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Willen, Matthias
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Willen, Matthias
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On the quantification of ice sheet mass changes and glacial isostatic adjustment...
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Globally consistent estimates of high-resolution Antarctic ice mass balance and...
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Feasibility of a global inversion for spatially resolved glacial isostatic adjus...
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Spatially resolved GIA in Antarctica from a global inversion ...
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Globally consistent estimates of high-resolution Antarctic ice mass balance and...
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Geodetic GNSS observations disclose the response of the solid Earth to changing...
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The hydrostatic control of load-induced height changes above subglacial Lake Vos...
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The hydrostatic control of load-induced height changes above subglacial Lake Vos...
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Sensitivity of inverse glacial isostatic adjustment estimates over Antarctica
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Sensitivity of inverse glacial isostatic adjustment estimates over Antarctica
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Sensitivity of inverse glacial isostatic adjustment estimates over Antarctica
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Sensitivity of inverse glacial isostatic adjustment estimates over Antarctica
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How well can satellite altimetry and firn models resolve Antarctic firn thicknes...
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Sensitivity of inverse glacial isostatic adjustment estimates over Antarctica
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Mass and volume time series of Antarctic drainage systems derived by a coupled s...
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Mass and volume time series of Antarctic drainage systems derived by a coupled s...
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Surface Mass Balance Models Vs. Stake Observations: A Comparison in the Lake Vos...
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Surface Mass Balance Models Vs. Stake Observations: A Comparison in the Lake Vos...
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Related Subjects
Antarctica
Binary Object
DATE/TIME
Earth-Surface Processes
Event label
GRACE
Massenbilanz
Multiple investigations
Satellite altimetry
Satellitengeodäsie
Verlagsveröffentlichung
article
https://purl.org/becyt/ford/1
https://purl.org/becyt/ford/1.5
mass changes
state space filtering
ANTARCTICA
Antarctic_basin_10
Antarctic_basin_11
Antarctic_basin_12
Antarctic_basin_13
Antarctic_basin_14
Antarctic_basin_19
Antarctic_basin_20
Antarctic_basin_21
Antarctic_basin_22
Antarctic_basin_23
Antarctic_basin_24
Antarctic_basin_4
Antarctic_basin_5
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