International journal of

ADVANCED AND APPLIED SCIENCES

EISSN: 2313-3724, Print ISSN:2313-626X

Frequency: 12

line decor
  
line decor

Volume 4, Issue 11 (November 2017), Pages: 11-16

----------------------------------------------

Technical Note

Title:  Rainfall analysis in the northern region of Peninsular Malaysia

Author(s): A. H. Syafrina 1, *, A. Norzaida 2, O. Noor Shazwani 2

Affiliation(s):

1Department of Science in Engineering, Kuliyyah of Engineering, International Islamic University of Malaysia, 53100 Gombak, Selangor, Malaysia
2UTM Razak School of Engineering and Advanced Technology, Universiti Teknologi Malaysia, Jalan Sultan Yahya Petra, 54100 Kuala Lumpur, Malaysia

https://doi.org/10.21833/ijaas.2017.011.002

Full Text - PDF          XML

Abstract:

Modeling of rainfall is important for assessing the possible impacts of climate change. To achieve accurate projections of rainfall events, availability of sufficient hydrological station data is critical. Precipitation is one of the most important meteorological variables for hydrological modeling. In cases where long series of observed precipitation are not available, they can be stochastically generated by weather generators. Advanced Weather Generator (AWE-GEN) has been proven to generate precipitation data at the temperate climate regions with Gamma distribution being incorporated in the model to represent rainfall intensity. However, in a tropical climate such as Malaysia, some studies disputed the incorporation of Gamma distribution. As such, in this study, Weibull a heavy tail distribution is proposed to be used. The AWE-GEN has well performed in the wetter region such as the eastern of the peninsular. However, rainfall distribution within Peninsular Malaysia is highly variable temporally and spatially. The northern region is drier especially during the southwest monsoon season. This region receives minimal rain during the northeast monsoon due to the presence of the Titiwangsa Range which obstructs the region from getting rain by the north easterly winds. Therefore, the objectives of the study are two-fold. First, this study compares the performance of Gamma and Weibull that are incorporated in the AWE-GEN in simulating rainfall series for the northern region of the peninsular. Second, the monthly rainfall and the extreme rainfall series are simulated using the better distribution. The performances of Gamma and Weibull distributions are compared using the goodness of fit test, Root Mean Square Error (RMSE). Results showed that Gamma is the better distribution in simulating rainfall at rainfall stations located at the outer parts of the northern coast whereas Weibull is the better distribution for stations located in the interior parts of the northern coast. Hourly and daily extreme rainfalls seem to be well captured at all stations. Similarly, wet spell length is well simulated while in contrast, dry spell length is slightly underestimated at all stations. Overall, Gamma and Weibull produce commendable results in simulating extreme rainfall as well as wet spell length throughout the northern region of the peninsular. 

© 2017 The Authors. Published by IASE.

This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/).

Keywords: Extreme, Gamma, Rainfall intensity, Weather generator, Weibull, Goodness of fit

Article History: Received 14 July 2017, Received in revised form 15 September 2017, Accepted 16 September 2017

Digital Object Identifier: 

https://doi.org/10.21833/ijaas.2017.011.002

Citation:

Syafrina AH, Norzaida A, and Shazwani ON (2017). Rainfall analysis in the northern region of Peninsular Malaysia. International Journal of Advanced and Applied Sciences, 4(11): 11-16

Permanent Link:

http://www.science-gate.com/IJAAS/V4I11/Syafrina.html

----------------------------------------------

References (13)

  1. Abas N, Daud ZM, and Yusof F (2014). A comparative study of mixed exponential and Weibull distributions in a stochastic model replicating a tropical rainfall process. Theoretical and Applied Climatology, 118(3): 597-607. https://doi.org/10.1007/s00704-013-1060-4 
  2. Cheng CS, Auld H, Li Q, and Li G (2012). Possible impacts of climate change on extreme weather events at local scale in South-Central Canada. Climatic Change, 112(3-4): 963-979. https://doi.org/10.1007/s10584-011-0252-0 
  3. Chu HJ, Pan TY, and Liou JJ (2012). Change-point detection of long-duration extreme precipitation and the effect on hydrologic design: A case study of South Taiwan. Stochastic Environmental Research and Risk Assessment, 26(8): 1123-1130. https://doi.org/10.1007/s00477-012-0566-0 
  4. Huang CY, Wong CS, and Yeh TC (2011) Extreme rainfall mechanisms exhibited by Typhoon Morakot (2009). Terrestrial Atmospheric and Ocean Sciences, 22(6): 613-632. https://doi.org/10.3319/TAO.2011.07.01.01(TM) 
  5. IPCC (2007). Climate change 2007: The physical science basis. Summary for Policymakers, Contribution of Working Group I to the Fourth Assessment, Intergovernmental Panel on Climate Change, Geneva, Switzerland.     
  6. Norzaida A, Zalina MD, and Fadhilah Y (2016). Application of Fourier series in managing the seasonality of convective and monsoon rainfall. Hydrological Sciences Journal, 61(10): 1967-1980. https://doi.org/10.1080/02626667.2015.1062892 
  7. Sen Roy S (2009). A spatial analysis of extreme hourly precipitation patterns in India. International Journal of Climatology, 29(3): 345–355. https://doi.org/10.1002/joc.1763 
  8. Suhaila J, Deni SM, Zin WWZ, and Jemain AA (2010). Trends in peninsular Malaysia rainfall data during the Southwest Monsoon and Northeast Monsoon seasons: 1975-2004. Sains Malaysiana, 39(4): 533-542.     
  9. Syafrina AH, Zalina MD, and Juneng L (2015). Historical trend of hourly extreme rainfall in Peninsular Malaysia. Theoretical and Applied Climatology, 120(1-2): 259–285. https://doi.org/10.1007/s00704-014-1145-8 
  10. Tangang FT, Juneng L, Salimun E, Sei KM, Le LJ, and Muhamad H (2012). Climate change and variability over Malaysia. Sains Malaysiana, 41(11): 1355-1366.     
  11. Willems P, Arnbjerg-Nielsen K, Olsson J, and Nguyen VTV (2012). Climate change impact assessment on urban rainfall extremes and urban drainage: Methods and shortcomings. Atmospheric Research, 103: 106-118. https://doi.org/10.1016/j.atmosres.2011.04.003 
  12. Wong CL, Liew J, Yusop Z, Ismail T, Venneker R, and Uhlenbrook S (2016). Rainfall characteristics and regionalization in Peninsular Malaysia based on a high resolution gridded data set. Water, 8(11): 500-516. https://doi.org/10.3390/w8110500 
  13. Zin WZW, Jamaludin S, Deni SM, and Jemain AA (2010). Recent changes in extreme rainfall events in Peninsular Malaysia: 1971-2005. Theoretical and Applied Climatology, 99(3-4): 303-314. https://doi.org/10.1007/s00704-009-0141-x