Idealised modelling of tropical cyclones in vertical shear: The role of saturated ascent in the inner core

26th Conference on Hurricanes and Tropical Meteorology

Volumn , Issue , 2004, Pages 98-99

  Patra, Richard ^a  

^a UNIVERSITY OF MUNICH   (Germany)

Author keywords

[No Author keywords available]

Indexed keywords

LATENT HEAT RELEASE; STATIC STABILITY; TROPICAL CYCLONES (TC); VERTICAL CIRCULATION;

CLOUDS; HEAT CONVECTION; HEAT LOSSES; MATHEMATICAL MODELS; STORMS; WIND EFFECTS;

METEOROLOGY;

EID: 3042755362     PISSN: None     EISSN: None     Source Type: Conference Proceeding    
DOI: None     Document Type: Conference Paper

References (5)

1. DeMaria, M., 1996: The Effect of Vertical Shear on Tropical Cyclone Intensity Change. J. Atmos. Sci., 53, 2076-2087.
2. Durran, D. R. and J. B. Klemp, 1982: On the Effects of Moisture on the Brunt-Väisälä Frequency. J. Atmos. Sci., 39, 2152-2158.
3. Frank, W. M. and E. A. Ritchie, 1999: Effects of Environmental Flow upon Tropical Cyclone Structure. Mon. Wea. Rev., 127, 2044-2061.
4. Jones, S. C., 1995: The evolution of vortices in vertical shear. I: Initially barotropic vortices. Quart. J. Roy. Meteor. Soc., 121, 821-851.
5. Möller, J. D. and M. T. Montgomery, 1999: Tropical Cyclone Evolution via Potential Vorticity Anomalies in a Three-Dimensional Balance Model. J. Atmos. Sci., 57, 3366-3387.