Results 101 to 110 of about 917,323 (294)

Simulated melt rates for the Totten and Dalton ice shelves [PDF]

open access: yesOcean Science, 2014
The Totten Glacier is rapidly losing mass. It has been suggested that this mass loss is driven by changes in oceanic forcing; however, the details of the ice–ocean interaction are unknown.
D. E. Gwyther   +3 more
doaj   +1 more source

Catastrophic ice-shelf break-up by an ice-shelf-fragment-capsize mechanism [PDF]

open access: yesJournal of Glaciology, 2003
AbstractTwo disintegration events leading to the loss of Larsen A and B ice shelves, Antarctic Peninsula, in 1995 and 2002, respectively, proceeded with extreme rapidity (order of several days) and reduced an extensive, seemingly integrated ice shelf to ajumble of small fragments.
Christina L. Hulbe   +3 more
openaire   +2 more sources

Investigation of land ice-ocean interaction with a fully coupled ice-ocean model, Part 1: Model description and behavior [PDF]

open access: yes, 2012
Antarctic ice shelves interact closely with the ocean cavities beneath them, with ice shelf geometry influencing ocean cavity circulation, and heat from the ocean driving changes in the ice shelves, as well as the grounded ice streams that feed them.
A. Gnanadesikan   +62 more
core   +1 more source

On the interpretation of ice-shelf flexure measurements [PDF]

open access: yesJournal of Glaciology, 2017
ABSTRACTTidal flexure in ice shelf grounding zones has been used extensively in the past to determine grounding line position and ice properties. Although the rheology of ice is viscoelastic at tidal loading frequencies, most modelling studies have assumed some form of linear elastic beam approximation to match observed flexure profiles.
Rosier, Sebastian H.R.   +5 more
openaire   +5 more sources

Instantaneous Antarctic ice-sheet mass loss driven by thinning ice shelves [PDF]

open access: yes, 2019
Recent observations show that the rate at which the Antarctic Ice Sheet (AIS) is contributing to sea level rise is increasing. Increasing ice-ocean heat exchange has the potential to induce substantial mass loss through the melting of its ice shelves ...
Adusumilli, Susheel   +3 more
core   +1 more source

Energetics of Eddy-Mean Flow Interactions in the Amery Ice Shelf Cavity

open access: yesFrontiers in Marine Science, 2021
Previous studies demonstrated that eddy processes play an important role in ice shelf basal melting and the water mass properties of ice shelf cavities.
Yang Wu   +5 more
doaj   +1 more source

Ice-shelf buttressing and the stability of marine ice sheets [PDF]

open access: yesThe Cryosphere, 2012
Abstract. Ice-shelf buttressing and the stability of marine-type ice sheets is investigated numerically. Buttressing effects are analysed for a situation where a stable grounding line is located on a bed sloping upwards in the direction of flow. Such grounding-line positions are known to be unconditionally unstable in the absence of transverse flow ...
openaire   +5 more sources

Tidal modulation of ice-shelf flow: a viscous model of the Ross Ice Shelf [PDF]

open access: yesJournal of Glaciology, 2014
AbstractThree stations near the calving front of the Ross Ice Shelf, Antarctica, recorded GPS data through a full spring–neap tidal cycle in November 2005. The data revealed a diurnal horizontal motion that varied both along and transverse to the long-term average velocity direction, similar to tidal signals observed in other ice shelves and ice ...
Kelly M. Brunt, Douglas R. MacAyeal
openaire   +2 more sources

Deglaciation and ice shelf development at the northeast margin of the Laurentide Ice Sheet during the Younger Dryas chronozone [PDF]

open access: yes, 2017
Core 2011804‐0010 from easternmost Lancaster Sound provides important insights into deglacial timing and style at the marine margin of the NE Laurentide Ice Sheet (LIS). Spanning 13.2–11.0 cal.
Bennett, R   +4 more
core   +2 more sources

Projecting Antarctica's contribution to future sea level rise from basal ice shelf melt using linear response functions of 16 ice sheet models (LARMIP-2)

open access: yesEarth System Dynamics, 2019
. The sea level contribution of the Antarctic ice sheet constitutes a large uncertainty in future sea level projections. Here we apply a linear response theory approach to 16 state-of-the-art ice sheet models to estimate the Antarctic ice sheet ...
A. Levermann   +36 more
semanticscholar   +1 more source

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