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Mechanism Study of Tropical Cyclone Impact on East Asian Subtropical Upper-Level Jet: a Numerical Case Investigation

机译:热带气旋影响东亚副热带高压喷气机的机理研究:数值案例研究

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In the case study of this paper, sensitivity experiments are carried out using the mesoscale non-hydrostatic Weather Research and Forecasting (WRF) model to investigate the impact of tropical cyclone (TC) Soudelor (2003) on the East Asian subtropical upper-level jet (EASJ) before TC Soudelor transformed into an extratropical cyclone. The physical mechanism for changes in the EASJ intensity and position caused by TC Soudelor is explored. Results indicate that TC Soudelor would warm the air in the middle and upper troposphere over the Japan Sea and the adjacent areas through stimulating northward propagating teleconnection pattern as well as releasing large amounts of latent heat, which led to increase (decrease) the meridional air temperature gradient to the south (north) below the EASJ axis. As a result, the geopotential height abnormally increased in the upper troposphere, resulting in an anomalous anticyclonic circulation belt along the EASJ axis. Correspondingly, the westerly winds to the north (south) of the EASJ axis intensified (weakened) and the EASJ axis shifted northward by one degree. The case study also suggests that before the extratropical cyclone transition of TC Soudelor, the TC activities had exerted significant impacts on the EASJ through thermodynamic processes.
机译:在本文的案例研究中,使用中尺度非静水天气研究和预报(WRF)模型进行了敏感性实验,以研究热带气旋(TC)Soudelor(TC)(2003)对东亚副热带高空急流的影响(EASJ)在TC Soudelor转变为温带气旋之前。探索了由TC Soudelor引起的EASJ强度和位置变化的物理机制。结果表明,TC Soudelor会通过刺激向北传播的遥相关型并释放大量潜热来加热日本海及对流层中高空的空气,并释放大量潜热,从而导致子午空气温度升高(降低)。在EASJ轴下方向南(北)倾斜。结果,对流层上层的地势高度异常增加,导致沿EASJ轴的反气旋环流带异常。相应地,西风向EASJ轴的北(南)风增强(减弱),并且EASJ轴向北偏移1度。案例研究还表明,在TC Soudelor的温带气旋过渡之前,TC活动通过热力学过程对EASJ产生了重大影响。

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