- Quarterly Journal of the Royal Meteorological Society Q. J. R. Meteorol. Soc. 136: 19451953, October 2010 Part B Sensitivity of tropical-cyclone models
- Quarterly Journal of the Royal Meteorological Society Q. J. R. Meteorol. Soc. 137: 250263, January 2011 Part A The dynamics of heat lows over elevated terrain
- QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY Q. J. R. Meteorol. Soc. 137: 131 (2011)
- ForPeerReview Inner-Core Vacillation Cycles during the Intensification of Hurricane Katrina 1
- WeatherNovember2005,Vol.60,No.11 "Why must hurricanes have eyes?"
- In August 2005 Hurricane Katrina wreaked havoc on New Orleans, claiming 1300 lives and causing $125bn
- QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY Q. J. R. Meteorol. Soc. 135: 16971714 (2009)
- Tellus (2006), 58A, 98103 Copyright C Blackwell Munksgaard, 2006 Printed in Singapore. All rights reserved TELLUS
- The Role of Cumulus Convection in Hurricanes and its Representation in Hurricane Models
- Q. J. R. Meteorol. Soc. (2002), 128, pp. 23352347 doi: 10.1256/qj.01.53 Comparison of an axisymmetric hurricane model with the corresponding
- 1052 VOLUME 18W E A T H E R A N D F O R E C A S T I N G 2003 American Meteorological Society
- Available onlineat www.sciencedirect.com s c l E N c E @ D ~ n E c T * dynamics
- Low-Level Convergence Lines over Northeastern Australia. Part I: The North Australian Cloud Line
- Low-Level Convergence Lines over Northeastern Australia. Part II: Southerly Disturbances
- QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY Q. J. R. Meteorol. Soc. 134: 563582 (2008)
- QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY Q. J. R. Meteorol. Soc. 134: 551561 (2008)
- QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY Q. J. R. Meteorol. Soc. 00: 116 (2008)
- QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY Q. J. R. Meteorol. Soc. 135: 13211335 (2009)
- Australian Meteorological and Oceanographic Journal 60 (2010) 91-101 Introduction
- Quarterly Journal of the Royal Meteorological Society Q. J. R. Meteorol. Soc. 136: 549551, January 2010 Part B Notes and Correspondence
- QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY Q. J. R. Meteorol. Soc. 136: 16 (2010)
- ForPeerReview QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY
- Quarterly Journal of the Royal Meteorological Society Q. J. R. Meteorol. Soc. 136: 21762188, October 2010 Part B The formation of a multicell thunderstorm
- WMO/CAS/WWW SEVENTH INTERNATIONAL WORKSHOP ON TROPICAL CYCLONES
- Quarterly Journal of the Royal Meteorological Society Q. J. R. Meteorol. Soc. 137: 845857, April 2011 B Tropical cyclone convection: the effects of ambient vertical
- QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY Q. J. R. Meteorol. Soc. 00: 116 (2010)
- QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY Q. J. R. Meteorol. Soc. 00: 110 (2010)
- Q. J. R. Meteorol. Soc. (2002), 128, pp. 120 A simple model of the hurricane boundary layer
- MesoLAPS Predictions of Low-Level Convergence Lines over Northeastern Australia BERNADETT WEINZIERL
- Q. J. R. Meteorol. Soc. (2005), 131, pp. 31473165 doi: 10.1256/qj.04.177 The dynamics of heat lows in simple background flows
- QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY Q. J. R. Meteorol. Soc. 135: 17151731 (2009)
- Q. J. R. Meteorol. Soc. (2002), ?, pp. 115 Terrain influences on the dynamics of heat lows
- The Pre-Depression Investigation of Cloud Systems in the Tropics (PREDICT) Experiment: Scientific Basis, New Analysis Tools and
- QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY Q. J. R. Meteorol. Soc. 00: 116 (2011)
- QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY Q. J. R. Meteorol. Soc. 137: 118 (2011)
- Quarterly Journal of the Royal Meteorological Society Q. J. R. Meteorol. Soc. 137: 829844, April 2011 B Inner-core vacillation cycles during the intensification of
- Manuscript prepared for Atmos. Chem. Phys. with version 3.2 of the LATEX class copernicus.cls.
- Quarterly Journal of the Royal Meteorological Society Q. J. R. Meteorol. Soc. 138: 15 (2012) How important is the isothermal expansion effect to elevating
