97 citations as recorded by crossref.

1. The Relationship between Spatial Variations in the Structure of Convective Bursts and Tropical Cyclone Intensification as Determined by Airborne Doppler Radar J. Wadler et al. 10.1175/MWR-D-17-0213.1
2. The Role of Boundary Layer Dynamics in Tropical Cyclone Intensification. Part I: Sensitivity to Surface Drag Coefficient T. LI & Y. WANG 10.2151/jmsj.2021-027
3. A self‐weakening mechanism for tropical cyclones C. Corsaro & R. Toumi 10.1002/qj.3109
4. Intensity fluctuations in Hurricane Irma (2017) during a period of rapid intensification W. Torgerson et al. 10.5194/wcd-4-331-2023
5. Upper‐tropospheric inflow layers in tropical cyclones S. Wang et al. 10.1002/qj.3856
6. On the hypothesized outflow control of tropical cyclone intensification M. Montgomery et al. 10.1002/qj.3479
7. Response of a tropical cyclone to a subsurface ocean eddy and the role of boundary layer dynamics A. Kumar et al. 10.1002/qj.4210
8. Understanding hurricanes R. Smith & M. Montgomery 10.1002/wea.2776
9. A Parameter for Quantifying the Macroscale Asymmetry of Tropical Cyclone Cloud Clusters K. Ng et al. 10.1175/JTECH-D-19-0160.1
10. Weak Jets and Strong Cyclones: Shallow-Water Modeling of Giant Planet Polar Caps M. O’Neill et al. 10.1175/JAS-D-15-0314.1
11. The role of heating and cooling associated with ice processes on tropical cyclogenesis and intensification G. Kilroy et al. 10.1002/qj.3187
12. Contribution of mean and eddy momentum processes to tropical cyclone intensification M. Montgomery et al. 10.1002/qj.3837
13. Toward Clarity on Understanding Tropical Cyclone Intensification R. Smith & M. Montgomery 10.1175/JAS-D-15-0017.1
14. Tropical cyclone life cycle in a three‐dimensional numerical simulation R. Smith et al. 10.1002/qj.4133
15. The dynamics of intensification in a Hurricane Weather Research and Forecasting simulation of Hurricane Earl (2010) R. Smith et al. 10.1002/qj.2922
16. Impact of the Low Wavenumber Structure in the Initial Vortex Wind Analyses on the Prediction of the Intensification of Hurricane Patricia (2015) Q. Zhong et al. 10.1029/2022JD037082
17. An idealized numerical study of tropical cyclogenesis and evolution at the Equator G. Kilroy et al. 10.1002/qj.3701
18. A Comparison between Moist and Dry Tropical Cyclones: The Low Effectiveness of Surface Sensible Heat Flux in Storm Intensification Z. Ma & J. Fei 10.1175/JAS-D-21-0014.1
19. Influence of region-dependent error growth on the predictability of track and intensity of Typhoon Chan-hom (2020) in high-resolution HWRF ensembles J. Feng et al. 10.1016/j.atmosres.2024.107536
20. Modifications to Three‐Dimensional Turbulence Parameterization for Tropical Cyclone Simulation at Convection‐Permitting Resolution G. Ye et al. 10.1029/2022MS003530
21. A numerical study of deep convection in tropical cyclones G. Kilroy & R. Smith 10.1002/qj.2895
22. The azimuthally averaged boundary layer structure of a numerically simulated major hurricane S. Abarca et al. 10.1002/2015MS000457
23. Tropical cyclone evolution in a minimal axisymmetric model revisited C. Schmidt & R. Smith 10.1002/qj.2753
24. An analysis of the observed low‐level structure of rapidly intensifying and mature hurricaneEarl(2010) M. Montgomery et al. 10.1002/qj.2283
25. Size and Structure of Dry and Moist Reversible Tropical Cyclones D. Wang & Y. Lin 10.1175/JAS-D-19-0229.1
26. Minimal conceptual models for tropical cyclone intensification M. Montgomery & R. Smith 10.1016/j.tcrr.2022.06.002
