Abstract

The unpredictable extreme rainfall can affect flood. Prediction of extreme rainfall is needed to do, so that the efforts to preventing the flood can be effective. One of the methods that can predict the extreme rainfall is the Spatial Extreme Value (SEV) with the Max-Stable Process (MSP) approach. The important purpose of SEV is calculated of return level (the extreme value prediction). The calculation of return level depends on parameter estimation in that method. This research discusses about parameter estimation of the Spatial Extreme Value Max-Stable Process especially Smith model. Parameter estimation was performed using Maximum Composite Likelihood Estimation (MCLE) method and Maximum Pairwise Likelihood Estimation (MPLE) method. The result of estimation using this method is not closed form, it must be continued by using numerical iteration method. The iteration method used in this research is Broyden-Fletcher Goldfarb-Shanno (BFGS) Quasi Newton, which is faster than other methods to achieve convergence. The result of parameter estimation applied to the rainfall data of Ngawi Regency which is the Regency with the largest rice production in East Java Province (the province with the largest rice farm in Indonesia). Based on the results of data analysis obtained trend surface model (s) = 2,794 + 0,242 v(s); (s) = 1,8196 + 0,1106 v(s); (s) = 1,012 with goodness criterion model Takeuchi Information Criterion (TIC) 26237,62. Root Mean Square Error (RMSE) based on 20 testing data is 32,078 and Mean Absolute Percentage Error (MAPE) is 27,165%

Highlights

  • The unpredictable extreme rainfall can affect flood

  • Parameter estimation method which is mostly proposed by the previous researchers is Maximum Pairwise Likelihood Estimation (MPLE)

  • If the result of parameter estimation is not closed form, so that it must be continued by using numerical iteration method, in research, it will be used iteration method of Broyden-Fletcher GoldfarbShanno (BFGS) Quasi Newton

Read more

Summary

INTRODUCTION1

The unpredictable extreme rainfall is cause of flood. The extreme rainfall prediction needs to be done. One method to predict extreme rainfall value is Spatial Extreme Value (SEV). SEV can be approached by Max-Stable Process (MSP). The main goal of SEV is to acquire return level (prediction value of extreme happening). Return level can be acquired when a number of parameter estimators are known. Parameter estimation method which is mostly proposed by the previous researchers is Maximum Pairwise Likelihood Estimation (MPLE). This research estimates parameter toward Max-Stable Process (MSP), which involves one of its model, it is Smith Model. If the result of parameter estimation is not closed form, so that it must be continued by using numerical iteration method, in research, it will be used iteration method of Broyden-Fletcher GoldfarbShanno (BFGS) Quasi Newton

Extreme Value Theory
Spatial Extreme Value
Max-Stable Process
Block Maxima
Extremal Coefficient
Return Level
Takeuchi Information Criterion
Maximum Pairwise Likelihood Estimation
Smith Model Parameter Estimation Using MPLE w
Quasi Newton BFGS Iteration Algorithm
Application to Real Data
Conclusion
CONCLUSION

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.