Abstract
The settlement of Larissa in the eastern part of Central Greece suffers from continued land deformation as evidenced by ground fissures, sinkholes and subsidence. We used three different interferometric synthetic aperture radar (InSAR) techniques to monitor ground deformation dynamics in the study area. Spatial patterns of short-term changes (35 days) were studied using conventional InSAR, longer-term changes (13 years) by interferometric stacking, and change dynamics of single objects was assessed by permanent scatterer technique. The results indicate co-occurring subsidence and uplift processes in the region with their average annual change rates reaching up to −2.9 and 6.6 mm a−1, respectively. Some of these changes may be attributed to tectonic fault movements, but there are also other mechanisms of continued ground deformation in the region, particularly the swelling and shrinking of expansive soils and human-induced changes in the groundwater level.
Similar content being viewed by others
References
Bürgmann R, Rosen PA, Fielding EJ (2000) Synthetic aperture radar interferometry to measure Earth’s surface topography and its deformation. Annu Rev Earth Planet Sci 28(1):169–209
Caputo R (1993) The rodia fault system; an active complex share zone (Larissa Plain, Central Greece). Bull Geol Soc Xxviii(1):447–456
Caputo R, Helly B (2005) The holocene activity of the Rodi`a fault central Greece. Geodynamics, Osa/vuosikerta 40:153–169
Caputo R, Pavlides S (1993) Late Cainozoic geodynamic evolution of thessaly and surroundings (Central-Northern Greece). J Geodyn 223(3):339–362
Caputo R, Bravard J-P, Helly B (1994) The pliocene-quaternary tecto-sedimentary evolution of the Larissa plain (Eastern Thessaly Greece). Geodin Acta 7:57–85
Caputo R, Helly B, Pavlides S, Papadopoulos G (2004) Palaeoseismological investigation of the tyrnavos fault (Thessaly, Central Greece). Tectonophysics 394:1–20
Caputo R, Helly B, Pavlides S, Papadopoulos G (2006) Archaeo- and palaeoseismological investigations in Northern Thessaly (Greece): insights for the seismic potential of the region. Nat Hazards 39:195–212
Caputo R, Hinzen K-G, Liberatore D, Schreiber S, Helly B, Tziafalias A (2011) Quantitative archaeoseismological investigation of the great theatre of Larissa, Greece. Bull Earthq Eng 9:347–366
Chen Y, Zhang G, Ding X, Li Z (2000) Monitoring earth surface deformations with InSAR technology: principles and some critical issues. J Geospatial Eng 2(1):3–21
Ding XL, Li ZW, Zhu JJ, Feng GC, Long JP (2008) Atmospheric effects on InSAR measurements and their mitigation. Sensors 8:5426–5448
Ferretti A, Prati C, Rocca F (2001) Permanent scatterers in SAR interferometry. IEEE Trans Geosci Remote Sens 39(1):8–20
Gamma Remote Sensing (2008) Documentation—user’s guide, differential inteferometry and geocoding software—Diff&Geo. 1.2 ed Worbstrasse 255, Ch -3073 ed. Gumligen, Switzerland: Gamma Remote Sensing Ag
Ganas A, Salvi S, Atzori S, Tolomei C (2006) Ground deformation in Thessaly, Central Greece, retrieved from differential interferometric analysis of ERS-SAR data. 11th international symposium on natural and human induced hazards & 2nd workshop on Earthquake Prediction Abstract Volume, June 22–25, 2006, Patras, Greece, p 41
Hooper A, Zebker H, Segall P, Kampes B, (2004) A new method for measuring deformation on volcanoes and other natural terrains using InSAR persistent scatterers. Geophys Res Lett 31(23):L23611–L23611
Hooper A, Segall P, Zebker H (2007) Persistent scatterer interferometric synthetic aperture radar for crustal deformation analysis, with application to Volcán Alcedo, Galápagos. J Geophys Res Solid Earth 112(B7):1978–2012
Kontogianni V, Pytharouli S, Stiros S (2007) Ground subsidence, quaternary faults and vulnerability of utilities and transportation networks in Thessaly. Environ Geol 52(6):1085–1095
LPDAAC (2010) Land processes distribution active archive center. [Online]. https://lpdaac.usgs.gov/products/measures_products_table. Accessed Mar 2010
