Satgen330 ERS1 Volcano Monitor by GM4IHJ 22 July 95 In 1992 European Earth Resources Satellite ERS1 produced superb evidence of before/after land surface deformation caused by the Landers California earthquake of June of that year. Since then, amongst other targets, the satellite has been monitoring Mount Etna , the active volcano in the north east corner of the island of Sicily. The technique used is similar to that applied to the Landers data. Interference patterns are constructed from the differences between pairs of synthetic aperture radar (SAR) images acquired by ESR1. Separate interferograms are obtained showing changes in range to the volcano surface as the satellite tracks either, north to south , looking east on descending orbits, or south to north , looking west on ascending orbits. Descending orbits occur in daylight, ascending orbits occur at night. Only images from the same family of orbits are combined. Data quality received, suggests that night time passes give best results, perhaps because of steadier atmospheric conditions. Areas covered in vegetation and sites where ice and snow has gathered can obscure some of the data but this has not seriously affected the results. Indeed ERS1 results taken in the tropics on orbits passing the Gunung Merapi volcano on the island of Java, support the view that the rapid growth of the rich lush tropical vegetation there does not prevent the reception of good coherent image pairs. Interference due to propagation disturbance in the ionosphere and the troposphere is evident on some of the images from Mount Etna, but with the collection of increasing amounts of image data, it is now becoming possible to anticipate and recognise the effects of this natural interference, thereby avoiding false assumptions based on corrupted images. Excellent results have been obtained which show measurable deformation of the Etna volcano coincident with its recent eruption. These results are in general agreement with Navigation satellite Global Positioning system GPS measurements taken on the mountain. Readers familiar with the ominous swelling of the Mount St Helens volcano in the United States just before its explosive eruption some years ago will appreciate that SAR observation of this kind , and that used in the study of the Landers earthquake, are needed at a large number of sites around the world where there is risk from natural disasters of this kind. The recent launch of ERS2 , now operating in tandem with ERS1 will double the potential of this valuable new technique.