All Stories

  1. Quantifying driving ensemble influence on operational convection‐permitting ensemble spread
  2. Assessing the Value of Clustering Convection‐Permitting Ensemble Forecasts
  3. Sensitivity of the Representation of Polar Lows to Typical Climate Model Resolutions
  4. Evaluating trapped lee‐wave characteristics over the UK and Ireland in convection‐permitting model forecasts using satellite imagery
  5. A global climatology of sting-jet extratropical cyclones
  6. The THINICE Field Campaign: Interactions between Arctic Cyclones, Tropopause Polar Vortices, Clouds, and Sea Ice in Summer
  7. The impact of preceding convection on the development of Medicane Ianos and the sensitivity to sea surface temperature
  8. The importance of diabatic processes for the dynamics of synoptic-scale extratropical weather systems – a review
  9. Processes controlling extratropical near‐tropopause humidity and temperature in the ECMWF global weather forecast model
  10. The crucial representation of deep convection for the cyclogenesis of Medicane Ianos
  11. Extreme low‐level wind jets in Storm Ciarán
  12. Improvements in the spread–skill relationship of precipitation in a convective‐scale ensemble through blending
  13. Do AI models produce better weather forecasts than physics-based models? A quantitative evaluation case study of Storm Ciarán
  14. A composite approach to produce reference datasets for extratropical cyclone tracks: application to Mediterranean cyclones
  15. Strong surface winds in Storm Eunice. Part 2: airstream analysis
  16. Strong surface winds in Storm Eunice. Part 1: storm overview and indications of sting jet activity from observations and model data
  17. Rescuing historical weather observations improves quantification of severe windstorm risks
  18. Attribution of observed extreme marine wind speeds and associated hazards to midlatitude cyclone conveyor belt jets near the British Isles
  19. The role of tropopause polar vortices in the intensification of summer Arctic cyclones
  20. The sensitivity of probabilistic convective‐scale forecasts of an extratropical cyclone to atmosphere–ocean–wave coupling
  21. Characterising extratropical near‐tropopause analysis humidity biases and their radiative effects on temperature forecasts
  22. The Impact of Atmosphere–Ocean–Wave Coupling on the Near-Surface Wind Speed in Forecasts of Extratropical Cyclones
  23. A process-based anatomy of Mediterranean cyclones: from baroclinic lows to tropical-like systems
  24. A Physically Based Stochastic Boundary Layer Perturbation Scheme. Part II: Perturbation Growth within a Superensemble Framework
  25. Development of a prototype real‐time sting‐jet precursor tool for forecasters
  26. Linking rapid forecast error growth to diabatic processes
  27. Idealised simulations of cyclones with robust symmetrically unstable sting jets
  28. Impact of model upgrades on diabatic processes in extratropical cyclones and downstream forecast evolution
  29. Sting jets in extratropical cyclones: a review
  30. Downstream influence of mesoscale convective systems. Part 1: influence on forecast evolution
  31. Downstream influence of mesoscale convective systems. Part 2: Influence on ensemble forecast skill and spread
  32. A simple ensemble approach for more robust process‐based sensitivity analysis of case studies in convection‐permitting models
  33. Upstream Cyclone Influence on the Predictability of Block Onsets over the Euro-Atlantic Region
  34. Improvements in Forecasting Intense Rainfall: Results from the FRANC (Forecasting Rainfall Exploiting New Data Assimilation Techniques and Novel Observations of Convection) Project
  35. Atmospheric blocking and upper‐level Rossby‐wave forecast skill dependence on model configuration
  36. Sting jets in extratropical cyclones: a review
  37. The North Atlantic Waveguide and Downstream Impact Experiment
  38. Scientific Challenges of Convective-Scale Numerical Weather Prediction
  39. The role of mesoscale instabilities in the sting-jet dynamics of windstorm Tini
  40. Increased wind risk from sting-jet windstorms with climate change
  41. Convective-Scale Perturbation Growth across the Spectrum of Convective Regimes
