College of Surveying and GeoInformatics, Tongji University, Shanghai 200092, China; Center for Spatial Information Science and Sustainable Development Application, Tongji University, Shanghai 200092, China 在期刊界中查找 在百度中查找 在本站中查找
College of Surveying and GeoInformatics, Tongji University, Shanghai 200092, China; Center for Spatial Information Science and Sustainable Development Application, Tongji University, Shanghai 200092, China 在期刊界中查找 在百度中查找 在本站中查找
Ice surface velocity is one of the essential parameters for evaluating the mass balance and numerical simulation. In this paper, the research is mainly focused on the estimation of the ice surface velocity by combining the differential interferometry method and the multiaperture interferometry method. The twodimensional ice surface velocity of Lambert Drainage was estimated by employing the proposed method. A comparison between the estimated ice surface velocity and those obtained by using the offset tracking method and historical products was performed to analyze the dynamic characters. The results show that the proposed method is superior to the offset tracking method, and the glaciers in Lambert drainage is stable during the past 20 years.