27. A Triggering Mechanism for Rapid Intensification of Tropical Cyclones Y. Miyamoto & T. Takemi 10.1175/JAS-D-14-0193.1
28. On the Applicability of Linear, Axisymmetric Dynamics in Intensifying and Mature Tropical Cyclones M. Montgomery & R. Smith 10.3390/fluids2040069
29. Effective buoyancy and CAPE: Some implications for tropical cyclones R. Smith & M. Montgomery 10.1002/qj.4294
30. Application of the rotating-convection paradigm for tropical cyclones to interpreting medicanes: An example G. Kilroy et al. 10.1016/j.tcrr.2022.09.001
31. Why Do Model Tropical Cyclones Grow Progressively in Size and Decay in Intensity after Reaching Maturity? G. Kilroy et al. 10.1175/JAS-D-15-0157.1
32. Evaluation of the impact of moist convection on the development of asymmetric inner core instabilities in simulated tropical cyclones J. Naylor & D. Schecter 10.1002/2014MS000366
33. Eyewall Asymmetries and Their Contributions to the Intensification of an Idealized Tropical Cyclone Translating in Uniform Flow J. Martinez et al. 10.1175/JAS-D-21-0302.1
34. Numerical study of the spin‐up of a tropical low over land during the Australian monsoon S. Tang et al. 10.1002/qj.2797
35. Uncertainty in TC Maximum Intensity with Fixed Ratio of Surface Exchange Coefficients for Enthalpy and Momentum H. Ye et al. 10.1007/s13351-022-1120-8
36. Why Do Model Tropical Cyclones Intensify More Rapidly at Low Latitudes? R. Smith et al. 10.1175/JAS-D-14-0044.1
37. The urban effects on the planetary boundary layer wind structures of Typhoon Lekima (2019) G. Ye et al. 10.1016/j.atmosres.2024.107756
38. Axisymmetric Potential Vorticity Evolution of Hurricane Patricia (2015) J. Martinez et al. 10.1175/JAS-D-18-0373.1
39. Does the Rotating Convection Paradigm Describe Secondary Eyewall Formation in Idealized Three-Dimensional Simulations? J. Persing & M. Montgomery 10.1175/JAS-D-21-0143.1
40. Characterizing surface pressure and wind fields of typhoons approaching Hong Kong F. Hu et al. 10.1016/j.jweia.2024.105934
41. Maximizing Simulated Tropical Cyclone Intensity With Action Minimization D. Plotkin et al. 10.1029/2018MS001419
42. The Role of Eyewall Turbulent Transport in the Pathway to Intensification of Tropical Cyclones P. Zhu et al. 10.1029/2021JD034983
43. The response of tropical cyclone intensity to changes in environmental temperature J. Done et al. 10.5194/wcd-3-693-2022
44. Doppler Radar Analysis of the Rapid Intensification of Typhoon Goni (2015) after Eyewall Replacement U. Shimada et al. 10.1175/JAS-D-17-0042.1
45. On the Angular Momentum Loss of Tropical Cyclones: An f-Plane Approximation H. Kang et al. 10.1007/s13143-017-0058-8
46. Assessing the Sensitivity of the Tropical Cyclone Boundary Layer to the Parameterization of Momentum Flux in the Community Earth System Model K. Nardi et al. 10.1175/MWR-D-21-0186.1
47. The generalized Ekman model for the tropical cyclone boundary layer revisited: The myth of inertial stability as a restoring force R. Smith & M. Montgomery 10.1002/qj.3854
48. Why does tropical cyclone intensify faster under weaker parameterized horizontal diffusion in three-dimensional numerical simulations? X. Xie et al. 10.1016/j.atmosres.2024.107322
49. The role of boundary‐layer friction on tropical cyclogenesis and subsequent intensification G. Kilroy et al. 10.1002/qj.3104
50. Dependence of tropical cyclone intensification rate on sea‐surface temperature N. Črnivec et al. 10.1002/qj.2752