  42. Processes Maintaining Tropopause Sharpness in Numerical Models
  43. The weather's response to a solar eclipse
  44. Heavy rainfall in Mediterranean cyclones. Part I: contribution of deep convection and warm conveyor belt
  45. Sting-Jet Windstorms over the North Atlantic: Climatology and Contribution to Extreme Wind Risk
  46. Climatology of Size, Shape, and Intensity of Precipitation Features over Great Britain and Ireland
  47. North Atlantic storm driving of extreme wave heights in the North Sea
  48. Coherent evolution of potential vorticity anomalies associated with deep moist convection
  49. Modulation of precipitation by conditional symmetric instability release
  50. Climatology of Banded Precipitation over the Contiguous United States
  51. Atmospheric changes from solar eclipses
  52. The computation of reference state and APE production by diabatic processes in an idealized tropical cyclone
  53. Diabatic Processes and the Evolution of Two Contrasting Summer Extratropical Cyclones
  54. Eclipse-induced wind changes over the British Isles on the 20 March 2015
  55. The National Eclipse Weather Experiment: an assessment of citizen scientist weather observations
  56. Characterisation of convective regimes over the British Isles
  57. The Utility of Convection-Permitting Ensembles for the Prediction of Stationary Convective Bands
  58. The non‐conservation of potential vorticity by a dynamical core compared with the effects of parametrized physical processes
  59. A route to systematic error in forecasts of Rossby waves
  60. Detection of Coherent Airstreams Using Cluster Analysis: Application to an Extratropical Cyclone
  61. A Diabatically Generated Potential Vorticity Structure near the Extratropical Tropopause in Three Simulated Extratropical Cyclones
  62. A radar-based rainfall climatology of Great Britain and Ireland
  63. Secondary Cyclogenesis along an Occluded Front Leading to Damaging Wind Gusts: Windstorm Kyrill, January 2007
  64. Cloud Banding and Winds in Intense European Cyclones: Results from the DIAMET Project
  65. Synoptic versus orographic control on stationary convective banding
  66. Can reanalyses represent extreme precipitation over England and Wales?
  67. Distinguishing the Cold Conveyor Belt and Sting Jet Airstreams in an Intense Extratropical Cyclone
  68. Foehn jets over the Larsen C Ice Shelf, Antarctica
  69. A case study of sea breeze blocking regulated by sea surface temperature along the English south coast
  70. Understanding and representing atmospheric convection across scales: recommendations from the meeting held at Dartington Hall, Devon, UK, 28-30 January 2013
  71. Systematic model forecast error in Rossby wave structure
  72. Corrigendum: Sting jets in intense winter North-Atlantic windstorms (2012 Environ. Res. Lett. 7 024014)
  73. A mixed-phase bulk orographic precipitation model with embedded convection
  74. The dichotomous structure of the warm conveyor belt
  75. The role of anomalous SST and surface fluxes over the southeastern North Atlantic in the explosive development of windstorm Xynthia
  76. Flow‐dependent predictability of the North Atlantic jet
  77. Quantifying the climatological relationship between extratropical cyclone intensity and atmospheric precursors
  78. Idealised simulations of sting-jet cyclones
  79. Diabatic processes modifying potential vorticity in a North Atlantic cyclone
  80. Ensemble forecasts of a flood-producing storm: comparison of the influence of model-state perturbations and parameter modifications
  81. Sting jets in intense winter North-Atlantic windstorms
  82. Meteorology and eclipses
  83. Case-to-case variability of predictability of deep convection in a mesoscale model
  84. Objective detection of sting jets in low-resolution datasets
  85. Under what conditions does embedded convection enhance orographic precipitation?
  86. Targeted observations of a polar low in the Norwegian Sea
  87. Conditional symmetric instability in sting-jet storms
  88. Ensemble prediction of transitions of the North Atlantic eddy‐driven jet
  89. Mesoscale meteorology in midlatitudes by Paul Markowski and Yvette Richardson. Wiley‐Blackwell, 2010. ISBN: 978‐0470742136. 430 pp.
