PRELIMINARY STUDY ON RELATIONSHIP BETWEEN DOUBLE VORTICES SELF-ORGANIZATION AND TYPHOON FORMATION IN BAROCLINIC ENVIRONMENT
The relationship between the self-organization of double vortices (SODVs) and the formation of typhoons was discussed based on six numerical experiments with the Fifth-Generation National Center for Atmospheric Research/Penn State Mesoscale Model (MM5) and further discussion was made with a real typ...
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Published in | Journal of Tropical Meteorology Vol. 16; no. 4; p. 372 |
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Main Authors | , , , |
Format | Journal Article |
Language | English |
Published |
Guangzhou
Guangzhou Institute of Tropical & Marine Meteorology
01.12.2010
Zhejiang Meteorological Observatory, Hangzhou 310017 China%School of Remote Sensing, NUIST, Nanjing 210044 China%Shanghai Typhoon Institute of CMA, Shanghai 200030 China |
Subjects | |
Online Access | Get full text |
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Summary: | The relationship between the self-organization of double vortices (SODVs) and the formation of typhoons was discussed based on six numerical experiments with the Fifth-Generation National Center for Atmospheric Research/Penn State Mesoscale Model (MM5) and further discussion was made with a real typhoon case. The results showed that there is a critical distance d sub( c) for SODVs in baroclinic atmosphere. When the distance between separated vortices is smaller than or equal to d sub( c), the double vortices self-organize into a typhoon-like vortex with two spiral bands. But the double vortices cannot have such organization if the distance between them is larger than d sub( c). The value of d sub( c) is about 380 km in the context of ideal conditions in this paper, larger than that achieved in a barotropic model. A typical typhoon case in 2005 (Haitang) was selected to verify the above-mentioned conclusions. It was found that the SODV is one of the important and typical ways for the formation of typhoons. |
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Bibliography: | ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 |
ISSN: | 1006-8775 |
DOI: | 10.3969/j.issn.1006-8775.2010.04.009 |