51. An Analysis of a Barotropically Unstable, High–Rossby Number Vortex in Shear D. Ryglicki 10.1175/JAS-D-14-0180.1
52. On the Structure and Formation of UTLS PV Dipole/Jetlets in Tropical Cyclones by Convective Momentum Surges M. Hitchman & S. Rowe 10.1175/MWR-D-18-0232.1
53. Scrambling and Reorientation of Classical Atmospheric Boundary Layer Turbulence in Hurricane Winds M. Momen et al. 10.1029/2020GL091695
54. Understanding Atypical Midlevel Wind Speed Maxima in Hurricane Eyewalls D. Stern et al. 10.1175/JAS-D-19-0191.1
55. Recent Developments in the Fluid Dynamics of Tropical Cyclones M. Montgomery & R. Smith 10.1146/annurev-fluid-010816-060022
56. Concentric Eyewall Formation in Typhoon Sinlaku (2008). Part III: Horizontal Momentum Budget Analyses Y. Huang et al. 10.1175/JAS-D-18-0037.1
57. On steady‐state tropical cyclones R. Smith et al. 10.1002/qj.2329
58. Azimuthal Distribution of Deep Convection, Environmental Factors, and Tropical Cyclone Rapid Intensification: A Perspective from HWRF Ensemble Forecasts of Hurricane Edouard (2014) H. Leighton et al. 10.1175/JAS-D-17-0171.1
59. The Effect of Initial Vortex Asymmetric Structure on Tropical Cyclone Intensity Change in Response to an Imposed Environmental Vertical Wind Shear Q. Gao & Y. Wang 10.1029/2023GL104222
60. Effects of sidewall thermal condition on the formation of poloidal circulation in rotating three-dimensional convection V. Kannan et al. 10.1063/5.0190079
61. Tropical convection: the effects of ambient vertical and horizontal vorticity G. Kilroy et al. 10.1002/qj.2261
62. Note on Analyzing Perturbation Growth in a Tropical Cyclone–Like Vortex Radiating Inertia–Gravity Waves D. Schecter & K. Menelaou 10.1175/JAS-D-16-0289.1
63. Impact of the Tropopause Temperature on the Intensity of Tropical Cyclones: An Idealized Study Using a Mesoscale Model S. Wang et al. 10.1175/JAS-D-14-0029.1
64. Towards understanding the tropical cyclone life cycle R. Smith & M. Montgomery 10.1016/j.tcrr.2025.02.003
65. What controls the size of a tropical cyclone? Investigations with an axisymmetric model T. Frisius 10.1002/qj.2537
66. Axisymmetric Balance Dynamics of Tropical Cyclone Intensification and Its Breakdown Revisited R. Smith et al. 10.1175/JAS-D-17-0179.1
67. The Rapid Intensification of Hurricane Karl (2010): New Remote Sensing Observations of Convective Bursts from the Global Hawk Platform S. Guimond et al. 10.1175/JAS-D-16-0026.1
68. Eye of the Storm: Observing Hurricanes with a Small Unmanned Aircraft System J. Cione et al. 10.1175/BAMS-D-19-0169.1
69. Simulated dynamics and thermodynamics processes leading to the rapid intensification of rare tropical cyclones over the North Indian Oceans A. Munsi et al. 10.1007/s12040-022-01951-9
70. Distinct intensification pathways for a shallow-water vortex subjected to asymmetric “diabatic” forcing D. Schecter 10.1016/j.dynatmoce.2020.101156
71. An Observational Study of Tropical Cyclone Spinup in Supertyphoon Jangmi (2008) from 24 to 27 September N. Sanger et al. 10.1175/MWR-D-12-00306.1
72. On the role of convective available potential energy (CAPE) in tropical cyclone intensification M. Lee & T. Frisius 10.1080/16000870.2018.1433433
73. Characterizing the Energetics of Vortex-Scale and Sub-Vortex-Scale Asymmetries during Tropical Cyclone Rapid Intensity Changes F. Marks Jr. et al. 10.1175/JAS-D-19-0067.1
74. Comments on “Revisiting the Balanced and Unbalanced Aspects of Tropical Cyclone Intensification” M. Montgomery & R. Smith 10.1175/JAS-D-17-0323.1
