On the Asymmetry of Wind Distribution in the Lower Layer in Typhoon
On the Asymmetry of Wind Distribution in the Lower Layer in Typhoon
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DOI：
10.2151/jmsj1965.46.3_153
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发表时间：
1968
影响因子：
3.1
通讯作者：
S. Yoshizumi
中科院分区：
文献类型：
--
作者：
S. Yoshizumi
本文讨论了圆形同心等压线型移动台风的低层风场。风暴运动的影响导致右半球的风比左半球的风大，而地面摩擦的影响增加了风暴运动造成的前后不对称。对移动台风摩擦层风场的数值估计，反映了实际观测到的非对称性特征。
The wind field in the lower layer in a moving typhoon of circular concentric isobar pattern is discussed. Effect of storm movement results in higher wind in the right semicircle than in the left, and the effect of surface friction adds front-rear asymmetry to that due to storm movement. Numerical estimation of the wind field in the friction layer of the moving typhoon depicts characteristics of actually observed asymmetry.