Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/9692
AuthorsFornaro, G.* 
Giuliani, R.* 
Noviello, C.* 
Reale, D.* 
Verde, S.* 
D’Agostino, N.* 
TitleAssimilation of GPS-Derived Atmospheric Propagation Delay in DInSAR Data Processing
Issue Date26-Jan-2014
Series/Report no.2/8 (2014)
DOI10.1109/JSTARS.2014.2364683
URIhttp://hdl.handle.net/2122/9692
KeywordsAtmospheric delay, differential SAR interfer- ometry (DInSAR), GPS, SAR interferometry (InSAR), synthetic aperture radar (SAR).
Subject Classification04. Solid Earth::04.03. Geodesy::04.03.07. Satellite geodesy 
AbstractMicrowave radiation is almost insensitive in terms of power attenuation to the presence of atmosphere; the atmo- sphere is however an error source in repeat pass interferometry due to propagation delay variations. This effect represents a main limitation in the detection and monitoring of weak deformation patterns in differential interferometric Synthetic Aperture Radar (DInSAR), especially in emergency conditions. Due to the wave- length reduction current, X-Band sensors are even more sensitive to such error sources: procedures adopted in classical advanced DInSAR for atmospheric filtering may fail in the presence of higher revisiting rates. In this work, we show such effect on data acquired by the COSMO-SkyMed constellation. The dataset has been acquired with very high revisiting rates during the emer- gency phase. This feature allows clearly showing the inability of standard filtering adopted in common processing chains in handling seasonal atmospheric delay variations over temporal intervals spanning periods shorter than 1 year. We discuss a pro- cedure for the mitigation of atmospheric propagation delay (APD) that is based on the integration of data of GPS systems which carries out measurements with large observation angles diversity practically in continuous time. The proposed algorithm allows a robust assimilation of the GPS atmospheric delay measurements in the multipass DInSAR processing and found on a linear approx- imation with the height of the atmospheric delay corresponding to a stratified atmosphere. Achieved results show a significant mitigation of the seasonal atmospheric variations.
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