Results 31 to 40 of about 102,620 (291)

Brief communication: widespread potential for seawater infiltration on Antarctic ice shelves [PDF]

open access: yesThe Cryosphere, 2018
Antarctica's future contribution to sea level change depends on the fate of its fringing ice shelves. One factor which may affect the rate of iceberg calving from ice shelves is the presence of liquid water, including the percolation of seawater into ...
S. Cook   +5 more
doaj   +1 more source

Brief communication: A submarine wall protecting the Amundsen Sea intensifies melting of neighboring ice shelves [PDF]

open access: yesThe Cryosphere, 2019
Disintegration of ice shelves in the Amundsen Sea, in front of the West Antarctic Ice Sheet, has the potential to cause sea level rise by inducing an acceleration of ice discharge from upstream grounded ice. Moore et al.
Ö. Gürses   +4 more
doaj   +1 more source

Supervised classification of slush and ponded water on Antarctic ice shelves using Landsat 8 imagery

open access: yesJournal of Glaciology, 2022
Surface meltwater is becoming increasingly widespread on Antarctic ice shelves. It is stored within surface ponds and streams, or within firn pore spaces, which may saturate to form slush.
Rebecca L. Dell   +6 more
doaj   +1 more source

Can unconfined ice shelves provide buttressing via hoop stresses?

open access: yesJournal of Glaciology, 2020
The stress balance within an ice shelf is key to the resistance, or buttressing, it can provide and in part controls the rate of ice discharge from the upstream ice sheet. Unconfined ice shelves are widely assumed to provide no buttressing.
Martin G. Wearing   +2 more
doaj   +1 more source

New gravity-derived bathymetry for the Thwaites, Crosson, and Dotson ice shelves revealing two ice shelf populations [PDF]

open access: yesThe Cryosphere, 2020
Ice shelves play a critical role in the long-term stability of ice sheets through their buttressing effect. The underlying bathymetry and cavity thickness are key inputs for modelling future ice sheet evolution.
T. A. Jordan   +8 more
doaj   +1 more source

The origin of green icebergs in Antarctica [PDF]

open access: yes, 1992
A comparison of samples from a translucent green iceberg with a core from the Ronne Ice Shelf revealed an excellent agreement in isotopic composition, crystal structure, and incorporated sediment particles.
Amos   +34 more
core   +1 more source

Predicting the steady-state isochronal stratigraphy of ice shelves using observations and modeling [PDF]

open access: yesThe Cryosphere, 2022
Ice shelves surrounding the Antarctic perimeter moderate ice discharge towards the ocean through buttressing. Ice-shelf evolution and integrity depend on the local surface accumulation, basal melting and on the spatially variable ice-shelf viscosity ...
V. Višnjević   +7 more
doaj   +1 more source

Calving Fronts of Antarctica: Mapping and Classification

open access: yesRemote Sensing, 2013
Antarctica is surrounded by a variety of large, medium and small sized ice shelves, glacier tongues and coastal areas without offshore floating ice masses. We used the mosaic of the Radarsat-1 Antarctica Mapping Project (RAMP) Antarctic Mapping Mission 1
Christine Wesche   +2 more
doaj   +1 more source

'Calving laws', 'sliding laws' and the stability of tidewater glaciers [PDF]

open access: yes, 2007
A new calving criterion is introduced, which predicts calving where the depth of surface crevasses equals ice height above sea level. Crevasse depth is calculated from strain rates, and terminus position and calving rate are therefore functions of ice ...
Brown   +5 more
core   +1 more source

Evaluation of four calving laws for Antarctic ice shelves [PDF]

open access: yesThe Cryosphere, 2023
Many floating ice shelves in Antarctica buttress the ice streams feeding them, thereby reducing the discharge of icebergs into the ocean. The rate at which ice shelves calve icebergs and how fast they flow determine whether they advance, retreat, or ...
J. A. Wilner, M. Morlighem, G. Cheng
doaj   +1 more source

Home - About - Disclaimer - Privacy