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Numerical Study of the Influences of a Monsoon Gyre on Intensity Changes of Typhoon Chan-Hom (2015)

机译:季风回旋对台风Chan-Hom(2015)强度变化影响的数值研究

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摘要

Typhoon Chan-Hom (2015) underwent a weakening in the tropical western North Pacific (WNP) when it interacted with a monsoon gyre,but all operational forecasts failed to predict this intensity change.A recent observational study indicated that it resulted from its interaction with a monsoon gyre on the 15-30-day timescale.In this study,the results of two numerical experiments are presented to investigate the influence of the monsoon gyre on the intensity changes of Typhoon Chan-Hom (2015).The control experiment captures the main observed features of the weakening process of Chan-Hom (2015) during a sharp northward turn in the Philippine Sea,including the enlargement of the eye size,the development of strong convection on the eastern side of the monsoon gyre,and the corresponding strong outer inflow.The sensitivity experiment suggests that intensity changes of Chan-Hom (2015) were mainly associated with its interaction with the monsoon gyre.When Chan-Hom (2015) initially moved westward in the eastern part of the monsoon gyre,the monsoon gyre enhanced the inertial stability for the intensification of the typhoon.With its coalescence with the monsoon gyre,the development of the strong convection on the eastern side of the monsoon gyre prevented moisture and mass entering the inner core of Chan-Hom (2015),resulting in the collapse of the eyewall.Thus,the weakening happened in the deep tropical WNP region.The numerical simulations confirm the important effects of the interaction between tropical cyclones and monsoon gyres on tropical cyclone intensity.
机译:Chan-Hom(2015)台风在西北太平洋(WNP)与季风环流相互作用时经历了减弱,但所有运行预报均未能预测这种强度变化。最近的一项观测研究表明,它是由于与太平洋的相互作用而产生的。季风回旋在15-30天的时间尺度上。本研究通过两个数值实验的结果来研究季风回旋对台风Chan-Hom(2015)强度变化的影响。 Chan-Hom(2015)在菲律宾海向北急转期间减弱的主要观察特征,包括眼图扩大,季风回旋区东侧强对流的发展以及相应的强敏感性实验表明,Chan-Hom(2015)的强度变化主要与其与季风回旋的相互作用有关.Chan-Hom(2015)最初向西移动时在季风回旋区的东部,季风回旋区增强了台风激增的惯性稳定性。由于季风回旋区与季风回旋区汇合,在季风回旋区东侧形成了强对流,阻止了水分和物质进入Chan-Hom(2015)的内核,导致眼壁塌陷。因此,减弱作用发生在热带WNP区域。数值模拟证实了热带气旋和季风回旋对热带气旋的重要影响。强度。

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  • 来源
    《大气科学进展(英文版)》 |2018年第5期|567-579|共13页
  • 作者

    Jia LIANG; Liguang WU; Guojun GU;

  • 作者单位

    Pacific Typhoon Research Center, Key Laboratory of Meteorological Disaster, Ministry of Education, Nanjing University of Information Science and Technology, Nanjing 210044, China;

    Earth System Science Interdisciplinary Center, University of Maryland, College Park, Maryland 20740, USA;

    Pacific Typhoon Research Center, Key Laboratory of Meteorological Disaster, Ministry of Education, Nanjing University of Information Science and Technology, Nanjing 210044, China;

    State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences, Beijing 100081, China;

    Earth System Science Interdisciplinary Center, University of Maryland, College Park, Maryland 20740, USA;

  • 收录信息 中国科学引文数据库(CSCD);中国科技论文与引文数据库(CSTPCD);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
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  • 入库时间 2022-08-19 03:55:46
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