The role of cumulus convection in hurricanes and its representation in hurricane models

Reviews of Geophysics

Volumn 38, Issue 4, 2000, Pages 465-489

  Smith, R K ^a  

^a UNIVERSITY OF MUNICH   (Germany)

Author keywords

[No Author keywords available]

Indexed keywords

CONVECTION; CUMULUS; HURRICANE; MODELING;

EID: 0034544831     PISSN: 87551209     EISSN: None     Source Type: Journal    
DOI: 10.1029/1999RG000080     Document Type: Article

References (104)

1. Development of asymmetries in a three-dimensional numerical model of a tropical cyclone
2. A cumulus parameterization scheme utilizing a one-dimensional cloud model
3. Hurricane model experiments with a cumulus parameterization scheme
4. Preliminary results from an asymmetric model of the tropical cyclone
5. Comparisons of tropical cyclone simulations with and without the assumption of circular symmetry
6. Closure assumptions in the cumulus parameterization problem
7. Interaction of a cumulus cloud ensemble with the large-scale environment, part I
8. Tropical cyclone simulations with the Betts convective adjustment scheme, part I, Model description and control simulation
9. Tropical cyclone simulations with the Betts convective adjustment scheme, part II, Sensitivity experiments
10. Tropical cyclone simulations with the Betts convective adjustment scheme, part III, Comparison with the Kuo parameterization
11. Convection in the tropics
12. Saturation point analysis of moist convective overturning
13. A new convective adjustment scheme, I, Observational and theoretical basis
14. The nature of adjustment in cumulus clouds fields
15. Gravity waves, compensating subsidence and detrainment around cumulus clouds
16. A comparison of cumulus parameterization techniques
17. On the growth of the hurricane depression
18. CISK or WISHE as the mechanism for tropical cyclone intensification
19. A simplified system of equations for simulating tropical cyclones
20. Experiments with a spectral tropical cyclone model
21. The effects of convection and baroclinicity on the motion of tropical-cyclone-like vortices
22. A monsoon depression over northwestern Australia, part II, A numerical model study
23. Effects of parameterization of latent heating in a tropical prediction model
24. Is there any hope for tropical cyclone intensity prediction?-A panel discussion
25. The Lagrangian parcel dynamics of moist symmetric instability
26. An air-sea interaction theory for tropical cyclones, part I, Steady-state maintenance
27. The finite-amplitude nature of tropical cyclogenesis
28. The theory of hurricanes
29. The behaviour of a simple hurricane model using a convective scheme based on subcloud-layer entropy equilibrium
30. On large-scale circulations of convecting atmospheres
31. Reply to comments on "On large-scale circulations of convecting atmospheres"
32. Dynamic and thermodynamic aspects of the parameterization of cumulus convection
33. The cumulus parameterization problem
34. Nonlinear response of atmospheric vortices to heating by organized convection
35. The structure of a small, intense hurricane-Inez 1996
36. A nested grid for a three-dimensional model of a tropical cyclone
37. A three-dimensional tropical cyclone model with release of latent heat by the resolvable scales
38. Mesoscale and convective-scale characteristics of mature hurricanes, part II, Inner core structure of Hurricane Allen (1980)
39. Numerical experiments of tropical cyclones on a plane with variable Coriolis parameter
40. The simulation of three-dimensional convective storm dynamics
41. A calculation of percent area covered by convective clouds from moisture convergence
42. On parameterization of convective and nonconvective latent heat release
43. On the formation and intensification of tropical cyclones through latent heat release by cumulus convection
44. Further studies of the parameterization of the influence of cumulus convection on large-scale flow
45. Summary of a miniworkshop on cumulus parameterization for mesoscale models
46. A scheme for moist convective adjustment
47. Budget analysis of a tropical cyclone simulated in an axisymmetric model
48. On the development of spiral bands in a tropical cyclone
49. Use of a movable nested-mesh model for tracking a small vortex
50. Structure of a tropical cyclone developed in a three-dimensional numerical simulation model
51. Prediction experiments of Hurricane Gloria (1985) using a multiply nested movable mesh model
52. Numerical simulation of asymmetric hurricanes on a β-plane with vertical shear
53. On the dynamics and energy transformations in steady state hurricanes
54. Simulated climatology of a general circulation model with a hydrological cycle
55. Gregarious tropical convection
56. Equilibrium versus activation control of large-scale variations of tropical deep convection
57. An integrated view of the 1987 Australian monsoon and its mesoscale convective systems, part I, Horizontal structure
58. Parameterization of convective precipitation in mesoscale numerical models: A critical review
59. Thermally forced gravity waves in an atmosphere at rest
60. A dynamical model for the study of tropical cyclone development
61. Numerical simulation of the life cycle of tropical cyclones
62. A theory on parameterization of cumulus convection
63. Conceptual evolution of the theory and modeling of the tropical cyclone
64. Footnotes to "conceptual evolution"
65. Parameterization of convective heat and momentum transfer suggested by analysis of Carribean data
66. Normalized hurricane damage in the United States: 1925-1995
67. The Arakawa-Schubert parameterization
68. Quasi-equilibrium
69. Boundary layer quasi-equilibrium (BLQ)
70. The Kuo parameterization scheme
71. Some aspects of Hurricane Daisy, 1958
72. Numerical experiments with a multi-level primitive-equation model designed to simulate a tropical cyclone, Experiment I
73. Experiments with a numerical model of tropical cyclone development
74. A circularly symmetric primitive equation model of tropical cyclone development containing an explicit water-vapour cycle
75. The response of a tropical-cyclone model to variations in boundary-layer parameters, initial conditions, lateral boundary conditions, and domain size
76. Numerical simulation of tropical cyclone development with latent heat release by the resolvable scales, I, Model description and preliminary results
77. The sensitivity of simulated hurricane development to cumulus parameterization details
78. An air-sea interaction theory for tropical cyclones, part II, Evolutionary study using a nonhydrostatic axisymmetric numerical model
79. Inertial stability and tropical cyclone development
80. Hurricane vortex motion and evolution in a three-layer model
81. The response of balanced hurricanes to local sources of heat and momentum
82. A numerical modelling study of the geostrophic adjustment process following deep convection
83. The surface boundary layer of a hurricane
84. Tropical cyclone eye dynamics
85. On the theory of CISK
86. Numerical simulations of the development of tropical cyclones with a ten-level model, part I
87. The energy and angular momentum budgets of the three-dimensional tropical cyclone model
88. A numerical study on the effects of environmental flow on tropical storm genesis
89. Numerical experiments of the tropical cyclone model by use of the Arakawa-Schubert parameterization
90. Mature structure and evolution
91. Hurricane structure and evolution as simulated by an axisymmetric, nonhydrostatic numerical model
92. A tropical-cyclone model with parameterized partition of released latent heat
93. Detailed analysis of a tropical cyclone simulated with a 13-layer model
94. A numerical experiment of the interaction between cumulus convection and larger-scale motion
95. A preliminary experiment of the tropical cyclone without parameterizing the effects of cumulus convection
96. A further study of the tropical cyclone without parameterizing the effects of cumulus convection
97. A three-dimensional tropical cyclone model with parameterized cumulus convection
98. Parameterization of cumulus convection in a tropical cyclone model
99. A detailed analysis of typhoon formation