Results 51 to 60 of about 5,299 (206)

Quantifying Antarctic‐Wide Ice‐Shelf Surface Melt Volume Using Microwave and Firn Model Data: 1980 to 2021

open access: yesGeophysical Research Letters, 2023
Antarctic ice‐shelf stability is threatened by surface melt, which has been implicated in several ice‐shelf collapse events over recent decades. Here, we first analyze cumulative days of wet snow/ice status (“melt days”) for melt seasons from 1980 to ...
Alison F. Banwell   +3 more
doaj   +1 more source

Vulnerable Antarctic ice shelves

open access: yesNature Climate Change, 2016
Standfirst: The decay of floating ice shelves around Antarctica speeds up ice flow from the continent and enhances sea-level rise. Now meltwater attributed to warm winds has been discovered on an East Antarctic ice shelf, suggesting greater vulnerability than previously thought.
openaire   +3 more sources

Basal channels on ice shelves [PDF]

open access: yesJournal of Geophysical Research: Earth Surface, 2013
Recent surveys of floating ice shelves associated with Pine Island Glacier (Antarctica) and Petermann Glacier (Greenland) indicate that there are channels incised upward into their bottoms that may serve as the conduits of meltwater outflow from the sub‐ice‐shelf cavity.
openaire   +1 more source

Overview of areal changes of the ice shelves on the Antarctic Peninsula over the past 50 years [PDF]

open access: yesThe Cryosphere, 2010
In recent decades, seven out of twelve ice shelves around the Antarctic Peninsula (AP) have either retreated significantly or have been almost entirely lost. At least some of these retreats have been shown to be unusual within the context of the Holocene
A. J. Cook, D. G. Vaughan
doaj  

A Simplified Three-Dimensional Ice-Sheet Model Including Ice Shelves [PDF]

open access: yesAnnals of Glaciology, 1990
We present a simplified numerical three-dimensional ice-sheet/ice-shelf model with a coarse horizontal resolution (100 km), designed for simulations of ice-volume changes on ice-age time scales (100 000 years and longer). The ice-sheet part uses the shallow-ice approximation to determine the flow, and includes a three-dimensional temperature ...
Böhmer, W., Herterich, K.
openaire   +2 more sources

Evolution of supraglacial lakes over the pan-Antarctic ice sheet between 2014 and 2022: Assessment and the control factors

open access: yesAdvances in Climate Change Research
Widespread supraglacial lakes (SGLs) across the Antarctic surface can accelerate land ice flow and be linked to ice shelf disintegration, further affecting sea-level rise projections. However, previous studies usually focused on SGLs at regional scale or
Xiao-Yi Shen   +5 more
doaj   +1 more source

Fracture criteria and tensile strength for natural glacier ice calibrated from remote sensing observations of Antarctic ice shelves

open access: yesJournal of Glaciology
The conditions under which ice fractures and calves icebergs from Antarctic ice shelves are poorly understood due largely to a lack of relevant observations. Though previous studies have estimated the stresses at which ice fractures in the laboratory and
Sarah Wells-Moran   +2 more
doaj   +1 more source

Mechanical analysis of pinning points in the Ross Ice Shelf, Antarctica

open access: yesAnnals of Glaciology, 2019
Ice shelves regulate the rate of ice-sheet discharge along much of the Antarctic coastline. Pinning points, sites of localised grounding within floating ice, can in turn, regulate the flow and thickness of an ice shelf.
Holly Still   +2 more
doaj   +1 more source

Deformation of Floating Ice Shelves [PDF]

open access: yesJournal of Glaciology, 1957
AbstractThe problem of the creep deformation of floating ice shelves is considered. The problem is solved using Glen’s creep law for ice and Nye’s relation of steady-state creep (the analogue of the Lévy-Miles relation in plasticity theory). Good agreement is obtained between an observed creep rate at Maudheim in the Antarctic and that predicted from ...
openaire   +1 more source

Home - About - Disclaimer - Privacy