Variability in ice motion at a land-terminating Greenlandic outlet glacier: the role of channelized and distributed drainage systems

摘要

This work was funded by the UK Natural Environment Research Council (through grants to Nienow (NE/F021399/1) and Mair (NE/H024964/1)), the Edinburgh University Moss Centenary Scholarship (Cowton and Bartholomew) and a Carnegie Research Grant (Nienow). GPS equipment and training were provided by the NERC Geophysical Equipment Facility (loan 868).