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The degree of prevalence of similarity between outer tropical cyclone rainbands and squall lines

机译:外部热带旋风雨带和Squall线之间相似性的普遍性程度

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摘要

Tropical cyclone rainbands (TCRs) are not only one of the most striking and persistent features of tropical cyclones (TCs) but also one of the major causes for extreme floods as TCs approach or encounter the land area. TCRs have been traditionally considered as manifestations of atmospheric waves initiated near the eyewall or close to the TC center. However, the limited evidence from recent studies showed the possibility for TCRs to develop squall-line-like characteristics in the outer region of TCs. In this study, the degree of the prevalence for this similarity is explored by radar and surface observations from a large set of 50 outer TCRs associated with 22 TCs as they approached Taiwan. The results indicate that around 58% of outer TCRs are similar to squall lines. These outer TCRs are generally characterized by convective precipitation, an obvious convergence zone between the band-relative rear-to-front flow and front-to-rear flow at low levels, either frontward or rearward tilting updrafts, and a surface cold pool signature. The frequent similarity between the outer TCRs and squall lines documented provides important insights into the formation of organized, heavy precipitation associated with TCs.
机译:热带旋风雨带(TCRS)不仅是热带气旋(TCS)最引人注目和持续的特征之一,而且还是极端洪水作为TCS方法或遇到土地面积的主要原因之一。传统上,TCR被认为是在眼镜附近或靠近TC中心开始的大气波的表现。然而,来自最近研究的有限的证据表明TCR在TCS外部区域中开发Quall-Line的特征的可能性。在这项研究中,通过与22 TCS相关联的大量50个外部TCR,雷达和表面观测探讨了这种相似性的普遍性程度,因为它们接近台湾。结果表明,大约58%的外部TCR类似于Squall线。这些外部TCR通常是通过对流沉淀的特征在于,带有相对后到前流程和低水平的前后流动之间的明显会聚区,前或向后倾斜上升器和表面冷池签名。外部TCR和Squall系之间的频繁相似性提供了与与TCS相关的有组织,重沉淀的形成的重要见解。

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