Works matching IS 00359009 AND DT 2012 AND VI 138 AND IP 667
Results: 21
A three-dimensional monotone and conservative semi-Lagrangian scheme (SLICE-3D) for transport problems.
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- Quarterly Journal of the Royal Meteorological Society, 2012, v. 138, n. 667, p. 1640, doi. 10.1002/qj.1902
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Heterogeneous filtering of ensemble-based background-error variances.
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- Quarterly Journal of the Royal Meteorological Society, 2012, v. 138, n. 667, p. 1589, doi. 10.1002/qj.1890
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Variational data-assimilation experiments using flow-dependent dynamical constraints.
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- Quarterly Journal of the Royal Meteorological Society, 2012, v. 138, n. 667, p. 1571, doi. 10.1002/qj.1883
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Convective boundary-layer structure in the presence of wind-following swell.
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- Quarterly Journal of the Royal Meteorological Society, 2012, v. 138, n. 667, p. 1476, doi. 10.1002/qj.1898
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Complex bora flow in the lee of Southern Velebit.
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- Quarterly Journal of the Royal Meteorological Society, 2012, v. 138, n. 667, p. 1490, doi. 10.1002/qj.1901
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Ground-layer snow clouds.
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- Quarterly Journal of the Royal Meteorological Society, 2012, v. 138, n. 667, p. 1507, doi. 10.1002/qj.1882
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Assimilation of water-vapour airborne lidar observations: impact study on the COPS precipitation forecasts.
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- Quarterly Journal of the Royal Meteorological Society, 2012, v. 138, n. 667, p. 1652, doi. 10.1002/qj.1864
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Large-scale potential vorticity anomalies and deep convection.
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- Quarterly Journal of the Royal Meteorological Society, 2012, v. 138, n. 667, p. 1627, doi. 10.1002/qj.1875
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Accelerating and parallelizing minimizations in ensemble and deterministic variational assimilations.
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- Quarterly Journal of the Royal Meteorological Society, 2012, v. 138, n. 667, p. 1599, doi. 10.1002/qj.1886
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Droplet growth in warm turbulent clouds.
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- Quarterly Journal of the Royal Meteorological Society, 2012, v. 138, n. 667, p. 1401, doi. 10.1002/qj.1897
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Large-eddy simulations of surface influences on planetary boundary layer development in southwest Western Australia.
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- Quarterly Journal of the Royal Meteorological Society, 2012, v. 138, n. 667, p. 1465, doi. 10.1002/qj.1879
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Optimal control of katabatic flows within canopies.
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- Quarterly Journal of the Royal Meteorological Society, 2012, v. 138, n. 667, p. 1676, doi. 10.1002/qj.1904
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Relaxing the Tropics to an 'observed' state: analysis using a simple baroclinic model.
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- Quarterly Journal of the Royal Meteorological Society, 2012, v. 138, n. 667, p. 1618, doi. 10.1002/qj.1881
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Diurnal equilibrium convection and land surface-atmosphere interactions in an idealized cloud-resolving model.
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- Quarterly Journal of the Royal Meteorological Society, 2012, v. 138, n. 667, p. 1526, doi. 10.1002/qj.1892
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Evaluation of NWP results for wintertime nocturnal boundary-layer temperatures over Europe and Finland.
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- Quarterly Journal of the Royal Meteorological Society, 2012, v. 138, n. 667, p. 1440, doi. 10.1002/qj.1885
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Interdecadal variability of the ENSO-North Atlantic Oscillation connection in boreal summer.
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- Quarterly Journal of the Royal Meteorological Society, 2012, v. 138, n. 667, p. 1668, doi. 10.1002/qj.1889
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A new implementation of the adaptive mesh transform in the Met Office 3D-Var System.
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- Quarterly Journal of the Royal Meteorological Society, 2012, v. 138, n. 667, p. 1560, doi. 10.1002/qj.1880
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Evaluating raw ensembles with the continuous ranked probability score.
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- Quarterly Journal of the Royal Meteorological Society, 2012, v. 138, n. 667, p. 1611, doi. 10.1002/qj.1891
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Turbulence in the nocturnal boundary layer with light and variable winds.
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- Quarterly Journal of the Royal Meteorological Society, 2012, v. 138, n. 667, p. 1430, doi. 10.1002/qj.1884
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Balanced models of boundary-layer convergence.
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- Quarterly Journal of the Royal Meteorological Society, 2012, v. 138, n. 667, p. 1452, doi. 10.1002/qj.1877
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On the use of EDA background error variances in the ECMWF 4D-Var.
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- Quarterly Journal of the Royal Meteorological Society, 2012, v. 138, n. 667, p. 1540, doi. 10.1002/qj.1899
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