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Observation Representativeness Error
NWP models simulate the atmospheric state on a given model grid, thereby principally
limiting the...
GJ Marseille, A Stoffelen | Year: 2012
Publication
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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
Publication
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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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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
Publication
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Onset of stratospheric ozone recovery in the Antarctic ozone hole in assimilated daily total ozone columns.
In this paper we evaluate the long-term changes in ozone depletion within the Antarctic ozone hol...
A.T.J. de Laat, M. van Weele | Status: published | Journal: J. Geophys Res | Year: 2017 | doi: 10.1002/2016JD025723
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