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The marine geological imprint of Antarctic ice shelves [PDF]

open access: yesNature Communications, 2019
The recent collapses of ice shelves in Antarctica due to warming make it essential to understand past ice shelf conditions and mechanisms. Here Smith and colleagues review the latest progress in deciphering the geological imprint of Antarctic ice shelves
James A. Smith   +5 more
doaj   +8 more sources

Rapid disintegration and weakening of ice shelves in North Greenland [PDF]

open access: yesNature Communications, 2023
The glaciers of North Greenland are hosting enough ice to raise sea level by 2.1 m, and have long considered to be stable. This part of Greenland is buttressed by the last remaining ice shelves of the ice sheet. Here, we show that since 1978, ice shelves
R. Millan   +7 more
doaj   +3 more sources

Seawater softening of suture zones inhibits fracture propagation in Antarctic ice shelves. [PDF]

open access: goldNat Commun, 2019
Suture zones are abundant on Antarctic ice shelves and widely observed to impede fracture propagation, greatly enhancing ice-shelf stability. Using seismic and radar observations on the Larsen C Ice Shelf of the Antarctic Peninsula, we confirm that such ...
Kulessa B   +10 more
europepmc   +4 more sources

Annual mass budget of Antarctic ice shelves from 1997 to 2021. [PDF]

open access: yesSci Adv, 2023
Antarctic ice shelves moderate the contribution of the Antarctic Ice Sheet to global sea level rise; however, ice shelf health remains poorly constrained. Here, we present the annual mass budget of all Antarctic ice shelves from 1997 to 2021.
Davison BJ   +8 more
europepmc   +2 more sources

Ocean-excited plate waves in the Ross and Pine Island Glacier ice shelves [PDF]

open access: goldJournal of Glaciology, 2018
Ice shelves play an important role in buttressing land ice from reaching the sea, thus restraining the rate of grounded ice loss. Long-period gravity-wave impacts excite vibrations in ice shelves that can expand pre-existing fractures and trigger iceberg
ZHAO CHEN   +6 more
doaj   +3 more sources

Sea ice-free corridors for large swell to reach Antarctic ice shelves

open access: yesEnvironmental Research Letters, 2022
Sea ice can attenuate Southern Ocean swell before it reaches Antarctic ice shelves and imposes flexural stresses, which promote calving of outer ice-shelf margins and influence ice shelf stability.
N J Teder   +3 more
doaj   +2 more sources

The role of double-diffusive convection in basal melting of Antarctic ice shelves. [PDF]

open access: yesProc Natl Acad Sci U S A, 2021
Significance Ocean-driven melting of ice shelves is a leading cause of mass loss from Antarctica. However, the small-scale ocean processes responsible for melting are poorly understood due to the difficulty of making direct measurements in these hard to ...
Rosevear MG, Gayen B, Galton-Fenzi BK.
europepmc   +2 more sources

Interannual variations in meltwater input to the Southern Ocean from Antarctic ice shelves. [PDF]

open access: yesNat Geosci, 2020
Ocean-driven basal melting of Antarctica’s floating ice shelves accounts for about half of their mass loss in steady state, where gains in ice-shelf mass are balanced by losses. Ice-shelf thickness changes driven by varying basal melt rates modulate mass
Adusumilli S   +4 more
europepmc   +2 more sources

The Creep of Ice Shelves Theory [PDF]

open access: bronzeJournal of Glaciology, 1973
AbstractBudd’s expressions for strain-rate gradient along the centre line of a bounded ice shelf are shown to be applicable only to ice shelves with almost constant thickness and very small longitudinal strain-rates. A general expression is derived for creep in an ice shelf where the sole restriction is that of zero shear stresses in vertical planes ...
Robert Thomas
openalex   +4 more sources

Progressive unanchoring of Antarctic ice shelves since 1973. [PDF]

open access: yesNature
Mass loss of the Antarctic Ice Sheet has been driven primarily by the thinning of the floating ice shelves that fringe the ice sheet1, reducing their buttressing potential and causing land ice to accelerate into the ocean2.
Miles BWJ, Bingham RG.
europepmc   +2 more sources

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