Geomorphology under ice streams: moving from form to process
CR Stokes - Earth Surface Processes and Landforms, 2018 - Wiley Online Library
Ice streams are integral components of an ice sheet's mass balance and directly impact on
sea level. Their flow is governed by processes at the ice‐bed interface which create …
sea level. Their flow is governed by processes at the ice‐bed interface which create …
Subglacial water storage and drainage beneath the Fennoscandian and Barents Sea ice sheets
Subglacial hydrology modulates how ice sheets flow, respond to climate, and deliver
meltwater, sediment and nutrients to proglacial and marine environments. Here, we …
meltwater, sediment and nutrients to proglacial and marine environments. Here, we …
[HTML][HTML] Do subglacial bedforms comprise a size and shape continuum?
Understanding the evolution of the ice-bed interface is fundamentally important for gaining
insight into the dynamics of ice masses and how subglacial landforms are created. However …
insight into the dynamics of ice masses and how subglacial landforms are created. However …
Multisystem synthesis of radar sounding observations of the Amundsen Sea sector from the 2004–2005 field season
Abstract The Amundsen Sea Embayment of the West Antarctic Ice Sheet contains Thwaites
and Pine Island Glaciers, two of the most rapidly changing glaciers in Antarctica. To date …
and Pine Island Glaciers, two of the most rapidly changing glaciers in Antarctica. To date …
The kinematic significance of subglacial bedforms and their use in palaeo-glaciological reconstructions
Subglacial bedforms are relevant geomorphic markers for palaeo-glaciological
reconstructions. Due to the complexity of thermomechanical interactions between ice, till and …
reconstructions. Due to the complexity of thermomechanical interactions between ice, till and …
Subglacial bed form morphology controlled by ice speed and sediment thickness
Subglacial bed forms (drumlins, ribbed moraines, and megascale glacial lineations) are
enigmatic repetitive flow‐parallel and flow‐transverse landforms common in glaciated …
enigmatic repetitive flow‐parallel and flow‐transverse landforms common in glaciated …
Ice streams of the Late Wisconsin Cordilleran Ice Sheet in western North America
Abstract The Late Wisconsin Cordilleran Ice Sheet (CIS) of western North America is thought
to have reached its maximum extent (∼ 2.5× 10 6 km 2) as late at c. 14.5 ka. Most (80%) of …
to have reached its maximum extent (∼ 2.5× 10 6 km 2) as late at c. 14.5 ka. Most (80%) of …
Conceptual model for the formation of bedforms along subglacial meltwater corridors (SMCs) by variable ice‐water‐bed interactions
Subglacial meltwater landforms found on palaeo‐ice sheet beds allow the properties of
meltwater drainage to be reconstructed, informing our understanding of modern‐day …
meltwater drainage to be reconstructed, informing our understanding of modern‐day …
Patterns of ice recession and ice stream activity for the MIS 2 Laurentide Ice Sheet in Manitoba, Canada
Reconstruction of deglacial ice margins provides insights into the demise of past ice sheets
and ice‐marginal lakes and helps to understand how former ice sheets responded to climate …
and ice‐marginal lakes and helps to understand how former ice sheets responded to climate …
[HTML][HTML] Formation of ribbed bedforms below shear margins and lobes of palaeo-ice streams
Conceptual ice stream land systems derived from geomorphological and sedimentological
observations provide constraints on ice–meltwater–till–bedrock interactions on palaeo-ice …
observations provide constraints on ice–meltwater–till–bedrock interactions on palaeo-ice …