Development of Strong Convection in the Inner Core of Tropical Cyclones during Intensification

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Jeff Callaghan
Jeff Callaghan

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Development of Strong Convection in the Inner Core of Tropical Cyclones during Intensification

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Abstract

Recent intensifying tropical cyclones around the globe are analysed to examine the observed winds structure in their inner core. The winds in sectors with strong bands of thunderstorms were observed from computer model analyses to turn in an anticyclonic fashion from the 850hPa level up to the 500hPa level. This wind structure resembles Quasi-Geostrophic warm air advection and from Hysplit Trajectory analysis was in areas of ascending air currents suitable for the initiation of thunderstorms.

References

11 Cites in Article
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  4. John Knaff,T Cram,A Schumacher,J Kossin,M De Maria (2008). Objective Identification of Annular Hurricanes.
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  9. Herbert Riehl,Joanne Malkus (1958). ON THE HEAT BALANCE AND MAINTENANCE OF CIRCULATION IN THE TRADES.
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Funding

No external funding was declared for this work.

Conflict of Interest

The authors declare no conflict of interest.

Ethical Approval

No ethics committee approval was required for this article type.

Data Availability

Not applicable for this article.

How to Cite This Article

Jeff Callaghan. 2026. \u201cDevelopment of Strong Convection in the Inner Core of Tropical Cyclones during Intensification\u201d. Global Journal of Science Frontier Research - H: Environment & Environmental geology GJSFR-H Volume 22 (GJSFR Volume 22 Issue H2): .

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High-resolution study on tropical cyclone intensification in the inner core using advanced convection analysis.
Issue Cover
GJSFR Volume 22 Issue H2
Pg. 43- 62
Journal Specifications

Crossref Journal DOI 10.17406/GJSFR

Print ISSN 0975-5896

e-ISSN 2249-4626

Keywords
Classification
GJSFR-H Classification: DDC Code: 551.116 LCC Code: QE509.4
Version of record

v1.2

Issue date

April 16, 2022

Language
en
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Published Article

Recent intensifying tropical cyclones around the globe are analysed to examine the observed winds structure in their inner core. The winds in sectors with strong bands of thunderstorms were observed from computer model analyses to turn in an anticyclonic fashion from the 850hPa level up to the 500hPa level. This wind structure resembles Quasi-Geostrophic warm air advection and from Hysplit Trajectory analysis was in areas of ascending air currents suitable for the initiation of thunderstorms.

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Development of Strong Convection in the Inner Core of Tropical Cyclones during Intensification

Jeff Callaghan
Jeff Callaghan

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