Malinverni ES, Sandwell DT, Tassetti AN, Cappelletti L (2014) InSAR decorrelation to assess and prevent volcanic risk. Eur J Remote Sens 47:537–556
Massonnet D, Feigl KL (1998) Radar interferometry and its application to changes in the Earth’s surface. Rev Geophys 36(4):441–500
Mokhtari M, Dehghani M (2012) Swell-shrink behavior of expansive soils, damage and control. Electron J Geotech Eng 17:2673–2682
Papathanassiou G, Christaras B (2008) Geo-engineering assessment of liquefaction hazard of the town of Larissa, Central Greece. In: Madrid, Spain, Ii European conference of IAEG, cities and their underground environment
Parcharidis I, Foumelis M, Katsafados P (2011) Seasonal ground deformation monitoring over southern larissa plain (Central Greece) by SAR interferometry. Environ Earth Sci 2:497–504
Pavlides S, Kouskouna V, Ganas A, Caputo R, Karastathis V, Sokos E, (2004) The Gonnoi (NE Thessaly–Greece) earthquake (June 2003, Ms = 5.5) and the neotectonic regime of Lower Olympus. In: 5th international symposium on eastern Mediterranean geology Thessaloniki, Greece, 14–20 April 2004
Prati C, Ferretti A, Perissin D (2010) Recent advances on surface ground deformation measurement by means of repeated space-borne SAR observations. J Geodyn 49(3):161–170
Rozos D, Sideri D, Loupasakis C, Apostolidis E. (2010) Land subsidence due to excessive groundwater withdrawal. a case study from stavros—Farsala site, west Thessaly. Patras Greece. In: 12th international congress. Greece, bulletin of the geological society of Greece
Salvi S, Ganas A, Stramondo S, Atzori S, Tolomei C, Pepe A, Manzo M, Casu F, Berardino P, Lanari R (2004) Monitoring long-term ground deformation by SAR interferometry: examples from the Abruzzi, Central Italy, and Thessaly, Greece, paper presented at the 5th international symposium on eastern mediterranean geology, Thessaloniki, Greece, 14–20 April, 2004, Reference,T7–17
Scharoo R, Visser P (1998) Precise orbit determination and gravity field improvement for the ERS satellites. J Geophys Res 103:8113–8127
Sgouras I (1994) Relationship of calcareous geological substrate with the properties of overburden soil. s.l.: department of land improvement and agricultural engineering. Agricultural University of Athens PhD thesis
Smith LC (2002) Emerging applications of interferometric synthetic aperture radar (InSAR) in geomorphology and hydrology. Ann As Am Geogr 92(3):385–398
Vassilopoulou S, Sakkas V, Wegmuller U, Capes R (2013) long term and seasonal ground deformation monitoring of Larissa plain (Central Greece) by persistent scattering interferometry. Cent Eur J Geosci 5(1):61–76
Wang GY, You G, Shi B, Yu J, Li HY, Zong KH (2009) Earth fissures triggered by groundwater withdrawal and coupled by geological structures in Jiangsu Province, China. Environ Geol 57:1047–1054
Wegmüller U, Werner C, Strozzi T, Wiesmann A (2006) Application of SAR interferometric techniques for surface deformation monitoring. Baden, 3rd IAG/12th FIG symposium
Wegmόller, U., 2005. Gamma IPTA processing example Luxemburg gamma technical report 9-Nov., s.l.: GAMMA remote sensing http://www.gamma-rs.ch/
Zhang, Y. & Cheng, X., 2005. Application of SRTM-DEM based two-pass SAR interferometry for detecting seismic deformation on high-altitude rugged terrain—A case study in Kokoxili Ms 8.1 Earthquake. s.l., Igarss
Acknowledgments
The authors would like to acknowledge the European Space Agency (ESA) for providing the ERS_1/2, ENVISAT ASAR data. We also acknowledge Mr. Issaak Parcharidis for his comments and suggestions significantly improved an earlier version of this manuscript.
Author information
Authors and Affiliations
Corresponding author
Additional information
Falah Fakhri awarded PhD from Harokopio University of Athens
Rights and permissions
About this article
Cite this article
Fakhri, F., Kalliola, R. Monitoring ground deformation in the settlement of Larissa in Central Greece by implementing SAR interferometry. Nat Hazards 78, 1429–1445 (2015). https://doi.org/10.1007/s11069-015-1779-6
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s11069-015-1779-6