Dynamics of Hurricanes and Tropical Storms along the Pacific Coast of Mexico: A View from a Seismic Station

V. Zobin
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Abstract

This study presents the analysis of seismic signatures generated during passage of hurricanes Newton(September 2016) and Willa (October 2018), recorded on the daily helicorders of a short-period seismic station at thedistances about 450 km from the tracks of events. This view from seismic station allowed to obtain the following results.Periods of passage of these tropical storms and hurricanes were identified. Analysis of the dynamics of sequences ofthese seismic signals allowed to separate the time intervals of increase and decrease in the development of atmosphericdisturbances. The spectral analysis of the signals of tropical storm Newton and hurricane Willa showed that the spectralamplitudes of signals, recorded during the maximum stage of activity of the tropical storm, were larger than the samefor the maximum stage of activity of the hurricane. This may be related to the presence of intensive hailstorms duringtropical storm.
墨西哥太平洋沿岸飓风和热带风暴的动力学:从地震台站观察
本研究分析了牛顿飓风(2016年9月)和威拉飓风(2018年10月)通过期间产生的地震特征,这些特征记录在距离事件轨迹约450公里的短周期地震台站的每日螺旋仪上。从地震台站的视图可以得到以下结果。这些热带风暴和飓风经过的时间被确定。对这些地震信号序列的动力学分析可以分离出大气扰动发展的增减时间间隔。对热带风暴牛顿和飓风威拉信号的频谱分析表明,在热带风暴活动最大阶段记录的信号频谱振幅大于飓风活动最大阶段的信号频谱振幅。这可能与热带风暴期间强雹暴的出现有关。
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