Bulletin of the Seismological Society of America; February 2006; v. 96; no. 1;
p. 59-68; DOI: 10.1785/0120050108
© Seismological Society of America
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Figure 3. Baseline-time plot of the Envisat orbits used in this study. The elevation
change that would produce an interferometric fringe (i.e., altitude of
ambiguity), which depends on the interferometric baseline, is given in gray
boxes. Interferograms shown in
Figure 4 are produced using the
interferometric pairs connected with bold lines.
