Works matching IS 00359009 AND DT 2024 AND VI 150 AND IP 764
Results: 41
Issue Information.
- Published in:
- Quarterly Journal of the Royal Meteorological Society, 2024, v. 150, n. 764, p. i, doi. 10.1002/qj.4894
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- Article
Physics–dynamics–chemistry coupling across different meshes in LFRic‐Atmosphere: Formulation and idealised tests.
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- Quarterly Journal of the Royal Meteorological Society, 2024, v. 150, n. 764, p. 4650, doi. 10.1002/qj.4836
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A neural network to retrieve cloud cover from all‐sky cameras: A case of study over Antarctica.
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- Quarterly Journal of the Royal Meteorological Society, 2024, v. 150, n. 764, p. 4631, doi. 10.1002/qj.4834
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Generation of state‐dependent ensemble perturbations based on time‐varying seawater density for GloSea5 initialization.
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- Quarterly Journal of the Royal Meteorological Society, 2024, v. 150, n. 764, p. 4609, doi. 10.1002/qj.4833
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Mountain waves developing inside and aloft stably stratified turbulent boundary layers.
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- Quarterly Journal of the Royal Meteorological Society, 2024, v. 150, n. 764, p. 4594, doi. 10.1002/qj.4832
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The role of collision and coalescence on the microphysics of marine fog.
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- Quarterly Journal of the Royal Meteorological Society, 2024, v. 150, n. 764, p. 4580, doi. 10.1002/qj.4831
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On the thermodynamic invariance of fine‐grain and coarse‐grain fluid models.
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- Quarterly Journal of the Royal Meteorological Society, 2024, v. 150, n. 764, p. 4567, doi. 10.1002/qj.4830
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Beyond the regional average: Drivers of geographical rainfall variability during East Africa's short rains.
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- Quarterly Journal of the Royal Meteorological Society, 2024, v. 150, n. 764, p. 4550, doi. 10.1002/qj.4829
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Large model biases in the Pacific centre of the Northern Annular Mode due to exaggerated variability of the Aleutian Low.
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- Quarterly Journal of the Royal Meteorological Society, 2024, v. 150, n. 764, p. 4478, doi. 10.1002/qj.4825
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Importance of CCN activation for fog forecasting and its representation in the two‐moment microphysical scheme LIMA.
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- Quarterly Journal of the Royal Meteorological Society, 2024, v. 150, n. 764, p. 4217, doi. 10.1002/qj.4812
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Causal dependencies and Shannon entropy budget: Analysis of a reduced‐order atmospheric model.
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- Quarterly Journal of the Royal Meteorological Society, 2024, v. 150, n. 764, p. 4066, doi. 10.1002/qj.4805
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Establishing a limited‐area model based on a global model: A consistency study.
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- Quarterly Journal of the Royal Meteorological Society, 2024, v. 150, n. 764, p. 4049, doi. 10.1002/qj.4804
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Influences on North‐Atlantic summer climate from the El Niño‐Southern Oscillation.
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- Quarterly Journal of the Royal Meteorological Society, 2024, v. 150, n. 764, p. 4498, doi. 10.1002/qj.4826
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Dynamics of May 'onset' of Indian summer monsoon over Northeast India.
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- Quarterly Journal of the Royal Meteorological Society, 2024, v. 150, n. 764, p. 4533, doi. 10.1002/qj.4828
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Potential‐temperature variance budget in a saturated coastal‐fog environment.
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- Quarterly Journal of the Royal Meteorological Society, 2024, v. 150, n. 764, p. 4511, doi. 10.1002/qj.4827
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The fractions skill score for ensemble forecast verification.
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- Quarterly Journal of the Royal Meteorological Society, 2024, v. 150, n. 764, p. 4457, doi. 10.1002/qj.4824
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Impacts of free tropospheric turbulence parametrisation on a sheared tropical cyclone.
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- Quarterly Journal of the Royal Meteorological Society, 2024, v. 150, n. 764, p. 4437, doi. 10.1002/qj.4823
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Development of the signal‐to‐noise paradox in subseasonal forecasting models: When? Where? Why?
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- Quarterly Journal of the Royal Meteorological Society, 2024, v. 150, n. 764, p. 4417, doi. 10.1002/qj.4822
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Increasing frequency and precipitation intensity of convective storms in the Peruvian Central Andes: Projections from convection‐permitting regional climate simulations.
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- Quarterly Journal of the Royal Meteorological Society, 2024, v. 150, n. 764, p. 4371, doi. 10.1002/qj.4820
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Unprecedented monsoon precipitation over southwest Pakistan in 2022: Regional processes in moistening the climatological heat low.
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- Quarterly Journal of the Royal Meteorological Society, 2024, v. 150, n. 764, p. 4391, doi. 10.1002/qj.4821
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Developing a methodology for user‐oriented verification of polar low forecasts.
