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Contemporary ice sheet thinning drives subglacial groundwater exfiltration with potential feedbacks on glacier flow
Observations indicate that groundwater-laden sedimentary aquifers are extensive beneath
large portions of the Greenland and Antarctic ice sheets. A reduction in the mechanical …
large portions of the Greenland and Antarctic ice sheets. A reduction in the mechanical …
Worldwide version-controlled database of glacier thickness observations
Although worldwide inventories of glacier area have been coordinated internationally for
several decades, a similar effort for glacier ice thicknesses was only initiated in 2013. Here …
several decades, a similar effort for glacier ice thicknesses was only initiated in 2013. Here …
Inferring the subsurface geometry and strength of slow‐moving landslides using 3‐D velocity measurements from the NASA/JPL UAVSAR
The hazardous impact and erosive potential of slow‐moving landslides depends on
landslide properties including velocity, size, and frequency of occurrence. However …
landslide properties including velocity, size, and frequency of occurrence. However …
Glacier sliding, seismicity and sediment entrainment
The evolution of glaciers and ice sheets depends on processes in the subglacial
environment. Shear seismicity along the ice–bed interface provides a window into these …
environment. Shear seismicity along the ice–bed interface provides a window into these …
Bedforms of Thwaites Glacier, West Antarctica: Character and origin
Abstract Bedforms of Thwaites Glacier, West Antarctica both record and affect ice flow, as
shown by geophysical data and simple models. Thwaites Glacier flows across the tectonic …
shown by geophysical data and simple models. Thwaites Glacier flows across the tectonic …
Dilation of subglacial sediment governs incipient surge motion in glaciers with deformable beds
Glacier surges are quasi-periodic episodes of rapid ice flow that arise from increases in slip
rate at the ice–bed interface. The mechanisms that trigger and sustain surges are not well …
rate at the ice–bed interface. The mechanisms that trigger and sustain surges are not well …
Thermal controls on ice stream shear margins
Ice stream discharge responds to a balance between gravity, basal friction and lateral drag.
Appreciable viscous heating occurs in shear margins between ice streams and adjacent …
Appreciable viscous heating occurs in shear margins between ice streams and adjacent …
Continuous simulations over the last 40 million years with a coupled Antarctic ice sheet-sediment model
Much of the knowledge of Antarctic Ice Sheet variations since its inception~ 34 Ma derives
from marine sediments on the continental shelf, deposited in glacimarine or sub-ice …
from marine sediments on the continental shelf, deposited in glacimarine or sub-ice …