75. Does Balance Dynamics Well Capture the Secondary Circulation and Spinup of a Simulated Hurricane? M. Montgomery & J. Persing 10.1175/JAS-D-19-0258.1
76. Role of eyewall and rainband eddy forcing in tropical cyclone intensification P. Zhu et al. 10.5194/acp-19-14289-2019
77. Quantifying the Rightward Bias Extent of Tropical Cyclones' Cold Wakes Z. Ma et al. 10.1029/2023GL104578
78. Azimuthally averaged structure of Hurricane Edouard (2014) just after peak intensity R. Smith et al. 10.1002/qj.3423
79. A unified view of tropical cyclogenesis and intensification G. Kilroy et al. 10.1002/qj.2934
80. Forced, Balanced Model of Tropical Cyclone Intensification W. SCHUBERT et al. 10.2151/jmsj.2016-007
81. Understanding the Role of Mean and Eddy Momentum Transport in the Rapid Intensification of Hurricane Irma (2017) and Hurricane Michael (2018) A. Green et al. 10.3390/atmos12040492
82. Dynamics of Lower-Tropospheric Vorticity in Idealized Simulations of Tropical Cyclone Formation Y. Wang et al. 10.1175/JAS-D-18-0219.1
83. Comments on “Nonlinear Response of a Tropical Cyclone Vortex to Prescribed Eyewall Heating with and without Surface Friction in TCM4: Implications for Tropical Cyclone Intensification” R. Smith & M. Montgomery 10.1175/JAS-D-16-0163.1
84. Improving Hurricane Analyses and Predictions with TCI, IFEX Field Campaign Observations, and CIMSS AMVs Using the Advanced Hybrid Data Assimilation System for HWRF. Part I: What is Missing to Capture the Rapid Intensification of Hurricane Patricia (2015) when HWRF is already Initialized with a More Realistic Analysis? X. Lu & X. Wang 10.1175/MWR-D-18-0202.1
85. The Impacts of Dry Dynamic Cores on Asymmetric Hurricane Intensification S. Guimond et al. 10.1175/JAS-D-16-0055.1
86. Potential Uncertainties in the Analysis of Low-Wavenumber Asymmetries Caused by Aliasing Center in Tropical Cyclones C. Zhao et al. 10.3390/atmos10060300
87. Development and Nondevelopment of Binary Mesoscale Vortices into Tropical Cyclones in Idealized Numerical Experiments D. Schecter 10.1175/JAS-D-15-0028.1
88. Extreme Low-Level Updrafts and Wind Speeds Measured by Dropsondes in Tropical Cyclones D. Stern et al. 10.1175/MWR-D-15-0313.1
89. A case‐study of a tropical low over northern Australia H. Zhu & R. Smith 10.1002/qj.3762
90. Quasi steady-state hurricanes revisited J. Persing et al. 10.1016/j.tcrr.2019.07.001
91. Impacts of SST Patterns on Rapid Intensification of Typhoon Megi (2010) S. Kanada et al. 10.1002/2017JD027252
92. The Impact of Gradient Wind Imbalance on Tropical Cyclone Intensification within Ooyama’s Three-Layer Model T. Frisius & M. Lee 10.1175/JAS-D-15-0336.1
93. Effects of Horizontal Diffusion on Tropical Cyclone Intensity Change and Structure in Idealized Three-Dimensional Numerical Simulations J. Zhang & F. Marks 10.1175/MWR-D-14-00341.1
94. Putting to rest WISHE‐ful misconceptions for tropical cyclone intensification M. Montgomery et al. 10.1002/2014MS000362
95. On the Origin and Impact of a Polygonal Eyewall in the Rapid Intensification of Hurricane Wilma (2005) K. Menelaou et al. 10.1175/JAS-D-13-091.1
96. Relationships between convective asymmetry, imbalance and intensity in numerically simulated tropical cyclones D. Schecter 10.3402/tellusa.v65i0.20168
97. The Effects of Imposed Stratospheric Cooling on the Maximum Intensity of Tropical Cyclones in Axisymmetric Radiative–Convective Equilibrium H. Ramsay 10.1175/JCLI-D-13-00195.1