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首页> 外文期刊>ournal of the Meteorological Society of Japan >On Vortical Mesoscale Disturbances Observed During the Period of Heavy Snow or Rain in the Hokuriku District
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On Vortical Mesoscale Disturbances Observed During the Period of Heavy Snow or Rain in the Hokuriku District

机译:北陆地区大雪或暴雨期间观测到的涡旋中尺度扰动

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During the period of heavy and concentrated snow-or rainfall in the Hokuriku District, vortical mesoscale disturbances have often been observed by radar. These vortical disturbances are characterized by a diameter of about 50 to 80km, which is 100 times as large as that of tornado, and one order of magnitude smaller than that of typhoon, and may be classified as mesocyclone. Radar observations show the remarkable spiral or ring-shaped radar echoes corresponding to vortical disturbances. They usually develop off the coast. move across the plain and disappear in the mountain area of the Hokuriku District, having the lifetime of several hours. Further, it was found that the heavy and concentrated snow-or rainfalls sometimes took place along the track of these vortical disturbances, and that the intensity of precipitation may be estimated by means of wind divergence and the concept of vortical rain like the rain due to typhoon.
机译:在北陆地区,降雨或降雨集中且集中期间,经常通过雷达观测到涡旋的中尺度扰动。这些旋涡扰动的特征是直径约为50至80公里,是龙卷风直径的100倍,比台风的直径小一个数量级,可以归类为中旋风。雷达观测显示出与涡旋扰动相对应的明显的螺旋形或环形雷达回波。他们通常在沿海地区发展。穿越平原,消失在北陆地区的山区,生命长达数小时。此外,还发现有时会沿着这些涡旋扰动的轨迹发生大雪和集中降雨,并且降雨强度可以通过风的发散和涡旋雨的概念来估算,例如台风。

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