A numerical study of tropical cyclone formation from two mesoscale convective systems in a large-scale convective system

Scientific Online Letters on the Atmosphere

Volumn 2, Issue , 2006, Pages 57-60

  Yamasaki, Masanori ^a  

^a JAPAN AGENCY FOR MARINE EARTH SCIENCE AND TECHNOLOGY   (Japan)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 34848919237     PISSN: None     EISSN: 13496476     Source Type: Journal    
DOI: 10.2151/sola.2006-015     Document Type: Article

References (11)

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2. Gray, W. M., 1968: Global view of the origin of tropical disturbances and storms. Mon. Wea. Rev., 96, 669-700
3. Gray, W. M., 1979: Hurricanes: Their formation, structure and likely role in the tropical circulation. Meteorology Over the Tropical Oceans, D. B. Shaw, Ed., Roy. Meteor. Soc., 155-218
4. Reasor, P. D., M. T. Montgomery, and L. F. Bosart, 2005: Mesosale observations of the genesis of Hurricane Dolly (1996). J. Atmos. Sci., 62, 3151-3171
5. Simpson, J., E. Ritchie, G. J. Holland, J. Halverson, and S. Stewart, 1997: Mesoscale interactions in tropical cyclone genesis. Mon. Wea. Rev., 125, 2643-2661
6. Yamasaki, M., 1986: A three-dimensional tropical cyclone model with parameterized cumulus convection. Pap. Meteor. Geophys., 37, 205-234
7. Yamasaki, M., 1988: Towards an understanding of the interaction between convection and the larger-scale in the tropics. Aust. Met. Mag., 36, 171-182
8. Yamasaki, M., 1989a: Numerical experiment of tropical cyclone formation in the intertropical convergence zone. J. Meteor. Soc. Japan, 67, 529-540
9. Yamasaki, M., 1989b: Advances in basic understanding of tropical cyclone formation, The second WMO international workshop on tropical cyclones, Manila, WMO Tropical Meteorology Research Programme Report Series, WMO/TD-No. 319, Vol. 1, 125-142
10. Yamasaki, M., 2002: A study of cloud clusters associated with a Baiu front by use of a mesoscale-convection-resolving model. J. Meteor. Soc. Japan, 80, 595-619
11. Yamasaki, M., 2006: A study of tropical cyclone formation with a 20-km grid model. SOLA, 2, 9-12