Volcano‐wide fringes in ERS synthetic aperture radar interferograms of Etna (1992–1998): Deformation or tropospheric effect?

By F. Beauducel, P. Briole, J. Froger. 2000

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Corrections of stratified tropospheric delays in SAR interferometry: Validation with global atmospheric models (2009, background): “Temporal variations in the vertical stratification N _ (z) lead to a delay varying with surface elevation (Delacourt et al., 1998; Beauducel et al., 2000).”
Calibration and validation of SAR interferometry for DEM generation (2002, background): “(1998); Rigo and Massonnet (1999); Beauducel et al. (2000); and Ferretti et al.”
Neutral atmospheric delay in interferometric synthetic aperture radar applications: Statistical description and mitigation (2003, background): “In a study over Mount Etna, Beauducel et al. [2000] analyze 238 interferograms to separate the effect of the neutral atmosphere from that of deformations by analyzing the correlation between pixel altitude and phase values. [4] In these studies, the contribution of the atmospheric water vapor to the”