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Konrad, H.
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Sea-level and solid-Earth feedbacks on ice-sheet dynamics
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Advances in geodetic estimates of glacial-isostatic adjustment in Antarctica and...
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Potential of the solid-Earth response for limiting long-term West Antarctic Ice...
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Potential of the solid-Earth response for limiting long-term West Antarctic Ice...
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Determining the age distribution of Colle Gnifetti, Monte Rosa, Alps, by combini...
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Impact of lateral variations in Antarctica lithosphere structure on glacial isos...
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Lateral variations in lithosphere structure of Antarctica – Impact on GIA respon...
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Re-assessing the influence of glacial-isostatic adjustment on Antarctic ice-mass...
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Impact of Lateral variations in Antarctic lithosphere structure on glacial isost...
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Determining the age distribution of Colle Gnifetti, Monte Rosa, Swiss Alps, by c...
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Sensitivity of grounding line dynamics to viscoelastic deformation of the solid...
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Sea-level and solid-Earth deformation feedbacks in ice sheet modelling
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Sensitivity of Grounding-Line Dynamics to Viscoelastic Deformation of the Solid-...
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Acceleration of Dynamic Ice Loss in Antarctica From Satellite Gravimetry
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Observations of surface mass balance on Pine Island Glacier, West Antarctica, an...
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The Deformational Response of a Viscoelastic Solid Earth Model Coupled to a Ther...
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Uneven onset and pace of ice-dynamical imbalance in the Amundsen Sea Embayment,...
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Net retreat of Antarctic glacier grounding lines
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A new digital elevation model of Antarctica derived from CryoSat-2 altimetry
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Uneven onset and pace of ice-dynamical imbalance in the Amundsen Sea Embayment,...
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ddc:
550 - Earth sciences
AMUNDSEN SEA EMBAYMENT
Amundsen Sea
Antarctica
BASIN-SCALE
EARTH
EAST ANTARCTICA
ELEVATION CHANGE
EXCEED LOSSES
Earth sciences & physical geography
F890 Geographical and Environmental Sciences not elsewhere classified
GLACIAL-ISOSTATIC-ADJUSTMENT
GREENLAND
Glacier retreat
IMPACT
MAUD-LAND
MODELS
Multidisciplinary Sciences
NORTH-AMERICA
PENINSULA
PINE ISLAND
Physical
Physique
SEA-LEVEL CHANGE
SHEET
SIGNAL
SUBGLACIAL LAKE VOSTOK
SURFACE
Science & Technology
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