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Determination of periodic deformation from InSAR results using the FFT time series analysis method in Gediz Graben

Permanent Scatterers (PS) point velocities obtained by the interferometric synthetic aperture radar (InSAR) method are generally determined using the linear regression model, which ignores periodic and seasonal effects. In this study, software was developed that can detect periodic effects by applyi...

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Autores principales: Hastaoglu, K. O., Poyraz, F., Erdogan, H., Tiryakioglu, İ., Ozkaymak, C., Duman, H., Gül, Y., Guler, S., Dogan, A., Gul, Y.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Springer Netherlands 2023
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9942630/
https://www.ncbi.nlm.nih.gov/pubmed/36846809
http://dx.doi.org/10.1007/s11069-023-05870-w
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author Hastaoglu, K. O.
Poyraz, F.
Erdogan, H.
Tiryakioglu, İ.
Ozkaymak, C.
Duman, H.
Gül, Y.
Guler, S.
Dogan, A.
Gul, Y.
author_facet Hastaoglu, K. O.
Poyraz, F.
Erdogan, H.
Tiryakioglu, İ.
Ozkaymak, C.
Duman, H.
Gül, Y.
Guler, S.
Dogan, A.
Gul, Y.
author_sort Hastaoglu, K. O.
collection PubMed
description Permanent Scatterers (PS) point velocities obtained by the interferometric synthetic aperture radar (InSAR) method are generally determined using the linear regression model, which ignores periodic and seasonal effects. In this study, software was developed that can detect periodic effects by applying fast Fourier transformation (FFT) time series analysis to InSAR results. Using the FFT time series analysis, the periodic components of the surface movements at the PS points were determined, and then the annual velocity values free from periodic effects were obtained. The study area was chosen as the Gediz Graben, a tectonically active region where aseismic surface deformations have been observed in recent years. As a result, using the developed method, seasonal effects were successfully determined with the InSAR method at the PS points in the study area with a period of 384 days and an average amplitude of 19 mm. In addition, groundwater level changes of a water well in the region were modeled, and 0.93 correlation coefficient values were calculated between seasonal InSAR displacement values and water level changes. Thus, using the developed methodology, the relationship between the tectonic movement in the Gediz Graben in Turkey and the seasonal movements and the change in the groundwater level was determined.
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spelling pubmed-99426302023-02-22 Determination of periodic deformation from InSAR results using the FFT time series analysis method in Gediz Graben Hastaoglu, K. O. Poyraz, F. Erdogan, H. Tiryakioglu, İ. Ozkaymak, C. Duman, H. Gül, Y. Guler, S. Dogan, A. Gul, Y. Nat Hazards (Dordr) Original Paper Permanent Scatterers (PS) point velocities obtained by the interferometric synthetic aperture radar (InSAR) method are generally determined using the linear regression model, which ignores periodic and seasonal effects. In this study, software was developed that can detect periodic effects by applying fast Fourier transformation (FFT) time series analysis to InSAR results. Using the FFT time series analysis, the periodic components of the surface movements at the PS points were determined, and then the annual velocity values free from periodic effects were obtained. The study area was chosen as the Gediz Graben, a tectonically active region where aseismic surface deformations have been observed in recent years. As a result, using the developed method, seasonal effects were successfully determined with the InSAR method at the PS points in the study area with a period of 384 days and an average amplitude of 19 mm. In addition, groundwater level changes of a water well in the region were modeled, and 0.93 correlation coefficient values were calculated between seasonal InSAR displacement values and water level changes. Thus, using the developed methodology, the relationship between the tectonic movement in the Gediz Graben in Turkey and the seasonal movements and the change in the groundwater level was determined. Springer Netherlands 2023-02-21 2023 /pmc/articles/PMC9942630/ /pubmed/36846809 http://dx.doi.org/10.1007/s11069-023-05870-w Text en © The Author(s), under exclusive licence to Springer Nature B.V. 2023, Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. This article is made available via the PMC Open Access Subset for unrestricted research re-use and secondary analysis in any form or by any means with acknowledgement of the original source. These permissions are granted for the duration of the World Health Organization (WHO) declaration of COVID-19 as a global pandemic.
spellingShingle Original Paper
Hastaoglu, K. O.
Poyraz, F.
Erdogan, H.
Tiryakioglu, İ.
Ozkaymak, C.
Duman, H.
Gül, Y.
Guler, S.
Dogan, A.
Gul, Y.
Determination of periodic deformation from InSAR results using the FFT time series analysis method in Gediz Graben
title Determination of periodic deformation from InSAR results using the FFT time series analysis method in Gediz Graben
title_full Determination of periodic deformation from InSAR results using the FFT time series analysis method in Gediz Graben
title_fullStr Determination of periodic deformation from InSAR results using the FFT time series analysis method in Gediz Graben
title_full_unstemmed Determination of periodic deformation from InSAR results using the FFT time series analysis method in Gediz Graben
title_short Determination of periodic deformation from InSAR results using the FFT time series analysis method in Gediz Graben
title_sort determination of periodic deformation from insar results using the fft time series analysis method in gediz graben
topic Original Paper
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9942630/
https://www.ncbi.nlm.nih.gov/pubmed/36846809
http://dx.doi.org/10.1007/s11069-023-05870-w
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