A simple model of the hurricane boundary layerSMITH, Roger K.Quarterly Journal of the Royal Meteorological Society. 2003, Vol 129, Num 589, pp 1007-1027, issn 0035-9009, 21 p., CArticle

Accurate determination of a balanced axisymmetric vortex in a compressible atmosphereSMITH, Roger K.Tellus. Series A, Dynamic meteorology and oceanography. 2006, Vol 58, Num 1, pp 98-103, issn 0280-6495, 6 p.Article

Tropical cyclone convection: the effects of ambient vertical vorticityWISSMEIER, Ulrike; SMITH, Roger K.Quarterly Journal of the Royal Meteorological Society. 2011, Vol 137, Num 657, pp 845-857, issn 0035-9009, 13 p., bArticle

The dynamics of heat lows over flat terrainSPENGLER, Thomas; SMITH, Roger K.Quarterly Journal of the Royal Meteorological Society. 2008, Vol 134, Num 637, pp 2157-2172, issn 0035-9009, 16 p.Article

Tropical-cyclone intensification and predictability in a minimal three-dimensional modelSHIN, Seoleun; SMITH, Roger K.Quarterly Journal of the Royal Meteorological Society. 2008, Vol 134, Num 636A, pp 1661-1671, issn 0035-9009, 11 p.Article

The importance of three physical processes in a minimal three-dimensional tropical cyclone modelHONGYAN ZHU; SMITH, Roger K.Journal of the atmospheric sciences. 2002, Vol 59, Num 11, pp 1825-1840, issn 0022-4928Article

A simple model of the hurricane boundary layer revisitedSMITH, Roger K; VOGL, Stefanie.Quarterly Journal of the Royal Meteorological Society. 2008, Vol 134, Num 631, pp 337-351, issn 0035-9009, 15 p.Article

Effects of vertical differencing in a minimal hurricane modelHONGYAN ZHU; SMITH, Roger K.Quarterly Journal of the Royal Meteorological Society. 2003, Vol 129, Num 589, pp 1051-1069, issn 0035-9009, 19 p., CArticle

A numerical study of rotating convection during tropical cyclogenesisKILROY, Gerard; SMITH, Roger K.Quarterly Journal of the Royal Meteorological Society. 2013, Vol 139, Num 674, pp 1255-1269, issn 0035-9009, 15 p.Article

The dynamics of heat lows over elevated terrainSMITH, Roger K; SPENGLER, Thomas.Quarterly Journal of the Royal Meteorological Society. 2011, Vol 137, Num 654, pp 250-263, issn 0035-9009, 14 p., aArticle

Limitations of a linear model for the hurricane boundary layerVOGL, Stefanie; SMITH, Roger K.Quarterly Journal of the Royal Meteorological Society. 2009, Vol 135, Num 641, pp 839-850, issn 0035-9009, 12 p.Article

Terrain influences on the dynamics of heat lowsREICHMANN, Zsuzsanna; SMITH, Roger K.Quarterly Journal of the Royal Meteorological Society. 2003, Vol 129, Num 591, pp 1779-1793, issn 0035-9009, 15 p., BArticle

On the existence of the logarithmic surface layer in the inner core of hurricanesSMITH, Roger K; MONTGOMERY, Michael T.Quarterly Journal of the Royal Meteorological Society. 2014, Vol 140, Num 678, pp 72-81, issn 0035-9009, 10 p., aArticle

Observations of the convective environment in developing and non-developing tropical disturbancesSMITH, Roger K; MONTGOME, Michael T.Quarterly Journal of the Royal Meteorological Society. 2012, Vol 138, Num 668, pp 1721-1739, issn 0035-9009, 19 p.Article

Buoyancy in tropical cyclones and other rapidly rotating atmospheric vorticesSMITH, Roger K; MONTGOMERY, Michael T; HONGYAN ZHU et al.Dynamics of atmospheres and oceans. 2005, Vol 40, Num 3, pp 189-208, issn 0377-0265, 20 p.Conference Paper

Tropical convection: the effects of ambient vertical and horizontal vorticityKILROY, Gerard; SMITH, Roger K; WISSMEIER, Ulrike et al.Quarterly Journal of the Royal Meteorological Society. 2014, Vol 140, Num 682, pp 1756-1770, issn 0035-9009, 15 p.Article

How important is the isothermal expansion effect in elevating equivalent potential temperature in the hurricane inner core?SMITH, Roger K; MONTGOMERY, Michael T.Quarterly Journal of the Royal Meteorological Society. 2013, Vol 139, Num 670A1, pp 70-74, issn 0035-9009, 5 p.Article

Balanced boundary layers used in hurricane modelsSMITH, Roger K; MONTGOMERY, Michael T.Quarterly Journal of the Royal Meteorological Society. 2008, Vol 134, Num 635, pp 1385-1395, issn 0035-9009, 11 p.Article

A minimal three-dimensional tropical cyclone modelHONGYAN ZHU; SMITH, Roger K; ULRICH, Wolfgang et al.Journal of the atmospheric sciences. 2001, Vol 58, Num 14, pp 1924-1944, issn 0022-4928Article

On steady-state tropical cyclonesSMITH, Roger K; MONTGOMERY, Michael T; PERSING, John et al.Quarterly Journal of the Royal Meteorological Society. 2014, Vol 140, Num 685, pp 2638-2649, issn 0035-9009, 12 p., bArticle

Notes and Correspondence On an analytical model for the rapid intensification of tropical cyclonesMONTGOMERY, Michael T; SMITH, Roger K.Quarterly Journal of the Royal Meteorological Society. 2010, Vol 136, Num 647B, pp 549-551, issn 0035-9009, 3 p.Article

The formation of a multicell thunderstorm behind a sea-breeze frontWISSMEIER, Ulrike; SMITH, Roger K; GOLER, Robert et al.Quarterly Journal of the Royal Meteorological Society. 2010, Vol 136, Num 653, pp 2176-2188, issn 0035-9009, 13 p., bArticle

The Importance of the Boundary Layer Parameterization in the Prediction of Low-Level Convergence LinesTHOMSEN, Gerald L; SMITH, Roger K.Monthly weather review. 2008, Vol 136, Num 6, pp 2173-2185, issn 0027-0644, 13 p.Article

Dependence of tropical-cyclone intensification on the boundary-layer representation in a numerical modelSMITH, Roger K; THOMSEN, Gerald L.Quarterly Journal of the Royal Meteorological Society. 2010, Vol 136, Num 652, pp 1671-1685, issn 0035-9009, 15 p., aArticle

Hurricane boundary-layer theorySMITH, Roger K; MONTGOMERY, Michael T.Quarterly Journal of the Royal Meteorological Society. 2010, Vol 136, Num 652, pp 1665-1670, issn 0035-9009, 6 p., aArticle