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Simulated convective lines with parallel stratiform precipitation. Part II: Governing dynamics and associated sensitivities

机译:具有平行层状降水的模拟对流线。第二部分:治理动态和相关的敏感性

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This article is the second of two describing convective lines with parallel stratiform ( PS) precipitation. The PS mode appears to be the preferred organizational structure in environments with line-parallel vertical wind shear. This paper presents a detailed analysis of the processes that lead to the development of the PS structure within line-parallel shear, and the positive and negative feedbacks associated with the mature PS structure. As well, the particular importance of line-perpendicular and line-parallel wind shear, line-end effects, inertial stability, and patterns of convective initiation are investigated through a battery of sensitivity tests. Convective lines with PS precipitation develop in environments with both significant line-perpendicular and line-parallel vertical wind shear. Although the studied environments are initially supportive of supercells, the merging of outflows soon renders a predominant linear forcing and the characteristic PS structure. The systems' linearity in the presence of along-line wind shear makes the local wind field more dependent upon the mesoscale structure of the convective system. For example, the along-line transport of hydrometeors is required for the development of a line-parallel precipitation region, and yet this transport does not occur immediately down the convective line's axis because it is interrupted by the pressure maxima associated with other convective cells that are farther down the line. However, the along-line flow within the line's leading and trailing anvils is able to contribute substantially because there are along-line pressure gradient accelerations associated with the tilted mesoscale structure of the system's buoyancy field. This paper concludes the study by synthesizing its dynamical and sensitivity analyses with the overarching structures described in the companion article, yielding perhaps the first consolidated view of these little-studied systems.
机译:本文是描述两条平行层状降水的对流线的第二篇。在具有平行线垂直风切变的环境中,PS模式似乎是首选的组织结构。本文介绍了导致线平行剪切内PS结构发展的过程的详细分析,以及与成熟PS结构相关的正反馈和负反馈。同样,通过一系列的敏感性测试来研究线垂直和线平行风切变,线端效应,惯性稳定性和对流启动方式的特殊重要性。 PS降水的对流线在垂直线和垂直风切变很大的环境中发展。尽管所研究的环境最初支持超级细胞,但流出的合并很快提供了主要的线性强迫和特征性PS结构。在存在沿线风切变的情况下,系统的线性度使局部风场更依赖于对流系统的中尺度结构。例如,为了形成一条线平行的降水区域,就需要沿水线方向进行输运,但是这种输运不会立即沿着对流线的轴向下发生,因为它被与其他对流单元相关的最大压力所中断。更远的地方。然而,由于存在与系统浮力场的倾斜的中尺度结构相关的沿线压力梯度加速度,因此线的前砧和尾砧内的沿线流动能够做出实质性贡献。本文通过将其动力学和灵敏度分析与随附文章中描述的总体结构进行综合来结束本研究,从而得出这些鲜为研究的系统的第一个综合观点。

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