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Exceptionally High Geothermal Heat Flux Needed to Sustain the Northeast Greenland Ice Stream (1) ·
Implementing an empirical scalar tertiary anisotropic rheology (ESTAR) into large-scale ice sheet models (1) ·
Sensitivity of Greenland ice sheet projections to spatial resolution in higher-order simulations: the AWI contribution to ISMIP6-Greenland using ISSM (1)
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