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dc.date.accessioned2019-02-18T11:45:40Z
dc.date.available2019-02-18T11:45:40Z
dc.date.created2018-07-18T10:49:22Z
dc.date.issued2018
dc.identifier.citationAslan, G Cakir, Ziyadin Ergintav, Semih Lasserre, Cécile Renard, Francois . Analysis of secular ground motions in istanbul from a long-term InSAR time-series (1992-2017). Remote Sensing. 2018, 10(3)
dc.identifier.urihttp://hdl.handle.net/10852/66593
dc.description.abstractThe identification and measurement of ground deformations in urban areas is of great importance for determining the vulnerable parts of the cities that are prone to geohazards, which is a crucial element of both sustainable urban planning and hazard mitigation. Interferometric synthetic aperture radar (InSAR) time series analysis is a very powerful tool for the operational mapping of ground deformation related to urban subsidence and landslide phenomena. With an analysis spanning almost 25 years of satellite radar observations, we compute an InSAR time series of data from multiple satellites (European Remote Sensing satellites ERS-1 and ERS-2, Envisat, Sentinel-1A, and its twin sensor Sentinel-1B) in order to investigate the spatial extent and rate of ground deformation in the megacity of Istanbul. By combining the various multi-track InSAR datasets (291 images in total) and analysing persistent scatterers (PS-InSAR), we present mean velocity maps of ground surface displacement in selected areas of Istanbul. We identify several sites along the terrestrial and coastal regions of Istanbul that underwent vertical ground subsidence at varying rates, from 5 ± 1.2 mm/yr to 15 ± 2.1 mm/yr. The results reveal that the most distinctive subsidence patterns are associated with both anthropogenic factors and relatively weak lithologies along the Haramirede valley in particular, where the observed subsidence is up to 10 ± 2 mm/yr. We show that subsidence has been occurring along the Ayamama river stream at a rate of up to 10 ± 1.8 mm/yr since 1992, and has also been slowing down over time following the restoration of the river and stream system. We also identify subsidence at a rate of 8 ± 1.2 mm/yr along the coastal region of Istanbul, which we associate with land reclamation, as well as a very localised subsidence at a rate of 15 ± 2.3 mm/yr starting in 2016 around one of the highest skyscrapers of Istanbul, which was built in 2010.en_US
dc.languageEN
dc.publisherMDPI AG
dc.rightsAttribution 4.0 International
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/
dc.titleAnalysis of secular ground motions in istanbul from a long-term InSAR time-series (1992-2017)en_US
dc.title.alternativeENEngelskEnglishAnalysis of secular ground motions in istanbul from a long-term InSAR time-series (1992-2017)
dc.typeJournal articleen_US
dc.creator.authorAslan, G
dc.creator.authorCakir, Ziyadin
dc.creator.authorErgintav, Semih
dc.creator.authorLasserre, Cécile
dc.creator.authorRenard, Francois
cristin.unitcode185,15,22,20
cristin.unitnameGEO Physics of Geological processes
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1
dc.identifier.cristin1597739
dc.identifier.bibliographiccitationinfo:ofi/fmt:kev:mtx:ctx&ctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Remote Sensing&rft.volume=10&rft.spage=&rft.date=2018
dc.identifier.jtitleRemote Sensing
dc.identifier.volume10
dc.identifier.issue3
dc.identifier.doihttp://dx.doi.org/10.3390/rs10030408
dc.identifier.urnURN:NBN:no-69783
dc.type.documentTidsskriftartikkelen_US
dc.type.peerreviewedPeer reviewed
dc.source.issn2072-4292
dc.identifier.fulltextFulltext https://www.duo.uio.no/bitstream/handle/10852/66593/2/2018_RemoteSensing_Aslan.pdf
dc.type.versionPublishedVersion


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