Abstract The area located East to Cairo, the Capital of Egypt, represents an obvious example for the rapid urban expansion, as it contains many new housing cities. Beside its socio-economic importance, it’s located in the Cairo-Suez seismic zone. We utilized Persistent Scatterer Interferometry (PSI) of 2015–2021 Sentinel-1 SAR scenes along with two GNSS stations (KATA and PHLW) to assess the distribution and rates of crustal deformation of this region. The PSI analysis is applied to 140 Sentinel-1 SAR images collected from the ascending track number (58) and the descending track number (167). The Bernese software V. 5.0 is used for the processing of the GNSS data. A good agreement between the rates estimated from the PSI analysis and GNSS data is observed. Based on results, most of the new cities showing land subsidence with variable rates. The rates at Obour, New Cairo, Shorouk, Madinty, and Capital Gardens are 0.54 ± 0.30 mm/year, 0.58 ± 0.30 mm/year, 1.01 ± 0.30 mm/year, 0.58 ± 0.30 mm/year, and 0.99 ± 0.30 mm/year, respectively. The highest recorded subsidence rates are at Asher, Administrative Capital, and Badr with 2.18 ± 0.30 mm/year, 1.89 ± 0.30 mm/year, and 1.69 ± 0.30 mm/year, respectively. Nasr city is the only city with an uplift of 0.82 ± 0.30 mm/year. Our new findings introduce the probable use of integrated techniques such as GNSS and InSAR to evaluate the extent of crustal deformation connected to rapid urbanization in arid areas. Beside tectonic setting, it should be considered while executing mega-projects for sustainable development especially within Egypt’s Vision 2030.
Read full abstract