Camp J. P.,M. T. Montgomery, 2001: Hurricane maximum intensity: Past and present. Mon. Wea. Rev., 129, 1704-1717, .https://doi.org/10.1175/1520-0493(2001)129<1704:HMIPAP>2.0.CO;2
Eliassen A.,1951: Slow thermally or frictionally controlled meridional circulation in a circular vortex. Astrophisica Norvegica, 5, 19- 60.09907af1f526477dc601882dd7d3f5b2http%3A%2F%2Fwww.ams.org%2Fmathscinet-getitem%3Fmr%3D49032
Emanuel K. A.,1986: An air-sea interaction theory for tropical cyclones. Part I: Steady-state maintenance. J. Atmos. Sci., 43, 585-605, .https://doi.org/10.1175/1520-0469(1986)043<0585:AASITF>2.0.CO;2
Emanuel K. A.,1988: The maximum intensity of hurricanes. J. Atmos. Sci., 45, 1143-1155, .https://doi.org/10.1175/1520-0469(1988)045<1143:TMIOH>2.0.CO;2
Emanuel K. A.,1995: Sensitivity of tropical cyclones to surface exchange coefficients and a revised steady-state model incorporating eye dynamics. J. Atmos. Sci., 52, 3969-3976, .https://doi.org/10.1175/1520-0469(1995)052<3969:SOTCTS>2.0.CO;2
Fudeyasu H.,Y. Q. Wang, 2011: Balanced contribution to the intensification of a tropical cyclone simulated in TCM4: Outer-core spinup process. J. Atmos. Sci., 68, 430-449, .https://doi.org/10.1175/2010JAS3523.1
Hack J. J.,W. H. Schubert, 1986: Nonlinear response of atmospheric vortices to heating by organized cumulus convection. J. Atmos. Sci., 43, 1559-1573, .https://doi.org/10.1175/1520-0469(1986)043<1559:NROAVT>2.0.CO;2
Holland, G. J.,R. T. Merrill, 1984: On the dynamics of tropical cyclone structural changes. Quart. J. Roy. Meteor. Soc., 110, 723-745, .https://doi.org/10.1002/qj.49711046510
Hong S. Y.,J. O. J. Lim, 2006: The WRF single-moment 6-class microphysics scheme (WSM6). Journal of the Korean Meteorological Society, 42, 129- 151.
Hong S. Y.,Y. Noh, and J. Dudhia, 2006: A new vertical diffusion package with an explicit treatment of entrainment processes. Mon. Wea. Rev., 134, 2318-2341, .https://doi.org/10.1175/MWR3199.1
Kepert J.,2001: The Dynamics of Boundary Layer Jets within the Tropical Cyclone Core. Part I: Linear Theory. J. Atmos. Sci., 58, 2469-2484, .https://doi.org/10.1175/1520-0469(2001)058<2469:TDOBLJ>2.0.CO;2
Pendergrass A. G.,H. E. Willoughby, 2009: Diabatically induced secondary flows in tropical cyclones. Part I: Quasi-steady forcing. Mon. Wea. Rev., 137, 805-821, .https://doi.org/10.1175/2008MWR2657.1
Schubert W. H.,J. J. Hack, 1982: Inertial stability and tropical cyclone development. J. Atmos. Sci., 39, 1687-1697, .https://doi.org/10.1175/1520-0469(1982)039<1687:ISATCD>2.0.CO;2
Shapiro L. J.,H. E. Willoughby, 1982: The response of balanced hurricanes to local sources of heat and momentum. J. Atmos. Sci., 39, 378-394, .https://doi.org/10.1175/1520-0469(1982)039<0378:TROBHT>2.0.CO;2
Smith R. K.,M. T. Montgomery, and H. Bui, 2018: Axisymmetric balance dynamics of tropical cyclone intensification and its breakdown revisited. J. Atmos. Sci., 75, 3169-3189, .https://doi.org/10.1175/JAS-D-17-0179.1
Willoughby H. E.,1979: Forced secondary circulations in hurricanes. J. Geophys. Res. Oceans., 84, 3173-3183, .https://doi.org/10.1029/JC084iC06p03173
Wong M. L. M.,J. C. L. Chan, 2004: Tropical cyclone intensity in vertical wind shear. J. Atmos. Sci., 61, 1859-1876, .https://doi.org/10.1175/1520-0469(2004)061<1859:TCIIVW>2.0.CO;2