Ice sheet motion in inland Antarctica from JERS-1 sar interferometry

説明

From a series of three JERS-1 SAR interferograms over the Yamato mountains area in the Antarctica, ice surface movement is detected. In spite of less accurate orbit information, baselines are estimated using 1 km global DEM and referring phases over bare rock areas. The Detected movement fields from three interferograms resemble, but different subtly

収録刊行物

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