  90. Forecast Impact of Targeted Observations: Sensitivity to Observation Error and Proximity to Steep Orography
  91. A comparison of stratosphere‐troposphere transport in convection‐permitting and convection‐parameterizing simulations of three mesoscale convective systems
  92. Sting Jets in Simulations of a Real Cyclone by Two Mesoscale Models
  93. Can 4D‐Var use dynamical information from targeted observations of a baroclinic structure?
  94. Categorisation of synoptic environments associated with mesoscale convective systems over the UK
  95. Controls on boundary layer ventilation: Boundary layer processes and large‐scale dynamics
  96. Perturbation growth at the convective scale for CSIP IOP18
  97. Synoptic Controls on Boundary-Layer Characteristics
  98. The impact of targeted observations made during the Greenland Flow Distortion Experiment
  99. Horizontal potential vorticity dipoles on the convective storm scale
  100. The dynamics of a polar low assessed using potential vorticity inversion
  101. On the dependence of boundary layer ventilation on frontal type
  102. The Spatial Distribution and Evolution Characteristics of North Atlantic Cyclones
  103. THE GREENLAND FLOW DISTORTION EXPERIMENT
  104. Boundary‐layer ventilation by baroclinic life cycles
  105. MESOSCALE DYNAMICS, by Yuh‐Lang Lin, Cambridge University Press, 2007 ISBN: 9780521808750
  106. The impact of deformation strain on the formation of banded clouds in idealized modelling experiments
  107. Analysis of convectively‐generated gravity waves in mesoscale model simulations and wind‐profiler observations
  108. An objective climatology of the dynamical forcing of polar lows in the Nordic seas
  109. A case study of boundary layer ventilation by convection and coastal processes
  110. Stratosphere‐troposphere transport in a numerical simulation of midlatitude convection
  111. Life‐cycle simulations of shallow frontal waves and the impact of deformation strain
  112. Mechanisms of midlatitude cross‐tropopause transport using a potential vorticity budget approach
  113. Reply to comments by David M. Schultz on ‘Cloud-resolving model simulations of multiply-banded frontal clouds’ (October A, 2005,131, 2617–2637)
  114. Mesoscale simulations of organized convection: Importance of convective equilibrium
  115. Classifying dynamical forcing mechanisms using a climatology of extratropical cyclones
  116. Cloud‐resolving model simulations of multiply‐banded frontal clouds
  117. Numerical modeling study of boundary‐layer ventilation by a cold front over Europe
  118. The Extratropical Transition of Tropical Cyclone Lili (1996) and Its Crucial Contribution to a Moderate Extratropical Development
  119. The extratropical transition of hurricane Irene (1999): A potential‐vorticity perspective
  120. Dynamics of the atmosphere: a course in theoretical meteorology, by Wilford Zdunkowski and Andreas Bott, Cambridge University Press, Cambridge, 2003. No. of Pages: xviii + 719. ISBN 0‐521‐00666‐X (paperback), ISBN 0‐521‐8099‐5 (hardback).
  121. On a threefold classification of extratropical cyclogenesis
  122. On a threefold classification of extratropical cyclogenesis
  123. A case study of stratosphere to troposphere transport: The role of convective transport and the sensitivity to model resolution
  124. Quantifying mesoscale variability in ocean transient tracer fields
  125. Parcel Theory in Three Dimensions and the Calculation of SCAPE
  126. Constraining a North Atlantic Ocean General Circulation Model with Chlorofluorocarbon Observations
  127. Potential energy for slantwise parcel motion
  128. Analysis of the eyes formed in simulated tropical cyclones and polar lows
  129. A simple theoretical model for the intensification of tropical cyclones and polar lows
  130. CISK or WISHE as the Mechanism for Tropical Cyclone Intensification