Articles | Volume 26, issue 1
https://doi.org/10.5194/nhess-26-41-2026
https://doi.org/10.5194/nhess-26-41-2026
Research article
 | 
13 Jan 2026
Research article |  | 13 Jan 2026

The quest for reference stations at the National Observatory of Athens, Greece

Olga-Joan Ktenidou, Erion-Vasilis Pikoulis, Antonia Papageorgiou, Fevronia Gkika, Spyros Liakopoulos, Ziya Cekinmez, Panagiotis Savvaidis, Kalliopi-Elli Fragouli, Fanis Chalaris, and Christos P. Evangelidis

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Cited articles

Anderson, J. G. and Hough, S. E.: A model for the shape of the fourier amplitude spectrum of acceleration at high frequencies, B. Seismol. Soc. Am., 74, 1969–1993, https://doi.org/10.1785/BSSA0740051969, 1984. 
Ashford, S. A. and Sitar, N.: Analysis of Topographic Amplification of Inclined Shear Waves in a Steep Coastal Bluff, B. Seism. Soc. Am., 87, 692–700, https://doi.org/10.1785/BSSA0870030692, 1997. 
Borcherdt, R. D.: Effects of local geology on ground motion near San Francisco Bay, B. Seismol. Soc. Am., 60, 29–61, 1970. 
Brune, J. N.: Tectonic stress and the spectra of seismic shear waves from earthquakes, J. Geoph. Res., 75, 4997–5002, 1970. 
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Short summary
Greek seismic data are invaluable to global databases. Recordings from stations on rock (i.e. not soft deposits) are needed in seismology in order to define reference ground conditions and ground motions, which serve as the basis for all hazard calculations. However, very little knowledge exists on how rock stations in Greece behave. This is the first time the network of the National Observatory is studied systematically and multiparametrically to reveal the most adequate reference stations.
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