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- Quarterly Journal of the Royal Meteorological Society, 2024, v. 150, n. 764, p. 4348, doi. 10.1002/qj.4819
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Evaluation of near‐surface and boundary‐layer meteorological conditions that support cold‐fog formation using Cold Fog Amongst Complex Terrain field campaign observations.
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- Quarterly Journal of the Royal Meteorological Society, 2024, v. 150, n. 764, p. 4329, doi. 10.1002/qj.4818
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Grey‐zone simulations of shallow‐to‐deep convection transition using dynamic subgrid‐scale turbulence models.
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- Quarterly Journal of the Royal Meteorological Society, 2024, v. 150, n. 764, p. 4306, doi. 10.1002/qj.4817
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Summer Heatwaves in Southeastern Australia.
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- Quarterly Journal of the Royal Meteorological Society, 2024, v. 150, n. 764, p. 4285, doi. 10.1002/qj.4816
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A mixed finite‐element, finite‐volume, semi‐implicit discretisation for atmospheric dynamics: Spherical geometry.
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- Quarterly Journal of the Royal Meteorological Society, 2024, v. 150, n. 764, p. 4252, doi. 10.1002/qj.4814
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Estimating the gain of increasing the ensemble size from analytical considerations.
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- Quarterly Journal of the Royal Meteorological Society, 2024, v. 150, n. 764, p. 4270, doi. 10.1002/qj.4815
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Insights from very‐large‐ensemble data assimilation experiments with a high‐resolution general circulation model of the Red Sea.
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- Quarterly Journal of the Royal Meteorological Society, 2024, v. 150, n. 764, p. 4235, doi. 10.1002/qj.4813
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Spectral scaling of unstably stratified atmospheric flows: Turbulence anisotropy and the low‐frequency spread.
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- Quarterly Journal of the Royal Meteorological Society, 2024, v. 150, n. 764, p. 4196, doi. 10.1002/qj.4811
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Towards unified land data assimilation at ECMWF: Soil and snow temperature analysis in the SEKF.
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- Quarterly Journal of the Royal Meteorological Society, 2024, v. 150, n. 764, p. 4133, doi. 10.1002/qj.4808
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Two‐way feedback between the Madden–Julian Oscillation and diurnal warm layers in a coupled ocean–atmosphere model.
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- Quarterly Journal of the Royal Meteorological Society, 2024, v. 150, n. 764, p. 4113, doi. 10.1002/qj.4807
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Improving supercooled liquid water representation in the microphysical scheme ICE3.
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- Quarterly Journal of the Royal Meteorological Society, 2024, v. 150, n. 764, p. 4086, doi. 10.1002/qj.4806
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Evaluating synthetic aperture radar surface winds for convective squalls in the Gulf of Mexico.
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- Quarterly Journal of the Royal Meteorological Society, 2024, v. 150, n. 764, p. 4178, doi. 10.1002/qj.4810
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Ensemble weather forecast post‐processing with a flexible probabilistic neural network approach.
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- Quarterly Journal of the Royal Meteorological Society, 2024, v. 150, n. 764, p. 4156, doi. 10.1002/qj.4809
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The ERA5 global reanalysis from 1940 to 2022.
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- Quarterly Journal of the Royal Meteorological Society, 2024, v. 150, n. 764, p. 4014, doi. 10.1002/qj.4803
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Improving inland precipitation forecast in China through data assimilation of microwave temperature sounding data from a three‐orbit constellation.
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- Quarterly Journal of the Royal Meteorological Society, 2024, v. 150, n. 764, p. 3989, doi. 10.1002/qj.4802
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Investigating the medium‐range predictability of European heatwave onsets in relation to weather regimes using ensemble reforecasts.
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- Quarterly Journal of the Royal Meteorological Society, 2024, v. 150, n. 764, p. 3957, doi. 10.1002/qj.4801
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Time variability and periodicities of cross‐regional hydroclimatic causation in the contiguous United States.
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- Quarterly Journal of the Royal Meteorological Society, 2024, v. 150, n. 764, p. 3942, doi. 10.1002/qj.4800
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An analytical model for daily‐periodic slope winds. Part 2: Solutions.
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- Quarterly Journal of the Royal Meteorological Society, 2024, v. 150, n. 764, p. 3925, doi. 10.1002/qj.4787
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An analytical model for daily‐periodic slope winds. Part 1: Surface radiation budget.
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- Quarterly Journal of the Royal Meteorological Society, 2024, v. 150, n. 764, p. 3911, doi. 10.1002/qj.4785
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- Article
Near‐surface wind profiles from numerical model predictions. Part II: Verifications against Australia‐wide surface wind observations.
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- Quarterly Journal of the Royal Meteorological Society, 2024, v. 150, n. 764, p. 3891, doi. 10.1002/qj.4780
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Near‐surface wind profiles from numerical model predictions. Part I: Algorithms and comparisons with wind profile based on Monin–Obukhov similarity theory.
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- Quarterly Journal of the Royal Meteorological Society, 2024, v. 150, n. 764, p. 3875, doi. 10.1002/qj.4779
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