Works matching IS 00359009 AND DT 2013 AND VI 139 AND IP 676
Results: 19
Departures from convective equilibrium with a rapidly varying surface forcing.
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- Quarterly Journal of the Royal Meteorological Society, 2013, v. 139, n. 676, p. 1731, doi. 10.1002/qj.2065
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A critical revision of the estimation of the latent heat flux from two-wavelength scintillometry.
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- Quarterly Journal of the Royal Meteorological Society, 2013, v. 139, n. 676, p. 1912, doi. 10.1002/qj.2076
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Tropical cyclone predictions over the Bay of Bengal using the high-resolution Advanced Research Weather Research and Forecasting (ARW) model.
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- Quarterly Journal of the Royal Meteorological Society, 2013, v. 139, n. 676, p. 1810, doi. 10.1002/qj.2064
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Improved variational analyses using a nonlinear humidity control variable.
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- Quarterly Journal of the Royal Meteorological Society, 2013, v. 139, n. 676, p. 1875, doi. 10.1002/qj.2073
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Comments on 'Sensitivity of tropical-cyclone models to the surface drag coefficient'.
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- Quarterly Journal of the Royal Meteorological Society, 2013, v. 139, n. 676, p. 1957, doi. 10.1002/qj.2066
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An iterative ensemble square root filter and tests with simulated radar data for storm-scale data assimilation.
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- Quarterly Journal of the Royal Meteorological Society, 2013, v. 139, n. 676, p. 1888, doi. 10.1002/qj.2077
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On-line calibration of the vertical distribution of ensemble spread.
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- Quarterly Journal of the Royal Meteorological Society, 2013, v. 139, n. 676, p. 1863, doi. 10.1002/qj.2072
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The role of upper-level dynamics and surface processes for the Pakistan flood of July 2010.
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- Quarterly Journal of the Royal Meteorological Society, 2013, v. 139, n. 676, p. 1780, doi. 10.1002/qj.2082
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Snowbands over the English Channel and Irish Sea during cold-air outbreaks.
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- Quarterly Journal of the Royal Meteorological Society, 2013, v. 139, n. 676, p. 1747, doi. 10.1002/qj.2079
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The effective density of small ice particles obtained from in situ aircraft observations of mid-latitude cirrus.
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- Quarterly Journal of the Royal Meteorological Society, 2013, v. 139, n. 676, p. 1923, doi. 10.1002/qj.2058
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Convective boundary layer wind dynamics and inertial oscillations: the influence of surface stress.
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- Quarterly Journal of the Royal Meteorological Society, 2013, v. 139, n. 676, p. 1694, doi. 10.1002/qj.2069
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Ensemble spread-based assessment of observation impact: application to a global ocean analysis system.
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- Quarterly Journal of the Royal Meteorological Society, 2013, v. 139, n. 676, p. 1842, doi. 10.1002/qj.2071
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A two-step variational method for analyzing severely aliased radar velocity observations with small Nyquist velocities.
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- Quarterly Journal of the Royal Meteorological Society, 2013, v. 139, n. 676, p. 1904, doi. 10.1002/qj.2075
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A method to diagnose boundary-layer type using Doppler lidar.
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- Quarterly Journal of the Royal Meteorological Society, 2013, v. 139, n. 676, p. 1681, doi. 10.1002/qj.2068
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Analysis error covariance versus posterior covariance in variational data assimilation.
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- Quarterly Journal of the Royal Meteorological Society, 2013, v. 139, n. 676, p. 1826, doi. 10.1002/qj.2070
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The evaluation of the integrated water vapour annual cycle over the Iberian Peninsula from EOS-MODIS against different ground-based techniques.
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- Quarterly Journal of the Royal Meteorological Society, 2013, v. 139, n. 676, p. 1935, doi. 10.1002/qj.2080
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Sensitivity of deep convection to terrain forcing over Mediterranean islands.
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- Quarterly Journal of the Royal Meteorological Society, 2013, v. 139, n. 676, p. 1762, doi. 10.1002/qj.2089
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The structure and evolution of lower stratospheric frontal zones. Part II: The influence of tropospheric ascent on lower stratospheric frontal development.
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- Quarterly Journal of the Royal Meteorological Society, 2013, v. 139, n. 676, p. 1798, doi. 10.1002/qj.2074
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Impact of soil moisture and convectively generated waves on the initiation of a West African mesoscale convective system.
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- Quarterly Journal of the Royal Meteorological Society, 2013, v. 139, n. 676, p. 1712, doi. 10.1002/qj.2062
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