Abstract
This study aimed to identify the wet period, peaks of mean rainfall amount per rainy day at Kelantan River basin. Daily rainfall data from 12 selected rainfall stations for the period of 1975–2014 which comprises of three main areas such as inland, river, and coastal are analyzed. The estimated wet period, date, and value at peak of mean rainfall amount per rainy day will be identified using Fourier series and compared with the actual flood events in 2013/2014 and 2014/2015. The findings indicate that duration of wet periods obtained from the results of best fitting justifies the flood event occurred most recently. Moreover, the coastal area of Kelantan also shows the highest probability of rainfall amounts exceeding 60 mm.
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References
Jimoh OD, Webster P (1999) Stochastic modeling of daily rainfall in Nigeria: intra-annual variation of model parameters. J Hydrol 222:1–17
Woolhiser DA, Pegram GGS (1979) Maximum likelihood estimation of Fourier coefficients to describe seasonal variations of parameters in stochastic daily precipitation models. J Appl Meteorol 18(1):34–44
Kottegoda NT, Natale L, Raiteri E (2004) Some considerations of periodicity and persistence in daily rainfalls. J Hydrol 296:23–37
Edelsten PR (1976) A stochastic model of the weather at Hurley in S.E. Engl Meteorol Mag 105:206–214
Coe R, Stern RD (1982) Fitting models to daily rainfall data. J Appl Meteorol 21:1024–1031
Stern RD, Coe R (1984) A model fitting analysis of daily rainfall data. J Roy Stat Soc Ser A 147:1–34
Suhaila J, Jemain AA (2009) A comparison of the rainfall pattern between stations on the east and west coasts of Peninsular Malaysia using the smoothing model of rainfall amounts. Meteorol Appl 16:391–401
Suhaila J, Deni SM, Jemain AA (2008) Detecting inhomogeneity of rainfall series in Peninsular Malaysia. Asia-Pac J Atmos Sci 44(4):369–380
Sullivan DO, Unwin DJ (2003) Geographic information analysis. Wiley, Hoboken
Firth D (1988) Multiplicative errors: lognormal or gamma? J Roy Stat Soc Ser B 50:266–268
McCullagh P, Nelder JA (1989) Generalized linear models. Chapman and Hall, London
Garbutt DJ, Stern RD, Dennett MD, Elston J (1981) A comparison of the rainfall climate of eleven places in West Africa using a two part model of daily rainfall. Arch Meteorol Geophys Bioclimatol Ser B 29:137–155
Acknowledgment
The authors are indebted to the staff of the Drainage and Irrigation Department and Malaysia Meteorological Department for providing the daily rainfall data for this study. They also acknowledge their sincere appreciation to the reviewers for their valuable suggestion and remarks in order to improve the manuscript. This research will not complete without the sponsorship from Ministry of Higher Education (600-RMI/TRGS DIS 5/3 (1/2015)).
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Mah Hashim, N., Mohd Deni, S., Shariff, S.S.R., Tahir, W., Jani, J. (2016). Identification of Seasonal Rainfall Peaks at Kelantan Using Fourier Series. In: Tahir, W., Abu Bakar, P., Wahid, M., Mohd Nasir, S., Lee, W. (eds) ISFRAM 2015. Springer, Singapore. https://doi.org/10.1007/978-981-10-0500-8_14
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DOI: https://doi.org/10.1007/978-981-10-0500-8_14
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