Radar interferometry for monitoring land subsidence and coastal change in the Nile Delta, Egypt

Show simple item record


dc.contributor Giardino , John Rick
dc.contributor Klein , Andrew George
dc.creator Aly , Mohamed Hassan
dc.date 2010 -01 -14T23 :57 :15Z
dc.date 2010 -01 -16T01 :12 :59Z
dc.date 2010 -01 -14T23 :57 :15Z
dc.date 2010 -01 -16T01 :12 :59Z
dc.date 2006 -08
dc.date 2009 -05 -15
dc.date.accessioned 2013 -03 -12T17 :52 :13Z
dc.date.available 2013 -03 -12T17 :52 :13Z
dc.date.issued 2013 -03 -12
dc.identifier http : / /hdl .handle .net /1969 .1 /ETD -TAMU -1022
dc.identifier.uri http : / /hdl .handle .net /1969 .1 /ETD -TAMU -1022
dc.description Land subsidence and coastal erosion are worldwide problems , particularly in densely populated deltas . The Nile Delta is no exception . Currently , it is undergoing land subsidence and is simultaneously experiencing retreat of its coastline . The impacts of these long -term interrelated geomorphic problems are heightened by the economic , social and historical importance of the delta to Egypt . Unfortunately , the current measures of the rates of subsidence and coastal erosion in the delta are rough estimates at best . Sustainable development of the delta requires accurate and detailed spatial and temporal measures of subsidence and coastal retreat rates . Radar interferometry is a unique remote sensing approach that can be used to map topography with 1 m vertical accuracy and measure surface deformation with 1 mm level accuracy . Radar interferometry has been employed in this dissertation to measure urban subsidence and coastal change in the Nile Delta . Synthetic Aperture Radar (SAR ) data of 5 .66 cm wavelength acquired by the European Radar Satellites (ERS -1 and ERS - 2 ) spanning eight years (1993 -2000 ) have been used in this investigation . The ERS data have been selected because the spatial and temporal coverage , as well as the short wavelength , are appropriate to measure the slow rate of subsidence in the delta . The ERS tandem coherence images are also appropriate for coastal change detection . The magnitude and pattern of subsidence are detected and measured using Permanent Scatterer interferometry . The measured rates of subsidence in greater Cairo , Mansura , and Mahala are 7 , 9 , and 5 mm yr -1 , respectively . Areas of erosion and accretion in the eastern side of the delta are detected using the ERS tandem coherence and the ERS amplitude images . The average measured rates of erosion and accretion are -9 .57 and +5 .44 m yr -1 , respectively . These measured rates pose an urgent need of regular monitoring of subsidence and coastline retreat in the delta . This study highlighted the feasibility of applying Permanent Scatterer interferometry in inappropriate environment for conventional SAR interferometry . The study addressed possibilities and limitations for successful use of SAR interferometry within the densely vegetated delta and introduced alternative strategies for further improvement of SAR interferometric measurements in the delta .
dc.format electronic
dc.format application /pdf
dc.format born digital
dc.language en _US
dc.subject Radar Interferometry
dc.subject InSAR
dc.subject Crustal Deformation
dc.subject Coastal Erosion
dc.subject Nile Delta
dc.subject Cairo
dc.subject Egypt
dc.title Radar interferometry for monitoring land subsidence and coastal change in the Nile Delta , Egypt
dc.type Book
dc.type Thesis
dc.type Electronic Dissertation
dc.type text

Citation

Radar interferometry for monitoring land subsidence and coastal change in the Nile Delta, Egypt. Available electronically from http : / /hdl .handle .net /1969 .1 /ETD -TAMU -1022 .

Files in this item

Files Size Format View

There are no files associated with this item.

This item appears in the following Collection(s)

Show simple item record

Search DSpace

Advanced Search

Browse