Numerical Simulation of Tornado-like Vortices Induced by Small-Scale Cyclostrophic Wind Perturbations

被引:0
作者
Liu, Yuhan [1 ]
Jiang, Yongqiang [1 ]
Chen, Chaohui [1 ]
Zhang, Yun [1 ]
He, Hongrang [2 ]
Chen, Xiong [1 ]
Zhong, Ruilin [1 ]
机构
[1] Natl Univ Def Technol, Coll Meteorol & Oceanog, Changsha 410073, Peoples R China
[2] Natl Univ Def Technol, Coll Adv Interdisciplinary Studies, Changsha 410073, Peoples R China
基金
中国国家自然科学基金;
关键词
tornado; numerical simulation; tornado-like low; small scale; SURFACE VERTICAL VORTICITY; DOPPLER RADAR OBSERVATIONS; ANTICYCLONIC TORNADOES; SUPERCELL; OKLAHOMA; WSR-88D;
D O I
10.3390/atmos16010108
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
This study introduces a tornado perturbation model utilizing the cyclostrophic wind model, implemented through a shallow-water equation framework. Four numerical experiments were conducted: a single cyclonic wind perturbation (EXP1), a single low-geopotential height perturbation (EXP2), a cyclonic wind perturbation with a 0 Coriolis parameter (EXP3), and a single anticyclonic wind perturbation (EXP4). The outputs showed that in a static atmosphere setting, a small-scale cyclonic wind perturbation generated a tornado-like pressure structure. The centrifugal force in the central area exceeded the pressure gradient force, causing air particles to flow outward, leading to a pressure drop and strong pressure gradient. The effect of the Coriolis force is negligible for meso-gamma-scale and smaller systems, while for meso-beta-scale and larger systems, it begins to have a significant impact. The results indicate that a robust cyclonic and an anticyclonic wind field can potentially generate a pair of cyclonic and anticyclonic tornadoes when the horizontal vortex tubes in an atmosphere with strong vertical wind shear tilt, forming a pair of positive and negative vorticities. These tornadoes are similar but have different rotation directions.
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页数:19
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