Abrupt cooling over the North Atlantic in modern climate models
Observations over the 20th century evidence no long-term warming in the subpolar North Atlantic (...
G Sgubin, D Swingedouw, SS Drijfhout | Status: accepted | Journal: Nature Communications | Volume: 8 | Year: 2017 | doi: https://doi.org/10.1038/ncomms14375
Observation Representativeness Error
NWP models simulate the atmospheric state on a given model grid, thereby principally
GJ Marseille, A Stoffelen | Year: 2012
Polar amplification in a coupled climate model with locked albedo
In recent years, a substantial reduction of the
sea ice in the Arctic has been observed. At the s...
RG Graversen, M Wang | Status: published | Journal: Clim. Dyn. | Volume: 33 | Year: 2009 | First page: 629 | Last page: 643 | doi: 10.1007/s00382-009-0535-6
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
Impact of ASCAT Scatterometer Wind Observations on the High-Resolution Limited-Area Model (HIRLAM) within an Operational Context
Denial experiments, also denoted observing system experiments (OSEs), are used to determine the i...
S de Haan, GJ Marseille, P de Valk, J de Vries | Status: published | Journal: Weather and Forecasting | Year: 2013 | doi: https://doi.org/10.1175/WAF-D-12-00056.1