Optical matching of ASTER (Advanced Spaceborne Thermal Emission and Reflection Radiometer) satellite image pairs is used to determine the surface velocities of major glaciers across the central Karakoram. The ASTER images were acquired in 2006 and 2007, and cover a 60×120km region over Baltoro glacier, Pakistan, and areas to the north and west. The surface velocities were compared with differential global position system (GPS) data collected on Baltoro glacier in summer 2005. The ASTER measurements reveal fine details about ice dynamics in this region. For example, glaciers are found to be active over their termini even where they are very heavily debris-covered. The characteristics of several surge-type glaciers were measured, with terminus advances of several hundred meters per year and the displacement of trunk glaciers as surge glaciers pushed into them. This study is the first synthesis of glacier velocities across this region, and provides a baseline against which both past and future changes can be compared.

T-3. The MLSI cover survived intact for 55-60 years until 2005, when Ͼ690 km 2 Ottawa, Ottawa, Ontario K1N 6N5, (90%) of MLSI was lost from Yelverton Bay. Further losses occurred in 2008, and the Canada last of the Yelverton Bay MLSI was lost in August 2010. Ground penetrating radar (GPR) †Department of Geography and transects and ice cores taken in June 2009 provide the first detailed assessment of MLSI Environmental Studies, Carleton in Yelverton Inlet, and indeed the last assessment now that it has all been replaced with

No abstract

No abstract