首页> 外文期刊>International Journal of Applied Engineering Research >Comparison of Hydrology Component Spatial Correlation Model (Continuous Model) and Markov Chain (Case Study of Cikapundung Watershed, Saguling Reservoir and Cipanunjang Reservoir)
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Comparison of Hydrology Component Spatial Correlation Model (Continuous Model) and Markov Chain (Case Study of Cikapundung Watershed, Saguling Reservoir and Cipanunjang Reservoir)

机译:水文分量空间相关模型(连续模型)和马尔可夫链的比较(Cikapundung流域,绘图水库和Capanunjang水库的案例研究)

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摘要

Water allocation in the watershed is a concern in developing countries where there are limited water resources and greater demands with more parties. Past data on water flow amount is the only information available to estimate future water delivery. One of the strategies used is to determine the exact number of water discharge based on past recorded data. Future prediction data is essential for sustainable management of water resources. The objective of this research is to construct a hydrological model to estimate or anticipate future water discharge using the Discrete Chain Markov model where the results are then compared with continuous discharge rain model by implementing multiple linear regression method. Both components (rain and discharge) are then modified into several alternatives in 3 different research sites to analyze and compare the combination of the results with the highest correlation value. The inflow discharge data in Cipanunjang used in this study is the data retrieved from 2000-2013; data of Cikapunung Watershed are retrieved from 2003-2012. Meanwhile, data of Saguling are extracted from 1986-2013. In spatial correlation method, QQQQ combination was acquired in Cipanunjang, while the best combination that can be acquired in Cikapundung and Saguling watersheds is QQ_(t-1)PP. The correlation values based on the spatial correlation method in Cipanunjang, Cikapundung watershed, and Saguling were 0.882, 0.871 and 0.857, respectively. Meanwhile, the correlation values of Discrete Markov method in the same places were 0.899, 0.718 and 0.782, respectively. These results suggest that this continuous method can be used to predict the amount of water discharge in the future well enough and is effectively used in Indonesia territories.
机译:分水岭中的水分配是发展中国家的担忧,水资源有限,更多的各方需求更大。过去的水流量数据是唯一可用于估算未来水交付的信息。使用的策略之一是基于过去录制数据来确定水放电的确切数量。未来的预测数据对于水资源的可持续管理至关重要。该研究的目的是使用离散链马尔可夫模型来构建水文模型来估计或预测未来的排水模型,然后通过实现多元线性回归方法与连续排放雨模型进行比较。然后将组件(雨和放电)修改为3种不同的研究部位中的几种替代品,以分析和比较结果与最高相关值的结果。本研究中使用的CIPANUNJANG中的流入放电数据是从2000 - 2013中检索的数据; Cikapunung流域的数据从2003 - 2012年回收。同时,从1986-2013提取了SAGULING的数据。在空间相关方法中,QQQQ组合在CIPANUNJANG获得,而可以在Cikapundung和SAGULING流域中获得的最佳组合是QQ_(T-1)PP。基于CIPANUNJANG,CIKAPUNDUNG流域和SAGULING的空间相关方法的相关值分别为0.882,0.871和0.857。同时,相同位置的离散性马尔可夫方法的相关值分别为0.899,0.718和0.782。这些结果表明,这种连续方法可用于预测未来的排水量足够好,并在印度尼西亚领土有效地使用。

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