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Under poor computing conditions, I divided the computational grid into 1000m and resolved the seismic wave frequency to 0.05hz, but the calculated PGA is much higher than the result obtained by GMMS. What is the reason? It stands to reason that low-frequency seismic waves will not produce such a large result.
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Under poor computing conditions, I divided the computational grid into 1000m and resolved the seismic wave frequency to 0.05hz, but the calculated PGA is much higher than the result obtained by GMMS. What is the reason? It stands to reason that low-frequency seismic waves will not produce such a large result.
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