CONCLUSIONS AND SUGGESTION Calibration of Monthly Spatial Runoff from the Root Zone using Water Balance Method (A Case Study in Cicatih Watershed, Sukabumi, West Java)

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V. CONCLUSIONS AND SUGGESTION

5. 1 Conclusions The calibration procedures consist of two steps parameters optimization. Firstly, optimize the parameters c and WHC according to the criterion RE. Secondly, optimize the parameter WHC again according to the criterion R 2 , with the value of c obtained in the first step. The results of monthly spatial runoff presented in the article had proved to be quite efficient of describing the monthly runoff with R 2 value of 66.15 and relative error RE of 1.4 . The method can easily be incorporated in water resources planning program to estimate monthly runoff in the Cicatih watershed because of their simplicity and efficiency of performance. The implication of the study is to describe the comparison between monthly spatial runoff of the 1999 land uses pattern and the recent year land uses pattern. The result of spatially distributed runoff clearly indicated the influence of rainfall, land cover types, and water holding capacity WHC. However, the monthly distibuted runoff was only affected by the rainfall. The runoff distributions of subwaterheds showed that runoff varied from 263 mm in Ciheulang subwatershed to 26 mm in Cikembar subwatershed. The monthly runoff distribution of Cicatih watershed showed that the lowest runoff was 35 mm occurred in September and the highest runoff was 260 mm occurred in January. The spatial runoff distribution in Cicatih watershed reflected that during the high rainfall period in Cicatih, maximum runoff could be found in the forest areas 286 mm and followed by cropland areas 269 mm. And minimum runoff was 251 mm occurred in settlement areas. In the low rainfall period, maximum runoff 109 mm was found in forest areas. Minimum runoff was 0 mm occured in the settlement areas, followed by cropland areas 5 mm around the mountain Salak and mountain Pangrango. It was found that runoff increased with significant incresing rainfall, following a positive linear function.

5. 2 Suggestion

For future applications, it is suggested to consider the rainfall-runoff pattern in water resources planning program Cicatih Watershed, Sukabumi, West Java.

VI. REFERENCES