This work was funded by the UK Natural Environment Research Council (through grants to Nienow, Mair, and Wadham, and a studentship to Bartholomew), the Edinburgh University Moss Centenary Scholarship (Cowton and Bartholomew), and a Carnegie Research Grant (Nienow). We thank Ian Willis, Tim Bartholomaus and an anonymous referee for valuable comments which significantly improved the manuscript.Peer reviewedPublisher PD
The dynamic response of the Greenland Ice Sheet (GrIS) depends on feedbacks between surface meltwate...
The Greenland Ice Sheet is losing mass at an accelerating rate due to a combination of increased sur...
Surface‐derived meltwater can access the bed of the Greenland ice sheet, causing seasonal velocity v...
Hydrology is recognised as an important component of the glacial system in alpine environments. In ...
Funding: The Scottish Alliance for Geoscience, Environment and Society (SAGES) provided financial su...
This work was funded by the UK Natural Environment Research Council (through grants to Nienow (NE/F0...
We measure hydrological parameters in meltwater draining from an outlet glacier in west Greenland to...
Coupling between runoff, hydrology, basal motion, and mass loss (“hydrology-dynamics”) is a critical...
Coupling between runoff, hydrology, basal motion, and mass loss (“hydrology-dynamics”) is a critical...
We present satellite-derived velocity patterns for the two contrasting melt seasons of 2009–10 acros...
Nienow, Sole and Cowton’s Greenland research has been supported by a number of UK NERC research gran...
We use a combination of field observations and hydrological modelling to examine the mechanisms thro...
We present satellite-derived velocity patterns for the two contrasting melt seasons of 2009–10 acros...
The purpose of this thesis is to investigate the hydrology and dynamics of a land-terminating outle...
Predictions of the Greenland Ice Sheet's response to climate change are limited in part by uncertain...
The dynamic response of the Greenland Ice Sheet (GrIS) depends on feedbacks between surface meltwate...
The Greenland Ice Sheet is losing mass at an accelerating rate due to a combination of increased sur...
Surface‐derived meltwater can access the bed of the Greenland ice sheet, causing seasonal velocity v...
Hydrology is recognised as an important component of the glacial system in alpine environments. In ...
Funding: The Scottish Alliance for Geoscience, Environment and Society (SAGES) provided financial su...
This work was funded by the UK Natural Environment Research Council (through grants to Nienow (NE/F0...
We measure hydrological parameters in meltwater draining from an outlet glacier in west Greenland to...
Coupling between runoff, hydrology, basal motion, and mass loss (“hydrology-dynamics”) is a critical...
Coupling between runoff, hydrology, basal motion, and mass loss (“hydrology-dynamics”) is a critical...
We present satellite-derived velocity patterns for the two contrasting melt seasons of 2009–10 acros...
Nienow, Sole and Cowton’s Greenland research has been supported by a number of UK NERC research gran...
We use a combination of field observations and hydrological modelling to examine the mechanisms thro...
We present satellite-derived velocity patterns for the two contrasting melt seasons of 2009–10 acros...
The purpose of this thesis is to investigate the hydrology and dynamics of a land-terminating outle...
Predictions of the Greenland Ice Sheet's response to climate change are limited in part by uncertain...
The dynamic response of the Greenland Ice Sheet (GrIS) depends on feedbacks between surface meltwate...
The Greenland Ice Sheet is losing mass at an accelerating rate due to a combination of increased sur...
Surface‐derived meltwater can access the bed of the Greenland ice sheet, causing seasonal velocity v...