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• W2790028531 abstract "Due to fluctuations in the thickness of the permafrost active layer, there exists a seasonal seismic impedance contrast in the permafrost table. The horizontal-to-vertical spectral ratio (HVSR) method is commonly used to estimate the resonant frequency of sedimentary layers on top of bedrock. Results obtained using this method are thought to be stable in time. The aim of the study is to verify whether seasonal variability in the permafrost active layer influences the results of the HVSR method. The research area lies in the direct vicinity of the Polish Polar Station, Hornsund, which is located in Southern Spitsbergen, Svalbard. Velocity models of the subsurface are obtained using the HVSR method, which are juxtaposed with electrical resistivity tomography profiles conducted near the seismic station. Survey results indicate that the active layer of permafrost has a major influence on the high-frequency section of the HVSR results. In addition, the depth of the permafrost table inferred using the HVSR method is comparable to the depth visible in electrical resistivity tomography results. This study proves that, in certain conditions, the HVSR method results vary seasonally, which must be taken into account in their interpretation." @default.
• W2790028531 created "2018-03-29" @default.
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• W2790028531 date "2018-03-23" @default.
• W2790028531 modified "2023-10-18" @default.
• W2790028531 title "Horizontal-to-vertical spectral ratio variability in the presence of permafrost" @default.
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• W2790028531 doi "https://doi.org/10.1093/gji/ggy118" @default.
• W2790028531 hasPublicationYear "2018" @default.
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