decay phase for all life cycles with non-monochromatic initial perturbations. In particular, the persistent cut-off cyclones that typically form for LC2 initialisations are found to eventually become unstable, with the onset of instability coming sooner for larger noise perturbations. All non-monochromatic life cycles result in a poleward jet shift in their final state, regardless of the strength of the initial shear. Consistently, anticyclonic wave breaking tends to be predominant during the mature and decay phases, even for LC2 initialisations. Equatorward jet shifts associated with cyclonic wave breaking still exist, although purely as a transient interim state. We show that wave–wave interactions resulting from the initialised random wave spectrum play an important role during all phases of the life cycle.
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