Kinematic and thermodynamic study of a shallow hailstorm sampled by the McGill bistatic multiple-doppler radar network

Journal of the Atmospheric Sciences

Volumn 58, Issue 10, 2001, Pages 1222-1248

  Protat, A ^a   Zawadzki, I ^a   Caya, A ^a  

^a SERVICE D AÉRONOMIE DU CNRS   (France)

Author keywords

[No Author keywords available]

Indexed keywords

COMPUTER SIMULATION; DOPPLER EFFECT; MORPHOLOGY; PRECIPITATION (METEOROLOGY); RADAR; TORNADOES;

CONVECTIVE CELLS;

METEOROLOGY;

CONVECTIVE SYSTEM; DOPPLER RADAR; HAIL; KINEMATICS; THERMODYNAMICS;

EID: 0035872795     PISSN: 00224928     EISSN: None     Source Type: Journal    
DOI: 10.1175/1520-0469(2001)058<1222:KATSOA>2.0.CO;2     Document Type: Article

References (41)

1. Some aspects of a severe, right-moving thunderstorm deduced from mesonetwork rawindsonde observations
2. Oklahoma thunderstorms on 29-30 April 1970. Part I: Morphology of a tornadic storm
3. Relationships between radar-derived thermodynamic variables and tornadogenesis
4. Initiation and evolution of updraft rotation within an incipient supercell storm
5. Airflow and precipitation trajectories within severe local storms which travel to the right of the winds
6. Midget supercell spawns tornadoes
7. Updraft properties deduced statistically from rawindsoundings
8. Sidelobe contamination in bistatic radars
9. Airborne Doppler radar analysis of supercell during COPS-91
10. What is an adjoint model
11. Structure of a midlatitude squall line formed in strong unidirectional shear
12. Case study of a hailstorm in Colorado.: Radar echo structure and evolution
13. A method for the initialization of the anelastic equations: Implications for matching models with observations
14. Errors in fixed and moving frame of references: Applications for conventional and Doppler radar analysis
15. Buoyancy and pressure perturbations derived from dual-Doppler radar observations of the planetary boundary layer: Applications for matching models with observations
16. Pressure and buoyancy fields derived from Doppler radar in a tornadic thunderstorm
17. Retrieval of thermodynamic variables within deep convective clouds: Experiments in three dimensions
18. Single-Doppler radar observations of a mini-supercell tornadic thunderstorm
19. The simulation of three-dimensional convective storm dynamics
20. A study of the tornadic region within a supercell thunderstorm
21. Observations of steady, low buoyancy, low-Ri thunderstorms
22. An observational and numerical study of a mini-supercell storm
23. A variational analysis method for retrieval of three-dimensional wind field from single-Doppler radar data
24. Variational algorithms for analysis and assimilation of meteorological observations: Theoretical aspects
25. Severe thunderstorm evolution and mesocyclone structure as related to tornadogenesis
26. The use of adjoint equations to solve a variational adjustment problem with advective constraints
27. Observations of mesoscale circulations within extratropical cyclones over the North Atlantic Ocean during ERICA
28. Simulations of shallow supercell storms in landfalling hurricane environments
29. Convective and rotational parameters associated with three tornado episodes in northern and central California
30. A variational method for real-time retrieval of three-dimensional wind field from multiple-Doppler bistatic radar network data
31. Optimization of dynamic retrievals from a multiple-Doppler radar network
32. Thermodynamic analytical fields from Doppler radar data by means of the MANDOP analysis
33. On the evolution of thunderstorm rotation
34. The influence of the shear induced pressure gradient on thunderstorm motion
35. On the rotation and propagation of simulated supercell thunderstorms
36. The 12/13 January 1988 narrow cold-frontal rainband observed during MFDP/FRONTS 87. Part I: Kinematics and thermodynamics
37. General circulation experiments with the primitive equations: I. The basic experiment
38. Updraft dynamics within a numerically simulated subtropical rainband
39. The structure and classification of numerically simulated convective storms in directionally varying wind shears