[HTML][HTML] Deglaciation of the Eurasian ice sheet complex
The Eurasian ice sheet complex (EISC) was the third largest ice mass during the Last
Glacial Maximum with a span of over 4500 km and responsible for around 20 m of eustatic …
Glacial Maximum with a span of over 4500 km and responsible for around 20 m of eustatic …
Modelling water flow under glaciers and ice sheets
GE Flowers - Proceedings of the Royal Society A …, 2015 - royalsocietypublishing.org
Recent observations of dynamic water systems beneath the Greenland and Antarctic ice
sheets have sparked renewed interest in modelling subglacial drainage. The foundations of …
sheets have sparked renewed interest in modelling subglacial drainage. The foundations of …
Distinct patterns of seasonal Greenland glacier velocity
T Moon, I Joughin, B Smith… - Geophysical …, 2014 - Wiley Online Library
Abstract Predicting Greenland Ice Sheet mass loss due to ice dynamics requires a complete
understanding of spatiotemporal velocity fluctuations and related control mechanisms. We …
understanding of spatiotemporal velocity fluctuations and related control mechanisms. We …
Sediment export, transient landscape response and catchment-scale connectivity following rapid climate warming and Alpine glacier recession
In the face of rapid climate warming, rapid glacier recession should lead to a marked
increase in the spatial extent of the paraglacial zone in glaciated drainage basins. The …
increase in the spatial extent of the paraglacial zone in glaciated drainage basins. The …
Efficient meltwater drainage through supraglacial streams and rivers on the southwest Greenland ice sheet
Thermally incised meltwater channels that flow each summer across melt-prone surfaces of
the Greenland ice sheet have received little direct study. We use high-resolution WorldView …
the Greenland ice sheet have received little direct study. We use high-resolution WorldView …
[HTML][HTML] Tunnel valley formation beneath deglaciating mid-latitude ice sheets: Observations and modelling
The geological record of landforms and sediments produced beneath deglaciating ice
sheets offers insights into inaccessible glacial processes. Large subglacial valleys formed …
sheets offers insights into inaccessible glacial processes. Large subglacial valleys formed …
Greenland subglacial drainage evolution regulated by weakly connected regions of the bed
Penetration of surface meltwater to the bed of the Greenland Ice Sheet each summer causes
an initial increase in ice speed due to elevated basal water pressure, followed by slowdown …
an initial increase in ice speed due to elevated basal water pressure, followed by slowdown …
[HTML][HTML] Dual-satellite (Sentinel-2 and Landsat 8) remote sensing of supraglacial lakes in Greenland
Remote sensing is commonly used to monitor supraglacial lakes on the Greenland Ice
Sheet (GrIS); however, most satellite records must trade off higher spatial resolution for …
Sheet (GrIS); however, most satellite records must trade off higher spatial resolution for …
Direct measurements of meltwater runoff on the Greenland ice sheet surface
Meltwater runoff from the Greenland ice sheet surface influences surface mass balance
(SMB), ice dynamics, and global sea level rise, but is estimated with climate models and …
(SMB), ice dynamics, and global sea level rise, but is estimated with climate models and …
Ice dynamic response to two modes of surface lake drainage on the Greenland ice sheet
Supraglacial lake drainage on the Greenland ice sheet opens surface-to-bed connections,
reduces basal friction, and temporarily increases ice flow velocities by up to an order of …
reduces basal friction, and temporarily increases ice flow velocities by up to an order of …