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台风"烟花"路径突然北折的热动力因子诊断与分析

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台风具有较强的致灾性,我国常受其影响,因此准确预报台风路径十分重要.本文在WRF模式数值模拟的基础上,结合高空环流和基本气流的演变,对2021年第6号台风"烟花"路径突然发生近乎90°北折的原因进行深入探究.结果表明:台风"烟花"出现突然北折的原因,一是台风接近台湾岛后,在增强的西太平洋副热带高压的控制下逐渐向西移动,但受到我国中高纬地区高空长波槽的加深发展和日本附近低涡影响,台风西行受阻;二是越赤道气流的北涌,使基本气流从东北气流转为西南气流,导致台风向北偏东的移动趋势加大;三是台风中心附近环境风垂直切变出现不利于台风西行,而利于北行的条件分布(台风中心北侧出现低值区);四是最大风速水平结构出现改变,移动到更利于北移的台风中心东侧;五是不稳定能量场中低能舌出现在台风西侧,这使台风更容易向大气层结不稳定区域移动.可见,此次"烟花"台风的突然北折是多种热动力因子共同造成的.
Diagnosis and analysis of thermodynamic factors influencing the sudden northward turn of Typhoon In-Fa
Typhoons can cause significant damage,and accurate forecasting of their paths is crucial for mitigating their impact.This study investigates the sudden northward turn of Typhoon In-Fa(2021),which veered nearly 90 degrees northward,using the WRF model to perform accurate numerical simulations combined with analyses of upper atmospheric circulation and basic airflow patterns.The findings indicate that the northward turn of Typhoon In-Fa was driven by several key factors:1)As Typhoon In-Fa approached Taiwan,its track shifted northward due to the strengthening and westward expansion of the western pacific Subtropical high,combined with the deepening of the upper-level long-wave trough over China and the blocking influence of a low-pressure vortex near Japan,which prevented further westward movement.Concurrently,the northward surge of cross-equatorial flow altered the basic airflow from a northeasterly to a southwesterly direction,enhancing the northward movement trend.2)The continuous eastward shift of the mid-latitude longwave trough over China and the eastward retreat of the sub-tropical high led to the formation of a significant positive potential vorticity center north of the center of Typhoon In-Fa,accompanied by counterclockwise positive potential vorticity advection on the northwest side of the center.This altered the structure of the potential vorticity field near the typhoon center,slowing its westward trajectory and steering it northward.3)The vertical shear of the ambient wind near the typhoon center was unfavorable for westward movement but facilitated northward movement due to the distribution of high and low values,with lower values north of the typhoon center.4)Both simulation experiments indicated persistent wind speed asymme-try around the typhoon center,with the 500 hPa wind speed maximum shifting from the west to the east side of the typhoon center.The presence of southerly winds on the right side of the typhoon increased the northward com-ponent of its movement,significantly contributing to its abrupt northward turn.5)In the unstable energy field,a low-energy tongue developed on the west side of the typhoon,promoting movement into the unstable atmospheric junction region.These findings highlight that the sudden northward turn of Typhoon In-Fa was driven by a combi-nation of thermodynamic factors,providing valuable insights for improving typhoon track forecasts.

Typhoon In-Fanorthward track shiftnumerical simulationdiagnostic analysis

罗斐然、闵锦忠

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南京信息工程大学大气科学学院,江苏南京 210044

台风"烟花" 路径北折 数值模拟 诊断分析

国家自然科学基金重大项目

42192553

2024

大气科学学报
南京信息工程大学

大气科学学报

CSTPCD北大核心
影响因子:1.558
ISSN:1674-7097
年,卷(期):2024.47(5)