Abstract
Tropical cyclones are frequent visitors to the North and South Pacific Ocean. In the Southwest Pacific region (south of the equator from the east coast of Australia to French Polynesia), approximately eight cyclones occur on average each year during the tropical cyclone season, which runs from November to April inclusive. The variability in tropical cyclone occurrence is high, ranging from as few as two (e.g., 1990/91) to as many as eighteen (e.g., 1997/98). Much of this variability is attributed to the influence of the El Niño/Southern Oscillation (ENSO) phenomenon as the warm oceanic waters move eastward and contribute to more favourable formation conditions.
This is a preview of subscription content, log in via an institution to check access.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
Preview
Unable to display preview. Download preview PDF.
Similar content being viewed by others
References
Fiji Meteorological Service (1996) Manual of Procedures-Cyclone Warning Organisation. Fiji Meteorological Services, Nadi Airport, Fiji
World Meteorological Organisation (WMO) (1997) Tropical Cyclone Operational Plan for the South Pacific and Southeast Indian Ocean. WMO/TD-No. 292, TCP-24, World Meteorological Organisation, Genèva
Author information
Authors and Affiliations
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 2003 Springer-Verlag Berlin Heidelberg
About this chapter
Cite this chapter
Prasad, V., Koop, N.L. (2003). The Tropical Cyclone Warning System in the Southwest Pacific. In: Zschau, J., Küppers, A. (eds) Early Warning Systems for Natural Disaster Reduction. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-55903-7_24
Download citation
DOI: https://doi.org/10.1007/978-3-642-55903-7_24
Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-642-63234-1
Online ISBN: 978-3-642-55903-7
eBook Packages: Springer Book Archive