Abstract
This study presents the spatial analysis of daily rainfall intensity and concentration index over Peninsular Malaysia. Daily rainfall data from 50 rainfall stations are used in this study. Due to the limited number of stations, the geostatistical method of ordinary kriging is used to compute the values of daily rainfall concentration and intensity and to map their spatial distribution. The resultant analysis of rainfall concentration indicated that the distribution of daily rainfall is more regular over the west, northwest and southwest regions compared to the east. Large areas of the eastern Peninsula display an irregularity in distribution of daily rainfall. In terms of number of rainy days, analysis of daily rainfall confirms that a large number of rainy days across the Peninsula arise from low-intensity events but only contribute a small percentage of total rain. On the other hand, a low frequency of rainy days with high-intensity events contributes the largest percentage of total rain. The results indicated that the total rain in eastern areas is mainly contributed by the high-intensity events. This finding explains the occurrence of a large number of floods and soil erosions in these areas. Therefore, precautionary measures should be taken earlier to prevent any massive destruction of property and loss of life due to the hazards. These research findings are of considerable importance in providing enough information to water resource management, climatologists and agriculturists as well as hydrologists for planning their activities and modelling processes.
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Acknowledgements
The authors are indebted to the staff of the Drainage and Irrigation Department and the Malaysian Meteorological Department for providing the daily rainfall data used in this study. The comments of an anonymous referee are also acknowledged. This research was funded by the Universiti Teknologi Malaysia (UTM—short-term vote 77354).
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Suhaila, J., Jemain, A.A. Spatial analysis of daily rainfall intensity and concentration index in Peninsular Malaysia. Theor Appl Climatol 108, 235–245 (2012). https://doi.org/10.1007/s00704-011-0529-2
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DOI: https://doi.org/10.1007/s00704-011-0529-2