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Thirteen years of subglacial lake activity in Antarctica from multi-mission sate...
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Elevation change and mass budget of Ross and Filchner-Ronne ice shelves, Antarct...
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Constructing improved decadal records of Antarctic ice shelf height change from...
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Volume loss from Antarctic ice shelves is accelerating
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Analysis of Ice Plains of Filchner/Ronne Ice Shelf Using ICESat Data
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Antarctic subglacial lakes drain through sediment-floored canals: theory and mod...
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Instantaneous Antarctic ice-sheet mass loss driven by thinning ice shelves
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Antarctic subglacial lakes drain through sediment-floored canals: theory and mod...
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Grounding Zone and Tidal Response of the Amery Ice Shelf, East Antarctica
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A high resolution, three-dimensional view of the D-28 calving event from Amery I...
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A new tide model for the Antarctic ice shelves and seas
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Seasonal variability in Antarctic ice shelf velocities forced by sea surface hei...
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Modeling the dynamic response of outlet glaciers to observed ice-shelf thinning...
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Seasonal variability in Antarctic ice shelf velocities forced by sea surface hei...
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Seasonal variability in Antarctic ice shelf velocities forced by sea surface hei...
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Viscous and elastic buoyancy stresses as drivers of ice-shelf calving
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A decade of progress in observing and modelling Antarctic subglacial water syste...
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Data from: Interannual variations in meltwater input to the Southern Ocean from...
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Modeling the dynamic response of outlet glaciers to observed ice-shelf thinning...
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Seismicity within a propagating ice shelf rift: The relationship between icequak...
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Related Subjects
Geophysics
Antarctica
ACCELERATION
FILCHNER-RONNE ICE
GREENLAND
GROUNDING LINES
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Ice shelves
MARINE ICE
MASS-BALANCE
OCEAN
ROSS SEA
SHELF COLLAPSE
[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography
ICESat-2
Oceanography
F800 Physical and Terrestrial Geographical and Environmental Sciences
Glaciology
Physical Geography and Environmental Geoscience
Sea ice
Verlagsveröffentlichung
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Antarctic glaciology
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Electrical and Electronic Engineering
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