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Boundary-layer model results for wind-sea growth
A numerical model of the boundary layer of the atmosphere above a gravity surface wave is rev...
G Burgers, VK Makin | Status: published | Journal: J. Phys. Oceanogr. | Volume: 23 | Year: 1993 | First page: 372 | Last page: 385
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InitMIP-Antarctica: an ice sheet model initialization experiment of ISMIP6
Ice sheet numerical modeling is an important tool to estimate the dynamic contribution of the Ant...
H Seroussi, TJ Reerink, Et al. | Status: published | Journal: The Cryosphere | Year: 2019 | doi: https://doi.org/10.5194/tc-13-1441-2019
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Rapid loss of firn pore space accelerates 21st century Greenland mass loss
Mass loss from the two major ice sheets and their contribution to global sea level rise is accele...
JH van Angelen, JTM Lenaerts, MR van den Broeke, X Fettweis, E van Meijgaard | Status: published | Journal: Geophys. Res. Lett. | Volume: 40 | Year: 2013 | First page: 2109 | Last page: 2113 | doi: 10.1002/grl.50490
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Partitioning Recent Greenland Mass Loss
Mass budget calculations, validated with satellite gravity observations [from the Gravity Recover...
M van den Broeke, J Bamber, J Ettema, E Rignot, E Schrama, WJ van den Berg, E van Meijgaard, I Velicogna, B Wouters | Status: published | Journal: Science | Volume: 326 | Year: 2009 | First page: 984 | Last page: 986 | doi: 10.1126/science.1178176
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Obliquely incident surface waves in shallow water of variable depth
The propagation properties of obliquely incident, weakly nonlinear surface waves in shallow water...
CA van Duin | Status: submitted | Journal: J. Fluid Mech. | Year: 2005
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