Abstract
East Coast of India is vulnerable for tropical cyclone hazards which form over Bay of Bengal (BoB). The average annual frequency of tropical cyclones over the BoB and Arabian Sea (AS) is about five (about 5-6% of the global annual average) and about 80 cyclones form around the globe in a year. The frequency is more in the BoB than in the Arabian Sea, the ratio being 4:1. The monthly frequency of tropical cyclones in the north Indian Ocean display a bi-modal characteristic with a primary peak in November and secondary peak in May.
Keywords
- Tropical Cyclone
- India Meteorological Department
- North Indian Ocean
- Tropical Cyclone Activity
- Tropical Cyclone Genesis
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.
This is a preview of subscription content, access via your institution.
Buying options
Preview
Unable to display preview. Download preview PDF.
References
Belanger, James I., Webster, Peter J., Curry, Judith A. and Jelinek, Mark T. (2012). Extended Prediction of North Indian Ocean Tropical Cyclones. Wea. Forecasting, 27: 757-769.
Burpee, B. (1974). Characteristics of North African easterly waves during the summers of 1968 and 1969. J. Atmos. Sci., 31: 1556-1570.
Carlson, T.N. (1969). Synoptic histories of three African disturbances that developed into Atlantic hurricanes. Mon.Weather Rev., 97: 256-276.
Das, P.K, Sinha, M.C. and Balasubramanyam, V. (1974). Storm surges in the Bay of Bengal. Quarterly Journal of the Royal Meteorological Society, 100: 437-449.
Dube, S.K., Rao, A.D., Sinha, P.C., Murty, T.S. and Bahulayan, N. (1997). Storm surge in the Bay of Bengal and Arabian Sea: The problem and its prediction. Mausam, 48: 283-304.
Emanuel, K.A. (2005). Divine Wind: The History and Science of Hurricanes. Oxford University Press, New York.
Frank, N.L. (1970). Atlantic tropical systems of 1969. Mon. Wea. Rev., 98: 307-314.
Hart, R.E. (2003). A cyclone phase space derived from thermal wind and thermal asymmetry. Mon. Wea. Rev., 131: 585-616.
IMD – http://www.imd.gov.in/section/nhac/dynamic/faq/FAQP.htm
Ind. Met. Dept. (1979). Tracks of storms and depressions.
Ind. Met. Dept. (1996). Tracks of storms and depressions – An addendum to the Storm Track Atlas (1891-1970).
Ritchie, E.A. and Holland, G.J. (1999). Large-scale patterns associated with tropical cyclogenesis in the western Pacific. Mon. Wea. Rev., 127: 2027-2043.
Thorncroft, C.D. and Hodges, K. (2001). African easterly wave variability and its relationship to Atlantic tropical cyclone activity. J. Climate, 14: 1166-1179.
Author information
Authors and Affiliations
Corresponding author
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 2014 Capital Publishing Company
About this chapter
Cite this chapter
Rajasekhar, M., Kishtawal, C.M., Prasad, M.Y.S., Rao, V.S., Rajeevan, M. (2014). Extended Range Tropical Cyclone Predictions for East Coast of India. In: Mohanty, U.C., Mohapatra, M., Singh, O.P., Bandyopadhyay, B.K., Rathore, L.S. (eds) Monitoring and Prediction of Tropical Cyclones in the Indian Ocean and Climate Change. Springer, Dordrecht. https://doi.org/10.1007/978-94-007-7720-0_13
Download citation
DOI: https://doi.org/10.1007/978-94-007-7720-0_13
Publisher Name: Springer, Dordrecht
Print ISBN: 978-94-007-7719-4
Online ISBN: 978-94-007-7720-0
eBook Packages: Earth and Environmental ScienceEarth and Environmental Science (R0)