Tracking Tropical Cyclone Zelia: Overview and Implications
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Tropical Cyclone Zelia has formed in the Indian Ocean with sustained winds of 58 miles per hour. Cyclones in the Southern Hemisphere, which spin clockwise, differ from Atlantic hurricanes. These storms can significantly impact various regions and have a seasonal pattern from late October to May, peaking in late February and March.
Tropical Cyclone Zelia emerged in the Indian Ocean early on Wednesday, as reported by the Joint Typhoon Warning Center. The storm exhibited sustained winds reaching 58 miles per hour, indicating its potential strength. Satellite imagery is instrumental in assessing a storm’s robustness; a well-defined and symmetrical eye suggests that the cyclone is not encountering significant weakening factors.
Cyclones predominantly develop in the Southern Hemisphere, accounting for only about a quarter of Earth’s tropical cyclones. In this region, storms classified with sustained winds of 74 miles per hour or higher are referred to as cyclones, contrasting with hurricanes in the Atlantic, which rotate counterclockwise. In the Southern Hemisphere, cyclones spin in a clockwise direction.
The geographical impact of cyclones is notable, as they can affect eastern Africa, particularly Madagascar, along with the western, northern, and eastern coastal regions of Australia and its nearby islands. The tropical cyclone season in the Southern Hemisphere typically commences in late October and lasts through May, with peak activity usually occurring in late February and early March, although variations exist based on the specific region involved.
In summary, Tropical Cyclone Zelia is currently being monitored in the Indian Ocean, displaying considerable wind strength. The understanding of cyclone formation and behavior, particularly in the Southern Hemisphere, highlights the differences from hurricanes. Additionally, the seasonal patterns of cyclones underscore their potential impact in various regions, emphasizing the importance of continued monitoring and analysis.
Original Source: www.nytimes.com