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Natural Frequencies of seiches in Lake Chapala

机译:恰帕拉湖塞切斯的自然频率

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摘要

This research presents an analysis of the frequencies and vibration modes of the structure of the superficial seiches of Lake Chapala using mathematical modelling and measurements. The HAMSOM model was run with wind fields from coastal meteorological stations and for different lake storage levels. The lake water level measurements were carried out in two campaigns in 2003. An analysis of the surface seiches in the lake was performed using the fast Fourier transform method. A spectral analysis of lake water level measurements reveals seiches with periods close to 5.9, 3, 2, and 1.5 h. A comparison with the periods calculated by the HAMSOM model indicates that these periods correspond to superficial seiches of the fundamental longitudinal mode of the lake and the subsequent three modes. The lake has undergone important changes in its storage level over time. Therefore, we modelled it with storage levels from the isobaths 90 to 95 m and found that surface seiche periods decreased to 5.2 h.
机译:这项研究提出了使用数学建模和测量方法对查帕拉湖浅表海峡结构的频率和振动模式进行分析。 HAMSOM模型是在沿海气象站的风场和不同湖泊存储水平下运行的。在2003年的两次活动中对湖泊水位进行了测量。使用快速傅里叶变换法对湖泊表面的色斑进行了分析。湖泊水位测量的频谱分析显示,周期接近5.9、3、2和1.5 h。与通过HAMSOM模型计算的周期的比较表明,这些周期对应于湖泊基本纵向模式及其后的三个模式的浅表生境。随着时间的推移,该湖的储水量发生了重要变化。因此,我们用等深线从90到95μm的存储水平对其进行了建模,发现地表成藏周期减少到5.2μh。

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