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Ice-sheet losses track high-end sea-level rise projections
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Discussing Progress in Understanding Ice Sheet-Ocean Interactions
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Evaluation of a Regional Coupled Ocean – Atmosphere – Sea-Ice Model System over...
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A new ensemble of Arctic and Antarctic regional climate models with storylines t...
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'Calving Laws', 'Sliding Laws', and the Stability of Tidewater Glaciers
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Evaluation of a regional coupled ocean – atmosphere – sea-ice model system over...
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Uncertainties in projected surface mass balance over the polar ice sheets from d...
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'Calving Laws', 'Sliding Laws', and the Stability of Tidewater Glaciers
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Uncertainties in projected surface mass balance over the polar ice sheets from d...
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Spatially distributed runoff at the grounding line of a large Greenlandic tidewa...
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Spatially distributed runoff at the grounding line of a large Greenlandic tidewa...
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Spatially distributed runoff at the grounding line of a large Greenlandic tidewa...
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21st-century climate change around Kangerlussuaq, west Greenland: From the ice s...
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21st-century climate change around Kangerlussuaq, west Greenland:From the ice sh...
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Characteristics of extreme accumulation events in West Antarctica
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Importance of basal processes in simulations of a surging Svalbard outlet glacie...
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Importance of basal processes in simulations of a surging Svalbard outlet glacie...
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Importance of basal processes in simulations of a surging Svalbard outlet glacie...
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Greenland surface air temperature changes from 1981 to 2019 and implications for...
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The importance of accurate glacier albedo for estimates of surface mass balance...
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/dk/atira/pure/sustainabledevelopmentgoals/climate_action
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
firn
name=SDG 13 - Climate Action
[SDU]Sciences of the Universe [physics]
east Antarctic ice sheet
model ensemble
ACCELERATION
Atmospheric turbulence
CLIMATE
CREVASSES
FRACTURE-MECHANICS APPROACH
ICE-SHEETS
PENETRATION
PRESSURE
RETREAT
Regional climate models
SUBGLACIAL WATER
VELOCITY
0750 Sea ice
0758 Remote sensing
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