Results 41 to 50 of about 708,716 (215)
Advances in understanding subglacial meltwater drainage from past ice sheets
Meltwater drainage beneath ice sheets is a fundamental consideration for understanding ice–bed conditions and bed-modulated ice flow, with potential impacts on terminus behavior and ice-shelf mass balance.
Lauren M. Simkins +4 more
doaj +1 more source
Modeling the spatially distributed nature of subglacial sediment transport and erosion [PDF]
Abstract. Glaciers expel sediment as they melt, in addition to ice and water. As a result, changing glacier dynamics and melt produce changes to glacier erosion and sediment discharge, which can impact the landscape surrounding retreating glaciers, as well as communities and ecosystems downstream.
I. Delaney +3 more
openaire +3 more sources
This paper presents the results of geomorphological, geochronological and lithological investigation of a young sedimentation basin – the periglacial Lake Bretjorna (Ledovoe).
N. I. Meshcheriakov +3 more
doaj +1 more source
Technologies for retrieving sediment cores in Antarctic subglacial settings [PDF]
Accumulations of sediment beneath the Antarctic Ice Sheet contain a range of physical and chemical proxies with the potential to document changes in ice sheet history and to identify and characterize life in subglacial settings. Retrieving subglacial sediments and sediment cores presents several unique challenges to existing technologies.
Hodgson, Dominic A. +14 more
openaire +6 more sources
Subglacial sediment deformation in the Ross Sea, Antarctica
Abstract:: The Ross Sea embayment is the outlet for one-third of all Antarctic ice flow, receiving input from both East and West Antarctica. Marine-based ice streams, whose stability is susceptible to global sea-level changes, expand and contract across the Ross Sea continental shelf, eroding and deforming the substrate and transporting sediment ...
Delaney E. Robinson +3 more
openaire +2 more sources
Meltwater discharge from tidewater glaciers impacts the adjacent marine environment. Due to the global warming, tidewater glaciers are retreating and will eventually terminate on land.
Laura Halbach +23 more
doaj +1 more source
Eurasian ice-sheet dynamics and sensitivity to subglacial hydrology
Ice-stream dynamics are strongly controlled by processes taking place at the ice/bed interface where subglacial water both lubricates the base and saturates any existing, underlying sediment. Large parts of the former Eurasian ice sheet were underlain by
EYTHOR GUDLAUGSSON +5 more
doaj +1 more source
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 understood.
B. Minchew, C. Meyer
semanticscholar +1 more source
Wet-based regions of glaciers and ice sheets are now recognized to host unique and diverse microbial communities capable of influencing global biogeochemical cycles.
Moya L. Macdonald +3 more
doaj +1 more source
Laterally continuous subglacial sediments are a necessary component for ice streaming in the modern onset regions of the ice streams draining the Siple Coast of West Antarctica on the basis of new seismic data combined with previous results.
L. E. Peters +6 more
semanticscholar +1 more source

