In this study we show how ascending and descending ERS-1/ERS-2 tandem data
can be used to generate a precise digital elevation model (DEM). In particu
lar we present the advantages, for DEM generation, of combining ascending a
nd descending interferometric data pairs with large baselines; unwrapping p
roblems caused by the high fringe rates of these data are minimized by appl
ying a flattening technique based on the use of a data pair with smaller ba
seline. The presented experiments carried out on the data of an area with s
teep topography (Etna volcano, Italy) confirm the potentiality of the propo
sed technique.